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Water contamination news: USA – Fracking – Investigation reveals fracking fluids were illegally dumped – STEM water education – Why dumping chemicals and waste endangers our water supply.

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Water contamination news: USA – Fracking

Water contamination news USA -  Fracking- Investigation reveals fracking fluids were illegally dumped - STEM water education - Why dumping chemicals and waste endangers our water supply.

Investigation reveals fracking fluids were illegally dumped

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After a video posted to YouTube sparked an investigation the state’s water watchdog says fluids containing chemicals from an oil well were illegally dumped into the ground.

The Vintage Oil Company well was drilled and fracked, a controversial process of extracting oil from dense rock. Although the Central Valley Regional Water Quality Control Board said its investigation isn’t complete but board officials say they know already something illegal was done. “Nobody is protecting us,” said almond farmer Tom Frantz.

We first showed you video last February of an Vintage Oil Company well being drilled near an almond orchard in Shafter. “Ten yards away a farmer was flood irrigating his almonds at about the same time,” said Frantz. Frantz captured the video back in October. At first he thought it was the release of fracking fluids, chemicals pumped into the ground to make oil flow. “It turns out they weren’t fracking until the next day they were just getting ready to frack,” said Frantz.

Documents released by Vintage reveal this was the release of what the oil company calls drilling and formation fluids. “We do not believe it was in compliance with the conditional waiver,” said Clay Rodgers, Executive Officer for the Central Valley Regional Water Quality Control Board.

However the documents reveal fracking fluids were released at that site at a later date. A letter says on October 7th and 8th fracking fluids “estimated to be five barrels or less on each date” were discharged into an unlined pond. According to the Rodgers, that is illegal. Tom Frantz thinks it’s happening often.

“I wasn’t that lucky to get there on the only day the only time they did something illegal. If I’m that lucky I should get a lottery ticket,” said Frantz. Vintage said in the documents they do not believe “drilling operations…contaminated soil, creeks, wetlands.” Vintage did say however the company is making progress toward “ceasing the use of unlined sumps” near farmland. “We think that is a promising solution that they are not going to use the unlined ponds,” said Rodgers.

But Tom Frantz said it’s too little late. “We already see when no one is watching, they do something illegal and this is the tip of the iceberg,” said Frantz. A Vintage spokesperson would not comment saying it was “premature.” Once Central Valley Water Board completes their investigation the company could face fines and a possible drilling moratorium. According to vintage, 83 percent of what was released was water, 8 percent was sand and the rest were chemicals like methanol, known as wood alcohol, potassium hydroxide, a corrosive substance and sodium hydroxide, also known as lye. There are a small percentage of chemicals not disclosed, which the company calls “trade secrets.” According to Vintage documents these chemicals were kept from ground water.

But Frantz who took video that lead to the investigation of the fracked well thinks otherwise. “It may not be a hazardous substance but do you want to drink it do you want it in your water no,” said Frantz.

Why dumping chemicals and waste endangers our water supply

Save the Water™ Education Dept. Groundwater can become contaminated in many ways. If rain water or surface water comes into contact with contaminated soil while seeping into the ground, it can become polluted and can carry the pollution from the soil to the groundwater.

Groundwater can also become contaminated when liquid hazardous substances themselves soak down through the soil or rock into the groundwater. Some liquid hazardous substances do not mix with the groundwater but remain pooled within the soil or bedrock. These pooled substances can act as long-term sources of groundwater contamination as the groundwater flows through the soil or rock and comes into contact with them.

Right click on image and view image to enlarge Groundwater can become contaminated in many ways. If rain water or surface water comes into contact with contaminated soil while seeping into the ground, it can become polluted and can carry the pollution from the soil to the groundwater. Groundwater can also become contaminated when liquid hazardous substances themselves soak down through the soil or rock into the groundwater. Some liquid hazardous substances do not mix with the groundwater but remain pooled within the soil or bedrock. These pooled substances can act as long-term sources of groundwater contamination as the groundwater flows through the soil or rock and comes into contact with them.
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Water contamination education news: Fracking – Fracking defined – Fracking infographics – Water education resources.

Water contamination news: Fracking

Fracking education update

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Hydraulic fracturing is the propagation of fractures in a rock layer by a pressurized fluid. Some hydraulic fractures form naturally certain veins or dikes are examples—and can create conduits along which gas and petroleum from source rocks may migrate to reservoir rocks. Induced hydraulic fracturing or hydrofracturing, commonly known as fracing, fraccing, or fracking, is a technique used to release petroleum, natural gas (including shale gas, tight gas, and coal seam gas), or other substances for extraction. This type of fracturing creates fractures from a wellbore drilled into reservoir rock formations.

The first use of hydraulic fracturing was in 1947. However, it was only in 1998 that modern fracturing technology, referred to as horizontal slickwater fracturing, made possible the economical extraction of shale gas; this new technology was first used in the Barnett Shale in Texas. The energy from the injection of a highly pressurized hydraulic fracturing fluid creates new channels in the rock, which can increase the extraction rates and ultimate recovery of hydrocarbons.

Proponents of hydraulic fracturing point to the economic benefits from vast amounts of formerly inaccessible hydrocarbons the process can extract. Opponents point to potential environmental impacts, including contamination of ground water, risks to air quality, the migration of gases and hydraulic fracturing chemicals to the surface, surface contamination from spills and flowback and the health effects of these. For these reasons hydraulic fracturing has come under scrutiny internationally, with some countries suspending or banning it.

History

Fracturing as a method to stimulate shallow, hard rock oil wells dates back to the 1860s. It was applied by oil producers in the US states of Pennsylvania, New York, Kentucky, and West Virginia by using liquid and later also solidified nitroglycerin. Later, the same method was applied to water and gas wells. The idea to use acid as a nonexplosive fluid for well stimulation was introduced in the 1930s. Due to acid etching, fractures would not close completely and therefore productivity was enhanced. The same phenomenon was discovered with water injection and squeeze cementing operations.

The relationship between well performance and treatment pressures was studied by Floyd Farris of Stanolind Oil and Gas Corporation. This study became a basis of the first hydraulic fracturing experiment, which was conducted in 1947 at the Hugoton gas field in Grant County of southwestern Kansas by Stanolind. For the well treatment 1,000 US gallons (3,800 l; 830 imp gal) of gelled gasoline and sand from the Arkansas River was injected into the gas-producing limestone formation at 2,400 feet (730 m).

The experiment was not very successful as deliverability of the well did not change appreciably. The process was further described by J.B. Clark of Stanolind in his paper published in 1948. A patent on this process was issued in 1949 and an exclusive license was granted to the Halliburton Oil Well Cementing Company. On March 17, 1949, Halliburton performed the first two commercial hydraulic fracturing treatments in Stephens County, Oklahoma, and Archer County, Texas.[15] Since then, hydraulic fracturing has been used to stimulate approximately a million oil and gas wells.

In the Soviet Union, the first hydraulic proppant fracturing was carried out in 1952. In Western Europe in 1977–1985, hydraulic fracturing was conducted at Rotliegend and Carboniferous gas-bearing sandstones in Germany, Netherlands onshore and offshore gas fields, and the United Kingdoms sector of the North Sea. Other countries in Europe and Northern Africa included Norway, the Soviet Union, Poland, Czechoslovakia, Yugoslavia, Hungary, Austria, France, Italy, Bulgaria, Romania, Turkey, Tunisia, and Algeria.

Due to shale’s high porosity and low permeability, technology research, development and demonstration were necessary before hydraulic fracturing could be commercially applied to shale gas deposits. In the 1970s the United States government initiated the Eastern Gas Shales Project, a set of dozens of public-private hydraulic fracturing pilot demonstration projects. During the same period, the Gas Research Institute, a gas industry research consortium, received approval for research and funding from the Federal Energy Regulatory Commission.

In 1977, the Department of Energy pioneered massive hydraulic fracturing in tight sandstone formations. In 1997, based on earlier techniques used by Union Pacific Resources, now part of Anadarko Petroleum Corporation, Mitchell Energy, now part of Devon Energy, developed the hydraulic fracturing technique known as “slickwater fracturing” which involves adding chemicals to water to increase the fluid flow, that made the shale gas extraction economical.

Method A hydraulic fracture is formed by pumping the fracturing fluid into the wellbore at a rate sufficient to increase pressure downhole to exceed that of the fracture gradient (pressure gradient) of the rock. The fracture gradient is defined as the pressure increase per unit of the depth due to its density and it is usually measured in pounds per square inch per foot or bars per meter. The rock cracks and the fracture fluid continues further into the rock, extending the crack still further, and so on.

Operators typically try to maintain “fracture width”, or slow its decline, following treatment by introducing into the injected fluid a proppant – a material such as grains of sand, ceramic, or other particulates, that prevent the fractures from closing when the injection is stopped and the pressure of the fluid is reduced. Consideration of proppant strengths and prevention of proppant failure becomes more important at greater depths where pressure and stresses on fractures are higher. The propped fracture is permeable enough to allow the flow of formation fluids to the well. Formation fluids include gas, oil, salt water, fresh water and fluids introduced to the formation during completion of the well during fracturing.

During the process fracturing fluid leakoff, loss of fracturing fluid from the fracture channel into the surrounding permeable rock occurs. If not controlled properly, it can exceed 70% of the injected volume. This may result in formation matrix damage, adverse formation fluid interactions, or altered fracture geometry and thereby decreased production efficiency.

The location of one or more fractures along the length of the borehole is strictly controlled by various methods that create or seal off holes in the side of the wellbore. Typically, hydraulic fracturing is performed in cased wellbores and the zones to be fractured are accessed by perforating the casing at those locations.

Hydraulic-fracturing equipment used in oil and natural gas fields usually consists of a slurry blender, one or more high-pressure, high-volume fracturing pumps (typically powerful triplex or quintuplex pumps) and a monitoring unit. Associated equipment includes fracturing tanks, one or more units for storage and handling of proppant, high-pressure treating iron, a chemical additive unit (used to accurately monitor chemical addition), low-pressure flexible hoses, and many gauges and meters for flow rate, fluid density, and treating pressure. Fracturing equipment operates over a range of pressures and injection rates, and can reach up to 100 megapascals (15,000 psi) and 265 litres per second (9.4 cu ft/s) (100 barrels per minute).

Fracturing fluids.

Proppants and fracking fluids and List of additives for hydraulic fracturing

High-pressure fracture fluid is injected into the wellbore, with the pressure above the fracture gradient of the rock. The two main purposes of fracturing fluid is to extend fractures and to carry proppant into the formation, the purpose of which is to stay there without damaging the formation or production of the well. Two methods of transporting the proppant in the fluid are used – high-rate and high-viscosity. High-viscosity fracturing tends to cause large dominant fractures, while high-rate (slickwater) fracturing causes small spread-out micro-fractures.

This fracture fluid contains water-soluble gelling agents (such as guar gum) which increase viscosity and efficiently deliver the proppant into the formation.

The fluid injected into the rock is typically a slurry of water, proppants, and chemical  additives. Additionally, gels, foams, and compressed gases, including nitrogen, carbon dioxide and air can be injected. Typically, of the fracturing fluid 90% is water and 9.5% is sand with the chemical additives accounting to about 0.5%.

A proppant is a material that will keep an induced hydraulic fracture open, during or following a fracturing treatment, and can be gel, foam, or slickwater-based. Fluids make tradeoffs in such material properties as viscosity, where more viscous fluids can carry more concentrated proppant; the energy or pressure demands to maintain a certain flux pump rate (flow velocity) that will conduct the proppant appropriately; pH, various rheological factors, among others. Types of proppant include silica sand, resin-coated sand, and man-made ceramics.

These vary depending on the type of permeability or grain strength needed. The most commonly used proppant is silica sand, though proppants of uniform size and shape, such as a ceramic proppant, is believed to be more effective. Due to a higher porosity within the fracture, a greater amount of oil and natural gas is liberated.

The fracturing fluid varies in composition depending on the type of fracturing used, the conditions of the specific well being fractured, and the water characteristics. A typical fracture treatment uses between 3 and 12 additive chemicals. Although there may be unconventional fracturing fluids, the typical used chemical additives are:

•Acids—hydrochloric acid (usually 28%-5%), or acetic acid is used in the pre-fracturing stage for cleaning the perforations and initiating fissure in the near-wellbore rock.

•Sodium chloride (salt)—delays breakdown of the gel polymer chains.

•Polyacrylamide and other friction reducers—minimizes the friction between fluid and pipe, thus allowing the pumps to pump at a higher rate without having greater pressure on the surface. Polyacrylamide are good suspension agents ensuring the proppant does not fall out.

• Ethylene glycol—prevents formation of scale deposits in the pipe.

•Borate salts—used for maintaining fluid viscosity during the temperature increase.

•Sodium and potassium carbonates—used for maintaining effectiveness of crosslinkers.

•Glutaraldehyde—used as disinfectant of the water (bacteria elimination).

•Guar gum and other water-soluble gelling agents—increases viscosity of the fracturing fluid to deliver more efficiently the proppant into the formation.

•Citric acid—used for corrosion prevention.

•Isopropanol—increases the viscosity of the fracture fluid.

The most common chemical used for hydraulic fracturing in the United States in 2005–2009 was methanol, while some other most widely used chemicals were isopropyl alcohol, 2-butoxyethanol, and ethylene glycol.

Typical fluid types.

• Conventional linear gels. These gels are cellulose derivatives (carboxymethyl cellulose, hydroxyethyl cellulose, carboxymethyl hydroxyethyl cellulose, hydroxypropyl cellulose, methyl hydroxyl ethyl cellulose), guar or its derivatives (hydroxypropyl guar, carboxymethyl hydroxypropyl guar) based, with other chemicals providing the necessary chemistry for the desired results.

•Borate-crosslinked fluids. These are guar-based fluids cross-linked with boron ions (from aqueous borax/boric acid solution). These gels have higher viscosity at pH 9 onwards and are used to carry proppants. After the fracturing job the pH is reduced to 3–4 so that the cross-links are broken and the gel is less viscous and can be pumped out.

•Organometallic-crosslinked fluids zirconium, chromium, antimony, titanium salts are known to crosslink the guar based gels. The crosslinking mechanism is not reversible. So once the proppant is pumped down along with the cross-linked gel, the fracturing part is done. The gels are broken down with appropriate breakers.

•Aluminium phosphate-ester oil gels. Aluminium phosphate and ester oils are slurried to form cross-linked gel. These are one of the first known gelling systems.

For slickwater it is common to include sweeps or a reduction in the proppant concentration temporarily to ensure the well is not overwhelmed with proppant causing a screen-off. As the fracturing process proceeds, viscosity reducing agents such as oxidizers and enzyme breakers are sometimes then added to the fracturing fluid to deactivate the gelling agents and encourage flowback. The oxidizer reacts with the gel to break it down, reducing the fluid’s viscosity and ensuring that no proppant is pulled from the formation.

An enzyme acts as a catalyst for the breaking down of the gel. Sometimes pH modifiers are used to break down the crosslink at the end of a hydraulic fracturing job, since many require a pH buffer system to stay viscous.  At the end of the job the well is commonly flushed with water (sometimes blended with a friction reducing chemical) under pressure.

Injected fluid is to some degree recovered and is managed by several methods, such as underground injection control, treatment and discharge, recycling, or temporary storage in pits or containers while new technology is being continually being developed and improved to better handle waste water and improve re-usability.

Text is available under the Creative Commons Attribution-ShareAlike License; additional terms may apply. See Terms of Use for details.
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USA water crisis news: Bayou Corne – Assumption Parish – Sinkhole suits will be consolidated into a class action – update news by Susan Buchan

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USA water crisis news: Bayou Corne – Assumption Parish

USA water crisis news:  Bayou Corne - Assumption Parish

Sinkhole suits will be consolidated into a class action.

Article courtesy of Susan Buchanan /Contributing Writer / The Louisiana Weekly newspaper

Residents near Bayou Corne in Assumption Parish noticed excessive bubbling a year ago, and on August 3 the state issued a mandatory evacuation for about 350 people as a sinkhole grew. They weren’t forced to leave, however.

Last week, plaintiffs’ attorneys said hundreds of residents and business owners near the Bayou Corne sinkhole can participate in a class-action suit in U.S. Eastern District Court in New Orleans.

Larry Centola of Martzell & Bickford in New Orleans said Thursday “we estimate there are over 300 people in the class. The class definition is awaiting approval by Judge Jay Zainey.” Centola is a member of the Plaintiffs’ Steering Committee chosen by the judge in December in LeBlanc et al. versus Texas Brine in U.S. District Court.

In a May 22 press release, the Plaintiffs’ Steering Committee, appointed by Judge Zainey and representing property owners near the sinkhole, said the judge issued a small entry certifying a class action against Houston-based Texas Brine and Dallas-based Occidental Chemical on behalf of Bayou Corne residents evacuated since August. The judge’s action was based on a PSC motion.

Last week’s PSC release said all cases filed in U.S. District Court will be consolidated into one legal action. Individuals who aren’t represented by an attorney are included if they’re within the class. The release said “the presumed class will likely consist of all persons who owned or leased property that is included in the mandatory evacuation area.”

A document filed by the Plaintiffs’ Steering Committee in Eastern District Court on May 16 provides more hints about class characteristics. According to it, the class could consist of those who lived in the evacuation area on August 2 or owned a business there, along with any businesses that conducted most of their activity there.

Last Tuesday, Judge Zainey said attorneys have until June 10 to give him a proposed order to grant class-action status to four lawsuits.

Last Thursday, Centola said “Texas Brine has until June 24 to make offers to people who do not have a lawyer. That deadline will be set by court order but the order hasn’t been formalized yet.”

Texas Brine spokesman Sonny Cranch said last week his company is trying to settle with 108 property owners who aren’t represented by attorneys. Texas Brine was ready to make settlement offers to homeowners this month when two of its three insurers pulled out of the plan early last week, he said.

“Our principal insurer, Zurich American, is in full support, but we suddenly learned that two ancillary insurers were not on board,” Cranach said last Tuesday. The ancillary insurers are Arch Specialty Insurance Co. and American Guarantee and Liability Insurance Co.

Cranch said his company phoned Governor Bobby Jindal’s office Monday morning to discuss problems with those two insurers. “We asked if there was any way the governor could use his office to influence them. But Governor Jindal was noncommittal.”

At the time of the phone call, Texas Brine wasn’t aware that Governor Jindal planned to hold a press conference Monday afternoon in Bayou Corne.

Last Monday, Jindal criticized the company for its slow progress in settlement talks with homeowners. He said Texas Brine’s failure to offer settlements to owners raises question about the company’s ability to operate in Louisiana. Jindal said he asked the state’s Commissioner of Conservation to review permits issued to Texas Brine to assess the company’s financial condition and to decide if those permits should be altered or terminated. Jindal said he instructed all state agencies, along with any local government entities involved in sinkhole response, to gauge whether Texas Brine can meet its regulatory obligations.

Jindal said “it has become clear that Texas Brine is trying to run out the clock on the citizens of Bayou Corne and Grand Bayou by hiding behind insurance companies, lawyers and lobbyists.” The governor said the company is responsible for the sinkhole.

Jindal’s first visit to the sinkhole was on March 13. At that time, he appointed a blue ribbon commission to assess the situation, including public safety.

Last Tuesday, Cranch said “we would be devastated if the state of Louisiana closed our operations.“ The family-owned business also produces brine in Texas, Virginia and New York. “We’re in talks with our insurers as I speak. We’re prepared to settle with Bayou Corne homeowners. That’s why we hired home inspectors and appraisers in March.”

Cranch said “For homeowners who want to move, we plan to buy their property at market prices seen in January 2012 before the first bubbles appeared in the sinkhole last summer. We will also pay for emotional distress. For those owners who plan to stay in their homes, we’ll pay for their loss in home value and emotional distress.”

In a May 20 letter to Bayou Corne residents, Texas Brine said the company has spent more than $40 million on sinkhole response, including over $4.8 million on evacuation assistance. “We are actively engaged with the offices of the Governor and the Insurance Commissioner to keep them informed of the current situation with our insurance carriers,” the letter signed by Texas Brine operations vice president Bruce Martin said.

According to Texas Brine, 111 property owners had requested settlement forms as of May 21; 105 had submitted claims information; 103 properties had been inspected; and two properties still had to be inspected.

Cranch said Texas Brine voluntarily committed to make settlement offers within 45 days of property inspections. As of May 24, however, 85 inspected properties had reached the 45-day threshold without settlement offers.

As for the two insurers that are dragging their feet, Cranch said “this is like paying for car insurance every year, then you get in an accident and the insurer won’t cover injuries to passengers in the other vehicle. You ask yourself what have I been paying for all along?”

He’s sympathetic to residents but said the closest homes to the sinkhole are half a mile away. “No homes have fallen into the hole,” he said. “No one’s been injured. Some owners claim damage to their foundations or door frames, and we’ll consider that on a case by case basis.”

John Boudreaux, director of the Assumption Parish Office of Homeland Security, said last week “many residents have reported cracked foundations and also sheetrock cracks in their residences.” He’s not aware of any sinkhole-related injuries to residents of Bayou Corne or Grand Bayou. He said “a few months ago, when a rig for a well at the sinkhole was being demobilized, a worker sustained a minor injury.”

Rodney Mallett, Louisiana Dept. of Environmental Quality spokesman, said “the air and water quality samples we’ve taken show no environmental impacts. The air is okay and surface water is okay.”

The sinkhole formed following the collapse of a Texas Brine-operated cavern in a salt dome. The company extracted brine from the cavern and piped it to chemical plants along the Mississippi River. The cavern’s failure released natural gas and oil from formations along the salt dome.

Residents have worried about radioactivity at the site but Cranch believes that’s a non-issue. “A bag of fertilizer, the bricks in your home and clay are all radioactive but at such low levels they pose no health threat,” he said. “When we replace tubing in our wells, we find tiny flakes of radioactive metal caused by interaction with sodium. We report all of it to DEQ. Radioactivity in the flakes is at levels that are no threat to human health.“

Most of the issues at the sinkhole are moving towards resolution, Cranch said. “The sinkhole has widened since last summer, and it’s now 15 acres in area,” he said. “But it’s also gotten much shallower. Today it’s 170 feet deep compared to 450 feet deep last August. Tetra Tech is building an 8-foot containment levee around it. We’re flaring off what’s left of the natural gas in the aquifer. We feel as if we’re on he road to a stable situation.” Tetra Tech is based in California.

The surrounding bayous also bubble

Cranch said “the sinkhole bubbles because gas in pockets squeezes up through rock and clay to the surface. The surrounding bayous also bubble.”

He said Texas Brine operates over a dozen brine wells in three salt domes in Assumption, Lafourche and Iberville parishes, supplying sodium chloride to chemical companies Georgia Gulf, OxyChem and Shintech for their plants on the Mississippi River between Baton Rouge and New Orleans. Those plants manufacture caustic soda and chlorine used in plastics, water purification, paper, pharmaceuticals and organic and inorganic chemicals. “PVC or polyvinyl chloride plastic pipes, widely used in home construction, are made from sodium chloride,” Cranch said.

Texas Brine produces water saturated with salt through solution mining, as opposed to dry mining. The cylindrically-shaped cavern at Bayou Corne was created in 1982 when the company drilled down 6,000 feet. Water injected into the underground salt dome dissolved salt and formed a liquid brine. The cavern was plugged under an order from the Louisiana Dept. of Natural Resources last June.

“It was our decision to close the cavern, and to do that we filled it with brine,” Cranch said. “We’d mined it to the end of its productive life.”

Cranch said the state-by-state contribution—from its operations in Louisiana, Texas, Virginia and New York—to the company’s bottom line is proprietary. Texas Brine is the nation’s top, independent brine producer, supplying over 30 percent of U.S. chlor-alkali needs, he said.

This article originally published in the May 27, 2013 print edition of The Louisiana Weekly newspaper.Copyright 2011 Louisianaweekly.com. All rights reserved

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WHOLE WORLD Water seeks to prove that economic, social, and environmental progress are not mutually exclusive. Developed to end the global water and sanitation crisis, WHOLE WORLD Water works to engage the hospitality and tourism industry to filter, bottle, and sell its own water, and contribute 10% of the proceeds to the WHOLE WORLD Water Fund. 100% of the proceeds will go directly to clean and safe water initiatives worldwide.
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  • Contaminated drinking water: Risk of viral acute gastrointestinal illness from nondisinfected drinking water distribution systems.
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    Louisiana water crisis news – Lake Peigneur bill defeated – SB200 Senator Fred H. Mills Jr. failed 17 yeas and 19 nays – Bayou Corne – House near sinkhole burns after lightning strike.

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    Water crisis: Louisiana – Lake Peigneur bill defeated

    Lake Peigneur

    SB200 Senator Fred H. Mills, Jr. Failed 17 yeas and 19 nays.

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    Save Lake Peigneur, Inc. / Nara Crowley / May 22, 2013
    SALT DOMES: Prohibits the issuance of certain permits to create or convert a solution mined cavern for storage purposes.

    SB200 had been amended. SB200 was to provide for the prohibition of certain permits on state owned water bottoms; to provide terms, conditions, and requirements; and to provide for related matters. The amended SB200 would have been just for 5 years until more research is done on the safety of natural gas salt dome storage caverns. SB200 would also have protected the 5 parishes that use the Chicot aquifer, our only fresh water source.

    AGL will not do an Environmental Impact Statement

    AGL Resources, Jefferson Island Storage & Hub, LLC, will not do an Environmental Impact Statement nor will they give the Seismic Study that was done to Save Lake Peigneur. Jefferson Island Storage & Hub, LLC employs 10 people and will hire one more after the expansion.

    Senator Adley came before the senate microphone and stood before Senator Mills, and told Sen. Mills that he was playing games. Adley again and again brought up the disaster at Lake Peigneur in 1980, as if that disaster was nothing. Senator Adley told Senator Mills that he appreciated his problems. I wonder if Senator Adley appreciates what has happened to the people that live in Assumption parish.

    Sen. Adley voted against SB200 on May 7 and 21. He ran a company that managed natural gas. In and Advocate article Sen. Adley stated that “I reached out to lobbyist friends I’ve known for years and said people need to be reasonable”. Senator Adley must have reached out to a lot of his lobbyist friends, as there were 20 lobbyists there for AGL Resources. Someone said the senate floor looked like an oil and gas convention.

    Do lobbyists run our state? Why didn’t the DNR protect the people in Assumption parish? Why don’t most of the senators protect or care about the people that live around natural gas storage caverns?

    To the Senators who voted and did the right thing thank you so much for caring about people’s lives. Save Lake Peigneur does not have lobbyists or money. The people that live in that area are hardworking people and so many work in the oil and gas industry but they are trying to protect their lives.

    Senator Guillory, St. Martinville, was on the Senate Floor 5/21/2013 but did not vote on either days.With a few hours notice we gathered 10 residents and Kathy Wascom, our lobbyist from LEAN to support our bill.

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    AGL had an estimated 20 lobbyists of extremely well-paid lobbyists.

    Although we lost by a mere 2 votes, ordinary citizens battled against the extremely experienced lobbyists. In that sense we did not lose.

    Lake Peigneur

    As always, Senator Mills was outstanding, in fact I was pleased to hear one of the lobbyists complain that his persistence and commitment was annoying.

    We continue to applaud his integrity. We are also very grateful to the support we received from the 17 senators who supported SB200, including Senator Perry and Senator Cortez. Senator Guillory from St. Martinville remained absent although the parish government and law enforcement officials were staunch in their support of SB200.

    The purpose of the bill was to stop the permitting process for at least 5 years to give time to truly study the numerous issues of concern; bubbling in the lake, contamination of the Chicot Aquifer, property devaluation and geological anomalies.

    The state’s policies failed the residents of Bayou Corne. After nine months there is no resolution. SB200 would have assured clear unbiased solution. The 19 senators who voted against SB200 have gambled with the lives of 4000 Lake Peigneur residents as well as the drinking water for numerous parishes from the Chicot Aquifer.

    Eight years have passed since AGL Resources began their quest to create additional caverns in Lake Peigneur. The Bayou Corne disaster and today’s loss has made us more determined to protect our homes and environment.

    Lake Peigneur bill defeated in Senate.

    Lake Peigneur bill defeated in Senate Right click and click view to enlarge

    For his initial pitch on legislation aimed at curtailing oil and gas activity at Lake Peigneur, state Sen. Fred Mills turned the Senate chamber into a movie theater.

    Mills, R-St. Martinville, showed grainy, decades-old news footage of the water draining in a violent whirlpool after a drilling accident in 1980.

    The images failed to convince the state Senate to embrace Mills’ Senate Bill 200 to stop the expansion of natural gas storage underneath the lake.

    Mills made another attempt Tuesday, this time relying on his own words. He asked legislators to side with the lake’s residents instead of the dozen lobbyists hired by the “oil and gas boys.”

    The result was the same.

    The Senate rejected SB200 with 17 members voting in favor of it and 19 voting against it. The bill needed 20 favorable votes to advance to the House.

    At issue is the Atlanta-based AGL Resources’ plans to expand an underground natural gas storage operation in the salt dome beneath Lake Peigneur, which straddles Vermilion and Iberia parishes.

    Residents oppose the expansion because of concerns that instability in the salt dome could result in a catastrophe similar to the 15.1-acre sinkhole that forced some Bayou Corne residents out of their homes in Assumption Parish.

    The expansion would occur more than three decades after a drilling rig pushed through the top of the salt mine and punched a hole in the bottom of Lake Peigneur. The lake drained in a whirlpool that also sucked in barges.

    AGL has been trying to expand its operation at Lake Peigneur for years. Then-Gov. Kathleen Blanco called for an extensive environmental study in 2006, sparking a lawsuit that resulted in an agreement for additional safeguards. The company still needs two additional permits to start the expansion. Mills’ bill initially would have prevented the expansion from taking place.

    AGL offered residents a compromise.

    After the legislation failed in a floor vote earlier this month, AGL offered residents a compromise. The company said it would put expansion plans on hold for a year and work with the state Department of Natural Resources to determine whether foaming on the lake’s surface stems from instability in the salt dome.

    Save Lake Peigneur’s board of directors rejected AGL’s offer Monday night. The group, which represents the lake’s 4,000 residents, determined the offer was not in members’ best interest. Nara Crowley, president of Save Lake Peigneur, said residents want a federal environmental impact statement, a scientific ultrasound of the salt dome and a clear determination on what is causing the foaming.

    “Bayou Corne’s disaster is a result of failed regulations of the state of Louisiana. We will never feel safe until all our questions are answered,” Crowley said. Duane A. Bourne, spokesman for AGL, said it is disappointing that residents rejected the company’s proposal. “The sole purpose of the SB200 legislation is to unfairly deny AGL Resources the opportunity to go through the regulatory process in a fair and equitable manner — we are just seeking the same right that other similar companies in the state have received,” Bourne said by email.

    With the residents urging him to push forward with SB200, Mills amended the bill Tuesday to call for a five-year halt in natural gas storage expansion at the lake. “All we’re saying is we want a five-year break, and for a company called AGL in Atlanta I think it’s OK,” Mills said. State Sen. Rick Ward III, who represents Bayou Corne, urged his colleagues to embrace the bill. Ward, D-Maringouin, said Mills just wants to take care of his community. “I don’t make a habit of getting up and speaking on other people’s bills, but I have to rise in support of this one,” he said.

    State Sen. Robert Adley, R-Benton, said he had several problems with the bill. The biggest issue, he said, is that the bill would not prevent the type of drilling that caused the 1980 accident. “If you want to fix the problem, face the problem straight up,” Adley said. Mills thanked Adley, who lives in north Louisiana, for caring about the people of Iberia and Vermilion parishes. He said the bill would help residents even if there are structural flaws in the language.

    “Since Bayou Corne, they’re scared,” Mills said. With the session ending June 6, Mills is short on time to rally legislators to his cause.

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    Click Here For Lake Peigneur Part One: Video – Lake Peigneur could be worse than Assumption sinkhole
    Click Here For Lake Peigneur Part Two: Largest man-made vortex – Lake Peigneur update – special report.
    Click Here For Grand Bayou sinkhole begins Part One: Bayou Corne – Grand Bayou sinkhole begins – can it end?
    Click Here For Grand Bayou sinkhole begins Part Two: 06/28/13–05/16/13–facts about Grand Bayou sink hole.

    Millions of celebrities have joined Matt Damon’s “Toilet Strike” protesting the lack of access to safe water and adequate sanitation for billions. Just today, innovative entrepreneur Richard Branson, rockstar-philanthropist Bono, and actress Olivia Wilde have made their own support public.

    Richard Branson – Water crisis – How do we save the water?

    WHOLE WORLD Water seeks to prove that economic, social, and environmental progress are not mutually exclusive. Developed to end the global water and sanitation crisis, WHOLE WORLD Water works to engage the hospitality and tourism industry to filter, bottle, and sell its own water, and contribute 10% of the proceeds to the WHOLE WORLD Water Fund. 100% of the proceeds will go directly to clean and safe water initiatives worldwide.
    We believe that everyone should have access to clean and safe water. Visit Sir Richard Branson

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    USA Water crisis: Bayou Corne and Grand Bayou sinkhole – Special water education edition part 2 of 3 History and video timeline – June 28, 2012 – May 16, 2013 – the facts about Grand Bayou sink hole.

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    USA: Bayou Corne and Grand Bayou sinkhole history

    USA Water crisis  Bayou Corne and Grand Bayou sinkhole

    Grand Bayou sink hole history timeline.

    Bubbles in Grand Bayou June of 2012 courtesy of WBRZRight click and click view image to enlarge

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    Introduction: Part 2 of 3: Bayou Corne – Grand Bayou sinkhole series May 17, 2013 / Anthony Kozuh Research Director / STW™

    Part two of this Save the Water™ special water education edition chronologically covers the history and timeline facts of the Bayou Corne – Grand Bayou sinkhole, beginning two months prior the actual collapse on August 3, 2012 until May 16, 2013. The videos within this report will assist you in visualizing the actual magnitude of this situation and I personally recommend to view these videos as pictures speak more than words. [ Click full screen: videos will be in high definition ]

    Part three: 05/18/2013 will consist of scientific facts regarding sink holes, videos, and material to assist you in further research of the Bayou Corne – Grand Bayou environmental – water crisis. We wish to thank WBRZ , TheAdvocate.com and WWLTV.com for the detailed coverage they have provided since the outset of this water crisis.

    Click Here For Lake Peigneur Part One: Video – Lake Peigneur could be worse than Assumption sinkhole
    Click Here For Lake Peigneur Part Two: Largest man-made vortex – Lake Peigneur update – special report.
    Click Here For Grand Bayou sinkhole begins Part One: Bayou Corne – Grand Bayou sinkhole begins – can it end?

    The beginning: June 27,2012 – Bubbles in bayou raise concerns.

    Jun 28, 2012 / Adrian Pittman / Education timeline courtesy of WBRZ..read more /see Video

    PIERRE PART – Assumption Parish authorities are holding a meeting to discuss a natural gas leak causing bubbles in Bayou Corne and Grand Bayou.

    For seven years, Shelly Hernandez has called Bayou Corne home. “I really love the area, it was very peaceful until we started having gas bubbling,” she said. For weeks now they’ve been blistering the surface of Bayou Corne and Grand Bayou, leaving residents living on these bayous concerned. “This is not an accident, this is something that’s been caused by someone,” said resident Randy Rousseau. But no one seems to know who. One thing parish officials do know is that the bubbles are caused by a natural gas leak. “It’s the fear of the unknown… we been seeing it, and wondered about it, and knew it wasn’t natural,” Rousseau said.

    The parish Office of Homeland Security and Emergency Preparedness is investigating the leak. Officials say there’s no serious risk of it catching fire. “There’s been no readings to show flamability of the product coming from bubbles, as of right now, no water ways or any evacuations have happened,” said parish OHSEP Manager John Boudreaux. But Rousseau says he’s not waiting around for that to happen. “I have a house and business in Grand Bayou, I don’t live there anymore. I bought other property, my wife and I didn’t feel safe,” he said.

    Residents living in Bayou Corne are on edge.

    Jul 13, 2012/ Adrian Pittman / Education timeline courtesy of WBRZ..read more

    BELLE ROSE- Residents living on Bayou Corne, in Assumption Parish, are living with fear, because of the uncertainty of a natural gas leaks, that’s boiling to the top of the bayou. Today, USGS will be installing seismic monitors in the area where the bubbles are appearing.

    Gas bubbles continue in Bayou Corne.

    Jul 18, 2012 / Education timeline courtesy of WBRZ..read more

    NAPOLEONVILLE – Analysts pulled gas samples today from the bubbling Bayou Corne and Grand Bayou areas in their continuing search to find out what’s causing them. The Department of Environmental Quality and Department of Natural Resources have been in the area since July 14 trying to determine the source of the gas bubbles. A spokesperson said samples taken today were intended to validate samples the teams had already pulled from the area. The U. S. Geological Survey encouraged people living in the area to continue to report any tremors felt in the community to the Assumption Parish Office of Homeland Security and Emergency Preparedness, either online or by calling (985) 369-7386.

    Abandoned well could be source of gas leak.

    Jul 25, 2012 / Adrian Pittman / Education timeline courtesy of WBRZ..read more / Photos / Video

    BELLE ROSE – Assumption Parish officials believe an abandon well leaking natural gas could be what’s causing bubbles on Bayou Corne and Grand Bayou.

    A resident came across the abandoned well two days ago off La. 70, in a swamp near Bayou Corne. Officials said the well is leaking flammable natural gas, but the chance of any ignition is 35 percent. Although a lot of fingers point to this well as the cause for the bubbling bayou, officials still aren’t saying the mystery’s solved. “We have to check and try and determine what is the source of the gas that is bubbling in Bayou Corne and Grand Bayou, if this is related to one larger incident,” said Assumption Parish Emergency Preparedness manager John Boudreaux. Residents said at this point, they don’t know what to believe. “I’m not a scientist, I’m not an engineer, I don’t know any of this stuff, I’m just having to take people at their word for it. But we feel like we’re not getting enough real concrete answers to make us feel safe,” said Bucky Mistretta. Engineers plan to excavate around the well on Thursday to see if it really is the really problem.

    Sinkhole appears in bubbling swamp.

    Grand Bayou sinkhole 200 feet by 200 feet

    Aug 3, 2012 / Russell Jones / Education timeline courtesy of WBRZ..read more

    BAYOU CORNE – A sinkhole formed overnight in an area of Assumption Parish swamps that have been bubbling for several weeks now.

    John Boudreaux, the director of the parish office of emergency preparedness, said the sinkhole measured about 200 feet by 200 feet and several trees had fallen into it. He said the sinkhole is on private land near the Texas Brine Co. LLC facility, near the areas of Bayou Corne and Grand Bayou which have been the site of unexplained gas bubbles for some time. Boudreaux said they will bring in a helicopter from Alexandria later today to get a better look at the sinkhole. Federal and state officials have been in the area searching for the cause of the bubbling and reported tremors in the area, but have not narrowed down a cause for the phenomena yet.

    “Sinkhole” now “slurry area” in bayou.

    Aug 3, 2012 / Russell Jones / Education timeline courtesy of WBRZ..read more

    BAYOU CORNE – Parish officials are now calling what they initially said was a “sinkhole” a “slurry area” near bubbling bayous in Assumption Parish.

    According to a press people in Bayou Corne reported a strong diesel smell this morning. Shortly after that authorities identified a “slurry area” where several trees had collapsed in a swamp area between Grand Bayou and Bayou Corne. State Police and parish emergency officials will fly over the site this afternoon to see if there are any other slurry areas. Other agencies will continue to monitor for any other slurry sites or expansion of the existing area. Bayou Corne and Grand Bayou have been the site of gas bubbling for the past few weeks, as well as tremors reported by people living in the area. So far no definite cause for the bubbling or tremors has been identified.

    Officials say diesel found in liquefied swampland.

    Aug 6, 2012 / Education timeline courtesy of WBRZ..read more

    BATON ROUGE – State officials say preliminary slurry water samples pulled from the acre of swampland that liquefied into muck over the weekend indicate the presence of small amounts of diesel hydrocarbons.

    The pond of muck, located in Assumption Parish, first appeared Friday night and grew quickly, bending a 36-inch natural gas pipeline buried 16 feet in the ground as the muck expanded. About 150 homes and several businesses were ordered to evacuate after Gov. Bobby Jindal declared a state of emergency for the parish when the slurry area appeared to be expanding. The Louisiana Department of Environmental Quality says it has not determined where diesel may be coming from. They plan to take more tests. Meanwhile parish officials say the size of the slurry hole has not changed since Sunday.

    Hundreds evacuate while agencies monitor sinkhole.

    Aug 6, 2012 / Adrian Pittman / Education timeline courtesy of WBRZ..read more

    Assumption Parish Flyover 11/14/12

    ASSUMPTION PARISH – Nearly 200 people left the Bayou Corne and Grand Bayou area after a sinkhole caused officials to order a mandatory evacuation.

    The massive sinkhole, the size of a football field, is located about 2,000 feet behind Shelly Hernandez’s house. “We don’t know what’s going to happen. I feared this all along: something sinking, something blowing up,” Hernandez said. That concern has officials on high alert. Today diesel was found in the area, which officials believe is coming from an inactive cavern on the property of Texas Brine. The Houston-based company brought in geologists and geo-mechanical experts today to begin examining the inactive mine cavern, and see if it is the cause of the sinkhole and the mysterious natural gas bubbles recently found in the two bayous.

    Parish officials are monitoring the area to make sure the diesel doesn’t reach a level where it could possibly ignite. “Air monitors that monitor the community have not shown any danger levels that would affect anything, but it is definitely there,” said emergency preparedness director John Boudreaux. But what’s behind all of this, is still up in the air. “Still fear of unknown,” said Hernandez, “because nobody knows anything.” Officials scheduled a community meeting Tuesday evening to brief the public about what they’ve found so far. The meeting is set for Aug. 7 at 6:30 p.m. at the St. Joseph the Worker Catholic Church Hall in Pierre Part, located on Highway 70. See Photos Video

    Scientists to examine sinkhole.

    Adrian Pittman: BAYOU CORNE – The company which owns land a massive sinkhole appeared on sent in experts today to see if they could connect it to bubbles that had been popping up in the nearby Assumption Parish bayous. A mandatory evacuation is still in affect for people living near Bayou Corne and Grand Bayou after the massive sinkhole was discovered. Parish officials are monitoring the area on Texas Brine’s 40-acre facility south of La. 70, and as of now it hasn’t grown. The Houston-based company is bringing in geologists and geo-mechanical experts today to begin examining an inactive salt mine cavern to see if it is the cause of the sinkhole and the mysterious natural gas bubbles recently found in the two bayous.

    Meeting set to brief community on sinkhole

    Aug 6, 2012 / Trey Schmaltz / Education timeline courtesy of WBRZ..read more

    BAYOU CORNE- Assumption Parish, State, and facility owners will meet with people who live near a sinkhole that developed Friday. The sinkhole may be caused by a failure in a brine cavern inside a salt dome. The sinkhole is connected with some bubbles that appeared in Bayou Corne earlier this summer. The meeting is set for Tuesday, August 7, 2012, at 6:30 p.m. at the St. Joseph the Worker Catholic Church Hall in Pierre Part, located on Highway 70.

    When the ground collapsed it also damaged a pipeline. Because of that, Highway 70 was closed- and remains closed- it may open overnight. The line is being depressurized. Friday night, people who live near the sinkhole were evacuated. A shelter at Belle Rose Middle School was opened.

    State: salt dome, mining operation failure likely cause of sinkhole and bubbles

    Trey Schmaltz: BATON ROUGE- State experts now think a failed salt dome, or mining operation, in Assumption Parish led to a sinkhole Friday and is also connected to a bubbling phenomenon in Bayou Corne as well as tremors in the area. “Through consultation with all the scientists involved, DNR has determined that the potential failure of a portion of an inactive salt-mining cavern near the area … is a likely cause of the occurrence and possibly the recent natural gas bubbling,” the state said in a news release late Friday.

    The sinkhole developed sometime early Friday morning

    The sinkhole developed sometime early Friday morning, a mandatory evacuation order was issued for the people who live near it about 16 hours later. “The Office of Conservation has issued an emergency order requiring a brine solution company to take steps to evaluate the structural integrity of one its inactive salt caverns,” the Louisiana Department of Natural Resources said. According to DNR, state leaders have been in contact with the company, and Texas Brine has “indicated that it intends to cooperate fully to evaluate the status of its cavern and take action to address any potential failure in structural integrity.” The bubbles are a natural gas mixture, and air monitoring is taking place. No unsafe air-related pollutants were found. The bubbles began about two months ago, followed by earthquakes, then the sinkhole on Friday. People in the area were asked to leave Friday night, a shelter was established at a school.

    Cavern described.

    Trey Schmaltz: BATON ROUGE- A representative for Texas Brine described what’s under Bayou Corne as a vase, where brine – a mixture of water and salt- is extracted from salt domes and used in various compounds. Under Bayou Corne, a cavern was created in a salt dome- nearly a mile under ground.

    The operation was running for twenty years before it was shuttered three years ago. Now, a brine mixture fills the cavern where salt once formed. Company leaders aren’t sure what’s caused a sinkhole or bubbles in the area. But, Friday night, experts with the state blamed a possible failure in the salt dome. It had been described as a “stable formation” by a company representative, now they’re looking to see what issues, if any, there are with the cavern. The cavern is large enough to hold millions of barrels of the brine mixture. Texas Brine operates as many as four other similar operations in the Assumption Parish area- those are active.

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    Natl. Guard reports sinkhole grew overnight.

    Aug 9, 2012 / Russell Jones / Assumption Parish Police Jury /Education timeline courtesy of WBRZ..read more

    BAYOU CORNE – Authorities in Assumption Parish reported that the slurry area near Bayou Corne grew overnight.

    The National Guard took infared readings by helicopter overnight, and observed the sinkhole grew by 10 to 20 feet from north to south. Earlier today authorities said they were taking readings for naturally-ocurring radiation in the area of the sinkhole, which may have been left over from oil and gas exploration in the area. They said additional monitoring near bubbling areas of the bayou detected no radiation. A state Department of Environmental Quality Mobile Lab arrived on site today to check air quality levels in the Bayou Corne and Grand Bayou communities. A mandatory evacuation order for residents in the Bayou Corne community remains in effect. Click here for more updates from the Assumption Parish Police Jury’s blog about the sinkhole.

    Residents near sinkhole voice relief well concerns

    Aug 14, 2012 / Adrian Pittman / Education timeline courtesy of WBRZ..read more / PhotosVideo

    ASSUMPTION PARISH – A company that owns an operation blamed for a massive sinkhole in Assumption Parish is expected to begin drilling an exploratory well by the end of the weekend.

    The well drilled by Texas Brine LLC, will investigate a salt cavern experts believe is behind a massive sinkhole and mysterious bubbles in Bayou Corne. Neighbors are concerned about the risks that could come with drilling, including the possibility it could collapse the salt dome cavern. The nearest neighbor is about 25,000 feet from the site of the relief-well. Experts say at this point, they don’t anticipate risks but residents say they’re not taking any chances. “We’re going to have to leave. There’s too many ifs, and I can’t live with ifs. Because one of those ifs could put me on the other side of the grass,” says Duane Bier. Parts of the rig will start arriving tomorrow from Lafayette. The rig will be installed by layers, and once complete, it will be about 14 stories high.

    Sinkhole swallows boat – workers rescued.

    Aug 16, 2012/ Russell Jones / Education timeline courtesy of WBRZ..read more

    BAYOU CORNE – Emergency personnel rescued two workers who were cleaning up a portion of the Assumption Parish sinkhole when their boat was caught in it.

    The Assumption Parish Police Jury said the workers were on the southwest side of the sinkhole when 50 feet of land collapsed into it, trapping their boat. The workers had to be rescued by an airboat, and shortly afterward the boat they were originally in was swallowed by the sinkhole. Authorities said all workers have been accounted for and no injuries were reported. Cleanup operations near the sinkhole have been suspended as a precaution. Crews with Texas Brine LLC are building a drilling rig to get into a salt cavern near the sinkhole to learn more about what caused it. The sinkhole appeared more than a week ago and has continued to grow as land surrounding it breaks off into the slurry area. Health and environmental monitors in the area haven’t found any health threats from the sinkhole, or bubbling that continues in the surrounding bayous.

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    Texas Brine offers residents checks.

    Texas Brine Co. LLC suspended cleanup work at a large sinkhole in northern Assumption Parish after the southwestern edge of the slurry area collapsed Thursday morning, company and parish officials said.

    Two workers with Texas Brine’s cleanup contractor, Clean Harbors of Norwell, Mass., were rescued from their small aluminum boat by a co-worker in an airboat shortly before the workers’ boat sank into the sinkhole along with the collapsing earth, the officials said. Assumption Parish Sheriff Mike Waguespack said the boat was tied to a leaning tree on the shoreline. The workers saw the tree begin to move and managed to get out the way, escaping with their equipment at about 8:30 a.m., the officials said.

    Waguespack said an area of earth collapsed

    that extended from the shoreline to about 50 feet inland. The sheriff said bubbling in the sinkhole intensified after the collapse. The sinkhole was discovered Aug. 3 about 200 feet from the well pad of a plugged and abandoned Texas Brine salt cavern in an area between Bayou Corne and Grand Bayou and south of La. 70 South. The collapse Thursday was on the well pad side of the sinkhole.

    Louisiana Department of Natural Resources scientists suspect the cavern failed, released its brine contents and caused the sinkhole, which swallowed up forested swamps. A mandatory evacuation order has remained in place since the evening of Aug. 3 for the Bayou Corne and Grand Bayou areas. Parish officials have said the order affects about 150 residences.

    DNR officials have ordered Texas Brine of Houston to drill a relief well to get a better understanding of what is happening with the cavern, a process that could take at least 40 days. Other developments also emerged from news statements Thursday and in recent interviews:

    Texas Brine Co. LLC contractor Worley Catastrophe Response will begin distributing weekly housing assistance checks for $875 at 10:30 a.m. Friday at the Sheriff’s Office substation, 4024 La. 70 S., Pierre Part, to households affected by the evacuation order.

    DNR and Louisiana Department of Environmental Quality officials said Thursday that a Crosstex Energy LP of Dallas salt cavern containing 940,000 barrels of liquid butane poses “little to no threat” to populations near the slurry hole.

    Sonny Cranch, Texas Brine spokesman, said company officials expected that the edges of the sinkhole would continue gradually to fall in, or slough off, making the sinkhole bigger and shallower. In an updated estimate of the hole’s size Wednesday evening — before the Thursday collapse — state officials said the sinkhole was expanding at the edges, though still much smaller than the maximum size estimated by DNR scientists.

    The statement said the sinkhole was 476 feet from the northeast to the southwest sides and 640 feet from the northwest to the southeast. “This natural growth of the sinkhole was expected and could continue,” the Wednesday statement said.

    On Thursday after the collapse, Cranch said company officials will re-evaluate the sinkhole Monday to see if it has stabilized and will deploy more oil retardant boom. “But (workers) will not continue physical cleanup activities until they evaluate the sinkhole on Monday,” he said.

    Workers with Clean Harbors have been collecting vegetation floating in the sinkhole in preparation for vacuuming diesel on the water’s surface. Cranch said the cleanup will move forward even though the sloughing process is continuing. “We’re not ready to abandon efforts to clean up the sinkhole at this time,” Cranch said. “We think that work can continue and continue safely as the sinkhole continues to stabilize.”

    Despite the setback on cleanup, Cranch said the delivery of drilling rig parts to Texas Brine’s facility continued Thursday and assembly is underway. Drilling work could start late Friday or early Saturday, Cranch said. Worley Catastrophe Response, which will coordinate and manage the “Bayou Corne Incident Evacuee Fund” for Texas Brine, plans to issue checks to the representative of each household affected by the evacuation order, Texas Brine officials said.

    The representative will have to display a Louisiana driver’s license or “other reasonably acceptable photo identification confirming residence in the evacuation zone,” company officials said in a news release. The original permit for the Texas Brine cavern requires the operator to provide assistance to residents in areas deemed to be at immediate potential risk, state officials have said. The requirement is triggered in the event of a sinkhole and evacuation, state officials said. Crosstex also submitted a revised worst-case scenario analysis in its risk management plan Wednesday at the request of DEQ Secretary Peggy Hatch. In a statement Thursday, DEQ officials noted that the cavern, which is a half-mile underground and far below the bottom of the sinkhole, cannot release its liquid butane contents without water being pumped into the cavern to push out the butane. The butane is also being held in the absence of oxygen.

    “While it is easy to simply convert the known quantity of butane into a blast scenario, that does not mean this scenario is possible,” DEQ officials said in a statement. Crosstex’s other nearby cavern, which has the capacity to hold 1.7 million barrels, has no hydrocarbons inside and is filled with brine at present, company officials said in their letter. The sinkhole’s emergence followed more than two months of earth tremors and mysterious natural gas releases in Bayou Corne, Grand Bayou and water wells.

    The gas bubbling has continued since the sinkhole emerged. Tremors ceased the day before the sinkhole was found. The Texas Brine salt cavern was carved out of the 1-mile by 3-mile Napoleonville Dome, a large underground salt deposit. The cavern, which was used to produce brine for industry and never for natural gas storage, was plugged and abandoned in June 2011 after company officials ran into trouble trying to expand the cavern.

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    Cavern damaged – now crews have to figure out what happened.

    Sep 25, 2012 / Trey Schmaltz / Education timeline courtesy of WBRZ..read more

    BAYOU CORNE- Scientists discovered a salt brine cavern, deep under Assumption Parish, has been damaged. Seismic activity in the area is blamed.

    The Louisiana Sinkhole Bugle

    “The cavern damage was caused by an external source,” a spokesperson for Texas Brine said in a news release late Monday. Texas Brine operated a brine operation in the Bayou Corne/ Grand Bayou area years ago. Caverns were created inside a salt dome, deep underground to extract brine. In May, people began reporting tremors and bubbles in the bayous. Over the summer, ground subsided and created a sinkhole. Since then, crews have been trying to determine the cause- and what can be done to fix the situation.

    “The tool used to measure cavern depth bottomed out at approximately 4,000 feet – a point estimated to be 1,300 feet higher than the floor had been measured prior to the cavern closure in 2011,” a representative of Texas Brine reported. “This preliminary finding indicates that some type of dense material has fallen to the bottom of the cavern. A sample of the material has been retrieved from the cavern floor and will be analyzed.” That material is described as abnormal, compared to what should be found in the sealed cavern. “Sonar inspection that is currently being conducted will provide a more detailed image of the cavern’s interior conditions and the possible source of the material at its base.” An entire community was evacuated, and still is not allowed to return.

    Residents angry as Assumption sinkhole continues collapsing.

    February 25, 2013 / wwltv.com / Katie Moore / Eyewitness News

    Related: News articles WWLTV
    Work halted at Assumption Parish sinkhole site
    Assumption Parish sinkhole swallows another 25 trees
    Jindal visiting sinkhole area for first time
    State leaders say company has promised to negotiate buyouts over sinkhole
    Jindal meets with parish officials over sinkhole, will visit next week
    Work at Assumption sinkhole suspended after increase in seismic activity

    BAYOU CORNE, La. — The Assumption Parish sinkhole is a lot like a living, breathing thing. More than 200 days after it mysteriously started swallowing up the swamp, hundreds of residents are still under a mandatory evacuation order.

    Geophysicists say the cavern that caused the sinkhole at the surface is still collapsing, leaving Bayou Corne residents wondering if there will ever be an end in sight. Bayou Corne has always been a peaceful place. Spanish moss dangles from the trees and inlets that lead to Grand Bayou are intertwined with the streets like a braid. Most of the homes are situated with a bit of the bayou in their backyards, and that’s exactly why most residents called the area home.

    We could drop the boat right there to go fishing

    “We could drop the boat right there to go fishing. It was just like a paradise,” said former Bayou Corne resident Jamie Weber. Weber decided to move hear family out last fall. A sign on her old home says “Evaucated: Thank you Texas Brine.” She had no idea that she was putting her mobile home on land on top of an underground salt dome. The Napoleon Salt Dome is full of caverns that have been mined to make brine, or salt water. Other caverns on the dome have been used to store hazardous, potentially explosive gasses, like Butane.

    Geophyisicists now say the western side of one of the brine caverns is collapsing, filling in from deep in the Earth, causing the sinkhole at the surface to expand and contract. “On Oct. 25, we moved out of our home when we finally found a rent house because they had put a vent well a hundred yards from my house,” Weber told a joint legislative committee at a hearing on the sinkhole at the State Capitol last week.

    She and some of the 350 evacuated Bayou Corne residents packed the Baton Rouge hearing looking for answers. Many of the ones they keep getting are conflicting and confusing, especially from the state and the company that once mined the collapsing salt cavern Texas Brine. “The cause of the sinkhole is the subject of pending litigation. At this point, I don’t think it’s proper to have any discussion about what the cause is and whether we accept what anyone has said regarding the cause of the sinkhole,” Troy Charpentier, an attorney for Texas Brine, told the committee.

    The secretary of the Louisiana Department of Natural Resources flat-out testified at the same hearing, “The cavern collapse led to the sinkhole and created a path for the natural gas to come to the surface.” But Secretary Stephen Chustz slipped out a backdoor, with his press secretary only offering an interview with himself after the hearing without giving us the chance to ask him any questions.

    One of those questions: What caused the cavern to collapse?

    “The sinkhole is constantly changing. It changes every time we go out there. Not just on the surface, but in the sub-surface,” said Gary Hecox, a hydrogeologist with CB&I, formerly the Shaw Group, who is a consultant for the state about how to best handle the sinkhole. He said it’s uncharted territory.

    “The cavern was 3,400 feet deep, which is deeper than any known cavern failure impacting the surface in the international record,” Hecox said. Nowhere in the world has a brine cavern this large collapsed, and Hecox said the data shows it’s not finished yet. “We still have 450 feet to fill. How long is it gonna take to fill this up? At one foot per day, we’re still looking at an event that’s gonna run over a year,” he said.

    Every time it shifts, recently installed seismic monitors pick up tremors like little earthquakes. When it does, big bubbles of natural gas, vegetation and crude oil are released to the surface. They call it a “burp”. “It appears that the sand and gravel that’s in the bottom of the sinkhole breaks up a large gas bubble into many small bubbles just like an aquarium,” Hecox continued, “That is a good thing. Because if you get a single bubble up and have an ignition source you can have a flash over.”

    A flash over is an explosion, like the kind you can see if you leave the gas on too long before lighting a propane grill. But Hecox said a large natural gas bubble from the sinkhole lit by any ignition source could mean major damage on the surface. Instead those little bubbles are coming out all around the actual sinkhole site in the form of bubble sites in the bayou. Twenty new bubble sites have been spotted in the last month.

    Nine months after the first ones surfaced, Texas Brine started installing vent wells to alleviate the pressure underground. A drive down Hwy. 70 will show you several of them burning around Bayou Corne. “We continue to install relief wells as fast as we can and will continue to do so as they continue to be effective,” said Bruce Martin, vice president of Texas Brine. But in recent weeks, some of the residents who stayed behind, and are living in the area at their own risk, noticed some problems that are typically invisible to the naked eye.

    Bubble sites popped up in neighborhoods that are typically dry during flooding after a recent rain storm. It caused Wilma Subra, a chemist with the Louisiana Environmental Action Network, to raise a red flag with the Louisiana Department of Environmental Quality. “A house acts like a tent. So, if it’s migrating up through the soil, and it’s being caught in the house, it’s building up concentrations in the house. And then if it reaches explosive level, then one little spark in the house would set it off,” Subra said.

    One of the residents who has stayed behind, Nick Romero, also testified before the legislative committee. He now has five DEQ monitors installed in his house to measure natural gas and other chemicals. “We have had our grand kids and now we can’t. I love to fish. And now I don’t want to,” he told the committee members, choking back tears. The residents are struggling not just with the instability underground, but in their lives.

    “Once they told us that they wanted to put monitors in our house and that we’d have to live like, to me, like lab rats, to me, that was no way for my kids to grow,” Weber said. Many feel forgotten, Weber said. Especially by Gov. Bobby Jindal. The governor has yet to visit the sinkhole site or publicly talk about it.

    “He’s promoting plants around the area, chemical plants. And he was in the area and he wouldn’t, still to this day does not acknowledge it,” Weber said. In October and November of 2012, Jindal announced two chemical plant expansions a few miles from Bayou Corne, one in nearby Geismar and one in Donaldsonville.

    But in six months, he’s made no visit to the sinkhole site.

    “Where is he? Where is Jindal? He’s all over the United States, but he can’t come forty minutes south of Baton Rouge and visit,” Weber asked. As photos from the Louisiana Environmental Action Network show, when the sinkhole first appeared, it was just 400 feet in diameter. As of mid-February, it had swallowed nine acres. Scientists say the worst-case scenario is it could swallow 40 acres.

    Even if it does, many, like Weber, are now just hoping Texas Brine will buy them out so they can move on. The company told residents that they are working to stabilize the area before tackling buy outs because some residents are still hoping to return. Lawmakers are planning another joint hearing on the sinkhole March 18. Katie Moore / Email: kmoore@wwltv.com / Twitter: @katiecmoore

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    Water still pouring through three breaches of Assumption sinkhole berm.

    Western Berm Breach 5-10-13

    High water driven by heavy rains poured inside a containment levee around the Assumption Parish sinkhole overnight Thursday and much of Friday, forcing workers to try to cut off the flow and to contain the hole’s brew of crude oil and brine.

    Sinkhole MapRight click on image & click view to enlarge

    Containment boom had not been laid out at that point, parish officials said. A second video shows the largest breach of all, about 75 feet across, with water levels nearly equalized between the swamps and inside the berm area, leaving an idle excavator sitting in shallow water.


    Western Berm Breach 5-10-13 Part II

    Because of problems going over wet clay on part of the berm’s southern leg, contractors worked Friday to finish the first phase of the V-shaped extension, or “bump out,” as a route to reach the largest breaches. But poor weather, including close lightning strikes, halted Texas Brine’s work Friday afternoon, Boudreaux said. The berm extension was nearly finished except for a small gap. “They can haul sand in the rain. I think their intention is to do that and finish the bump out and give good access to the bigger breaches,” he said.

    Grand Bayou Flyover 5/14/13

    Texas Brine Co. contractors plugged the final two breaches in a containment berm around the Assumption Parish sinkhole by early Tuesday after heavy rain and high water punched through the incomplete earthen barrier late last week, authorities said. With the holes plugged, Sonny Cranch, spokesman for Texas Brine, said workers resumed on Tuesday the previously planned work of building up the earthen levee surrounding the 71-acre area containing the sinkhole near the Bayou Corne community.

    The Louisiana Sinkhole Bugle

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    Water Crisis – Largest man-made vortex – Lake Peigneur update – Special report – history – facts – video – Lake Peigneur gets snubbed by Senate – Acadiana residents fear potential sinkhole ‘disaster’.

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    Lake Peigneur - Special water education report - Largest man-made vortex - history - facts - videos - Lake Peigneur gets snubbed by Senate  Acadiana residents fear potential sinkhole disaster

    Lake Peigneur gets snubbed by Senate … again.

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    Click Here For Part One: Video – Sheriff Ackal says Lake Peigneur could be worse than Assumption sinkhole

    Lake Peigneur is located in the U.S. State of Louisiana

    MAY 10, 2013 / INDReporter / Patrick Flanagan
    Right click on image and click view to enlarge

    Our state legislators have once again shown little concern for the plight of the thousands of people living near Lake Peigneur, siding once again with the interests of AGL Resources, an out-of-state company attempting to push forward expansion plans that some believe could lead to a sinkhole catastrophe similar to the one playing out at Bayou Corne — as if that wasn’t example enough.

    The example of the Bayou Corne sinkhole aside, the list of reason why Louisiana’s lawmakers should have overwhelmingly voted in favor of Senate Bill 200, authored by Sen. Fred Mills, R-Parks, is immense, and so is the support its received from the public, as well as from such entities as the Iberia Parish and Vermilion Parish governments, the City of New Iberia and the Iberia Parish Sheriff’s Office.

    Yet, when the vote was surprisingly called in the waning hours Tuesday, SB 200 failed 15 to 20. Nara Crowley, president of the nonprofit advocacy group Save Lake Peigneur, says Tuesday’s vote was unexpected, not necessarily the turnout, but how it was hurried before the Senate, and the fact that AGL somehow seemed tipped off to what was going down that day.

    AGL had 10 lobbyists working the Senate that day

    “AGL had 10 lobbyists working the Senate that day,” Crowley tells The IND. “We were given less than 12 hours notice, and were only able to get three people from our group there in time.”

    Even more disheartening, though not all too surprising based on the Legislature’s record when dealing with similar Lake Peigneur related bills in recent years, is the fact that of the eight members of the Senate Natural Resources Committee, which extensively heard all the problems AGL’s plans posed not only to Lake Peigneur, but also the Chicot Aquifer, only five voted in favor of SB 200. Those nay votes came from Sen. Gerald Long, the committee’s chair, and Sen. Jody Amedee. Sen. Norbert Chabert was a no-show.

    “We’ve had this happen so many times,” says Crowley. “We’ll think someone’s going to vote one way, but then the day comes and they don’t. We’ve gotten to the point that we just don’t expect our Legislators to do what’s right. The fact is they don’t listen to the people, especially when there’s so much outcry and it still fails. They just don’t listen to what the public has to say. Why? I’m sure there’s some gratuitous influence going on behind the scenes. Definitely.”

    This issue is nothing new to the state Legislature — the people’s fight against AGL has been ongoing since the early-1990s, when the company first dredged the lake, creating its two existing caverns. Since, the fight has centered on AGL’s push to expand those and develop two additional caverns, all at the risk of close to 4,000 people living nearby. Not only did all wildlife vacate the area for several years following the company’s first dredging excursion, but on more than 80 occasions since 2006, residents have documented strange bubbling and foaming coming from the lake’s center. The foam was tested in 2006, showing high levels of methylene chloride — a component of natural gas — yet, residents are still awaiting an explanation from AGL, not to mention the state Department of Natural Resources, which like the Legislature, seems more on the side of industry than the people it was created to protect.

    Fortunately for Crowley and other lake advocates, Sen. John Alario Jr., president of the senate, despite being among those against the legislation, did approve a request for a re-vote on SB 200, which is expected to go down sometime next week.

    “We’ll be keeping as close a watch as possible,” says Crowley. “We’re thinking it’ll happen either Monday or Tuesday.”

    The following list shows who voted for and against the bill, and those who didn’t vote at all:

    Yeas:
    Bret Allain II
    Troy E. Brown
    Page Cortez
    A.G. Crowe
    Jack Donahue
    Yvonne Dorsey-Colomb
    Dale Erdey
    David Heitmeir
    Eric LaFleur
    Fred Mills
    Jean-Paul Morrell
    Blade Morrish
    JP Perry
    Karen Carter Peterson
    Rick Ward III
    Nays:
    John Alario Jr. (Senate President)
    Robert Adley
    Jody Amedee
    Conrad Appel
    Sharon Broome
    Sherri Buffington
    Dan Claitor
    Rick Gallot
    Ronnie Johns
    Bob Kostelka
    Gerald Long
    Danny Martiny
    Edwin Murray
    Ben Nevers
    Barrow Peacock
    Neil Riser
    Gary Smith
    Gregory Tarver
    Francis Thompson
    Mike Walsworth
    Absent:
    Norby Chabert
    Elbert Guillory
    John R. Smith
    Bodi White

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    Click Here For Part One: Video – Sheriff Ackal says Lake Peigneur could be worse than Assumption sinkhole

    Timeline article: www.katc.com / May 8, 2013

    Sen. Mills ‘cautiously optimistic’ over Lake Peigneur bill’s chances.

    May 8, 2013 / www.katc.com

    The Louisiana State Senate failed to pass a bill that would require an environmental impact study before a salt cavern expansion under Lake Peigneur, but the bill’s supporters are still hopeful it will pass into law. “We fell short last night,” said Sen. Fred Mills, R-Parks, who authored SB 200. “The vote was 15 to 20. We will work to rewrite the bill to get rid of any other ramifications and try again.”

    The bill is aimed specifically to prevent AGL Resources from expanding its excavation under Lake Peigneur in Iberia Parish. Mills said he drafted the bill to protect residents from any potential threat posed by the company’s activity beneath the lake. AGL Resources is asking the state for a permit to expand the cavern to store natural gas. Several public officials, including Vermilion Parish President Nathan Granger, New Iberia Mayor Hilda Curry and Iberia Parish Sheriff Louis Ackal, added their voices to the public support for Mills bill.

    “It should come up for a rehearing newt week,” said Nara Crowley, a local activist and leader of Save Lake Peigneur, Inc. “It’s because of the letters they wrote and the work Sen. Mills has done that we are at this point.” Mills says he is looking forward to a better outcome on the bill’s next hearing in the Senate. “We got 15 votes on the first time out,” Mills said. “All we need are five more. I’m cautiously optimistic.”

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    Opponents of expanding the underground natural gas storage facility under Lake Peigneur asked state regulators on Wednesday to carefully review what they argue has the potential to become another disaster on the scale of the growing sinkhole in Assumption Parish.

    Comments at a public hearing on the project also harkened back to 1980, when a drilling rig pushed through the top of salt mine under Lake Peigneur and opened a hole that consumed the entire water body. “This lake, this region, these resources have sacrificed enough,” state Sen. Fred Mills, R-Parks, told state Department of Natural Resources officials at the hearing. “… Protect the lake. It has suffered enough.”

    Mills was joined in opposition by residents in the area, other public officials and representatives from the Sierra Club, the Louisiana Environmental Action Network and the Tulane Environmental Law Clinic. Atlanta-based AGL Resources is proposing to scour out two new salt caverns for natural gas storage at its Jefferson Island Storage & Hub Facility, expanding on the existing two storage caverns there.

    AGL has pointed to a record of no problems since the facility opened in the 1990s and maintains that the proposed expansion has been carefully studied to minimize environment impacts and ensure safe operations. The proposed expansion has met strong opposition and is now beginning its second permitting attempt. The project was halted in 2006 when then-Gov. Kathleen Blanco called for an extensive environmental study of the project.

    AGL responded with a lawsuit against the state that was settled in 2009 with some additional requirements, but not the environmental study that Blanco had sought. The permitting process is moving forward again at a time when there are near daily news reports about the problems created by a large sinkhole related to a failed salt cavern at Bayou Corne in Assumption Parish.

    “Coastal management can stop another disaster by denying this permit,” said Save Lake Peigneur President Nara Crowley, referring to DNR’s Office of Coastal Management. Crowley and other residents cited a host of potential safety and environmental concerns and pointed to the continued bubbling at the lake.

    Bubbling also was reported at Bayou Corne before the sinkhole developed there last year.

    The bubbling at Lake Peigneur has been more sporadic, but Crowley said there have been 79 documented instances of bubbling at the lake in recent years, including three in the past week. AGL Managing Director of Government Affairs Richard Hyde said in interview earlier this month that testing has not identified the precise cause of the bubbling but has confirmed that “it is not coming from our wells.”

    Crowley has questioned the thoroughness of testing done so far and said the critical issue is that there is currently no explanation for the bubbling.

    Opponents of the project have also raised concerns about how dredging for the project could impact water quality at the scenic lake and whether the up to 3 million of gallons of water a day needed to scour out the new salt caverns might draw down groundwater to the point where salt water would push in from farther south and contaminate local wells.

    “Y’all are messing with our drinking water and the places where we live,” said Iberia Parish Councilman Marty Trahan, who represents the Lake Peigneur area. AGL has maintained there would be no significant effect on water quality in the lake or in water wells. The subject of Wednesday’s public hearing was a permit for dredging work needed to bring equipment into the lake for the cavern expansion work.

    AGL needs two other state permits for the project — one to scour out caverns in the salt dome and another to use the scoured caverns for natural gas storage.

    JISH expansion opponents want bubbling source discovered first

    JISH expansion opponents want bubbling source discovered first.

    BY HOPE RURIK | THE DAILY IBERIAN | February 21, 2013

    A representative from the Jefferson Island Storage and Hub’s parent company AGL Resources gave a presentation Wednesday night at the onset of a public hearing in New Iberia Wednesday, but according to residents at the hearing, there was an important component missing.

    What is causing the bubbling on Lake Peigneur?

    “I don’t see how this agency can say this project has minimized or avoided all negative impacts without having an answer,” Lisa Jordan, supervising attorney for the Tulane Environmental Law Clinic, said. Jordan was one of two representatives from the clinic who joined more than a half dozen residents in voicing concerns regarding the company’s intent to create two additional natural gas storage caverns at the facility near Lake Peigneur.

    AGL announced its plans to create the additional caverns in 2006 and residents have been fighting the process ever since. About 50 people gathered at Willow Wood Park where residents from Erath, New Iberia and Abbeville spoke up. The public hearing was held by the Department of Natural Resources Office of Coastal Management to get input on AGL’s coastal use permit application. The application is specifically for dredging, pipelines and other infrastructure needed to access the site with equipment that could be used to create the caverns.

    There will be separate hearings on permits for the creation of the salt caverns and for the transformation of those caverns into natural gas storage facilities. Nara Crowley, Save Lake Peigneur Inc. president, said there have been 79 “bubbling events” at the lake since 2005.

    The most recent was Wednesday afternoon. The Vermilion and Iberia Parish sheriff’s offices as well as DNR were called out this morning when residents saw the lake was still bubbling. The Iberia Parish Sheriff’s Office is asking motorists to stay clear of the area until DNR and the Department of Environmental Quality assess the bubbling. Crowley said this is the first time bubbling has continued into a second day.

    Residents surrounding Lake Peigneur have long questioned the bubbling, but the disaster at Bayou Corne in nearby Assumption Parish has exacerbated concerns. “In the past, when Bayou Corne residents asked about the bubbling, the answer was, ‘It’s swamp gas,’” Gloria Conlin, of Abbeville, said. “To Lake Peigneur residents, that sounds familiar.”

    Residents also raised concerns regarding the amount of water from the Chicot Aquifer that would be needed to create the caverns. LAWCO regional manager Jim Brugh said the company knows of an arsenic plume within the aquifer east of his company’s wells in New Iberia. The company only recently developed a new well field west of the plume that it estimated the arsenic wouldn’t reach for 50 years. With accelerated draw down from AGL resources, Brugh said they couldn’t be so sure.

    “We’re very, very concerned the plume will contaminate the wells,” he said. State Sen. Fred Mills, R-Parks, questioned the need of caverns versus the impact on coastal resources. He said natural gas storage is 16 percent higher than the five-year average while, “our coastal resources are among the most valued in the nation, yet the fastest disappearing on the planet.”

    “Protect the lake,” Mills said, “she has suffered enough.”

    Patrick Courrege, DNR communications director, said the comments given during last night’s public hearing will be reviewed by permit analysts who will recommend whether or not the permit should be granted. He said the department should have a decision on the permit within 15 days.

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    Click Here For Part One: Video – Sheriff Ackal says Lake Peigneur could be worse than Assumption sinkhole

    Largest man-made vortex – Lake Peigneur sinkhole disaster.

    On 20 November, 1980, when the disaster took place, the Diamond Crystal Salt Company operated the Jefferson Island salt mine under the lake, while a Texaco oil rig drilled down from the surface of the lake searching for petroleum. Due to a miscalculation, the 14-inch (36 cm) drill bit entered the mine, starting a chain of events which at the time turned an almost 10-foot (3.0 m) deep freshwater lake into a salt water lake with a deep hole.

    It is difficult to determine exactly what occurred, as all of the evidence was destroyed or washed away in the ensuing maelstrom. One explanation is that a miscalculation by Texaco regarding their location resulted in the drill puncturing the roof of the third level of the mine. This created an opening in the bottom of the lake. The lake then drained into the hole, expanding the size of that hole as the soil and salt were washed into the mine by the rushing water, filling the enormous caverns left by the removal of salt over the years. The resultant whirlpool sucked in the drilling platform, eleven barges, many trees and 65 acres (260,000 m2) of the surrounding terrain. So much water drained into those caverns that the flow of the Delcambre Canal that usually empties the lake into Vermilion Bay was reversed, making the canal a temporary inlet. This backflow created, for a few days, the tallest waterfall ever in the state of Louisiana, at 164 feet (50 m), as the lake refilled with salt water from the Delcambre Canal and Vermilion Bay. The water downflowing into the mine caverns displaced air which erupted as compressed air and then later as 400-foot (120 m) geysers up through the mineshafts.[4]

    There were no injuries and no human lives lost. All 55 employees in the mine at the time of the accident were able to escape thanks to well-planned and rehearsed evacuation drills, while the staff of the drilling rig fled the platform before it was sucked down into the new depths of the lake, and Leonce Viator, Jr. (a local fisherman) was able to drive his small boat to the shore and get out.[4] Three dogs were reported killed, however. Days after the disaster, once the water pressure equalized, nine of the eleven sunken barges popped out of the whirlpool and refloated on the lake’s surface.

    What is Jefferson Island?

    wiseGEEK answers:

    Jefferson Island is a salt dome located in Iberia Parish, in Southern Louisiana

    Jefferson Island is a salt dome located in Iberia Parish, in Southern Louisiana. The term “Island” is a bit of a misnomer, as Jefferson Island and its nearby neighbor Avery Island are not actually islands at all, but rather protruding salt domes which stand out from the surrounding landscape. These salt domes were formed through the slow evaporation of the ocean which once covered the area, and they are a substantial natural resource.

    This island is part of a group of similar structures known collectively as the Five Islands. In addition to Avery Island, the Five Islands also include Weeks, Belle Isle, and Cote Blanche. Each of the islands sits on top of a dome of salt, and in addition to salt, the Five Islands also have rich oil and gas deposits which have been heavily exploited over the years. Because of the salt deposits present on the Five Islands, they became a fiercely defended property during the Civil War, when salt was at a premium. Avery Island, owned by the Tabasco Company, was once also used to produce cayenne peppers.

    Originally, Jefferson Island was known as Orange Island. It was purchased by actor Joseph Jefferson in 1869 for the purpose of establishing a summer home, and it was ultimately named after him. Jefferson built a mansion on the site which is now on the National Register of Historic Places; the mansion today is surrounded by sprawling gardens established by John Lyle Bayless, who purchased the Island after Jefferson’s death.

    What is a salt dome?

    wiseGEEK answers:

    A salt dome is a geologic formation caused by a phenomenon known as diapirism, in which lighter materials force their way up through denser ones. Salts and other evaporated minerals are generally lighter than the sedimentary rock which surrounds them, and as a result, salt has a tendency to well up, creating a visible bulge in the surface of the earth which is often capped with a layer of rock. Salt domes have been utilized by humans for centuries as readily available supplies of salt, since they typically contain a high concentration of halite, otherwise known as table salt.

    The formation of a salt dome takes centuries. It starts with the formation of an isolated marine inlet, which slowly evaporates, concentrating the salts. Geologists believe that these inlets must be flooded and evaporated several times to reach the concentration of salt needed to create a salt dome. Once a large deposit of salts is created, sediments are deposited over the salt as the centuries progress, but the salt will continue drifting to the top, because it is less dense than the sediments around it. As a result, the salt creates a distinctive bulge, and it appears to be boring its way through the surrounding rock when viewed in cross-section.

    What is a salt mine?

    wiseGEEK answers:

    A salt mine is an excavated area on or beneath the earth’s surface created for the purpose of extracting this sought-after mineral. This widely used crystalline mineral varies in color, and may be found in seawater or on land. It is necessary to mine salt to get to underground deposits. A salt mine has shafts for entry and exit and is typically comprised of rooms created in a checkerboard pattern. Extraction and processing includes blasting the crystals free, then crushing them several times before sending them to the surface for further processing.

    Also referred to as sodium chloride, salt is a mineral with a cubic, crystalline formation. Its color ranges from grayish to transparent or frosty white to pink, depending on its purity and mineral composition of the parent rock. It is widely used for industrial applications as well as in food.

    Salt is a very abundant mineral, and is most commonly found in seawater, making up 77 percent of dissolved solids there. Deposits on the earth’s surface are a result of the past evaporation of bodies of water. Salt deposits can also be found underground, in domes or veins among layers of sedimentary rock. In the latter cases, extraction requires the creation of a salt mine.

    Click Here For Part One: Video – Sheriff Ackal says Lake Peigneur could be worse than Assumption sinkhole

    Lake Peigneur research material by Wikipedia

    Lake Peigneur

    From Wikipedia, the free encyclopedia
    Lake Peigneur
    Location Iberia Parish, Louisiana, USA
    Coordinates 29.9808°N 91.9833°WCoordinates: 29.9808°N 91.9833°W
    Primary inflows estimated 8.47 cubic feet (0.240 m3) per second from catchment[1]
    Primary outflows unknown to Delcambre Canal
    Catchment area 10.2 square miles (26 km2) of the Vermilion-Teche Basin[1]
    Basin countries United States
    Surface area 1,125 acres (5 km2)[1]
    Average depth 3 feet (1 m)[1]
    Max. depth 200 feet (61 m)[1]

    Lake Peigneur is located in the U.S. State of Louisiana 1.2 miles (1.9 km) north of Delcambre and 9.1 miles (14.6 km) west of New Iberia, near the northernmost tip of Vermilion Bay.

    History

    The lake was a 10-foot (3 m) deep freshwater lake popular with sportsmen until an unusual man-made disaster on November 20, 1980, changed the structure of the lake and surrounding land.[2][3][1]

    Drilling disaster

    On November 20, 1980, when the disaster took place, the Diamond Crystal Salt Company operated the Jefferson Island salt mine under the lake, while a Texaco oil rig drilled down from the surface of the lake searching for petroleum. Due to a miscalculation, the 14-inch (36 cm) drill bit entered the mine, starting a chain of events which turned what was at the time an almost 10-foot (3.0 m) deep freshwater lake into a salt water lake with a deep hole.

    It is difficult to determine exactly what occurred, as all of the evidence was destroyed or washed away in the ensuing maelstrom. One explanation is that a miscalculation by Texaco regarding their location resulted in the drill puncturing the roof of the third level of the mine. This created an opening in the bottom of the lake. The lake then drained into the hole, expanding the size of that hole as the soil and salt were washed into the mine by the rushing water, filling the enormous caverns left by the removal of salt over the years. The resultant whirlpool sucked in the drilling platform, eleven barges, many trees and 65 acres (260,000 m2) of the surrounding terrain. So much water drained into those caverns that the flow of the Delcambre Canal that usually empties the lake into Vermilion Bay was reversed, making the canal a temporary inlet. This backflow created, for a few days, the tallest waterfall ever in the state of Louisiana, at 164 feet (50 m), as the lake refilled with salt water from the Delcambre Canal and Vermilion Bay. The water downflowing into the mine caverns displaced air which erupted as compressed air and then later as 400-foot (120 m) geysers up through the mineshafts.[4]

    There were no injuries and no human lives lost. All 55 employees in the mine at the time of the accident were able to escape thanks to well-planned and rehearsed evacuation drills, while the staff of the drilling rig fled the platform before it was sucked down into the new depths of the lake, and Leonce Viator, Jr. (a local fisherman) was able to drive his small boat to the shore and get out.[4] Three dogs were reported killed, however. Days after the disaster, once the water pressure equalized, nine of the eleven sunken barges popped out of the whirlpool and refloated on the lake’s surface.

    Salinity

    The lake had salt water after the event, not as a result of water entering the salt mine, but from the salt water from the Delcambre Canal and Vermilion Bay, which are naturally salt or brackish water. The event permanently affected the ecosystem of the lake by changing the lake from freshwater to saltwater and increasing the depth of part of the lake.

    Aftermath

    The drilling company, Texaco and Wilson Brothers, paid $32 million to Diamond Crystal and $12.8 million to nearby Live Oak Gardens in out-of-court settlements to compensate for the damage caused. The mine was finally closed in December 1986.[4]

    Since 1994 AGL Resources has been using Lake Peigneur’s underlying salt dome as a Storage and Hub facility for pressurized natural gas.[5][6]

    There is currently concern from local residents to the safety of storing the gas under the lake and nearby drilling operations.[7]

    See also

    References

    • Gold, Michael. “Who Pulled the Plug on Lake Peigneur?”, Science 81, November 1981, 56.

    External links

    This page was last modified on 28 February 2013 at 07:27.
    Text is available under the Creative Commons Attribution-ShareAlike License Top of page

    Richard Branson – Water crisis – How do we save the water?

    WHOLE WORLD Water seeks to prove that economic, social, and environmental progress are not mutually exclusive. Developed to end the global water and sanitation crisis, WHOLE WORLD Water works to engage the hospitality and tourism industry to filter, bottle, and sell its own water, and contribute 10% of the proceeds to the WHOLE WORLD Water Fund. 100% of the proceeds will go directly to clean and safe water initiatives worldwide.
    We believe that everyone should have access to clean and safe water. Visit Sir Richard Branson

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    Global water education: STEM – Water resource term dictionary and water infographic resource directory – teacher reference guide.

    Water Resource Terms

    Water Resource Term A

    A

    abandoned water right
    a water right which was not put to beneficial use for a number of years, generally five to seven years.
    abandoned well
    a well which is no longer used. In many places, abandoned wells must be filled with cement or concrete grout to prevent pollution of ground water bodies.
    absorption
    the uptake of water, other fluids, or dissolved chemicals by a cell or an organism (as tree roots absorb dissolved nutrients in soil).
    accretion
    a gradual increase in land area adjacent to a river.
    acid rain
    the acidic rainfall which results when rain combines with sulfur oxides emissions from combustion of fossil fuels.
    acidic
    the condition of water or soil that contains a sufficient amount of acid substances to lower the pH below 7.0.
    acre-foot
    the amount of water required to cover one acre to a depth of one foot. An acre-foot equals 325,851 gallons, or 43,560 cubic feet. A flow of 1 cubic feet per second produces 1.98 acre-feet per day.
    activated carbon adsorption
    the process of pollutants moving out of water and attaching on to activated carbon.
    adhesion
    the molecular attraction asserted between the surfaces of bodies in contact. Compare cohesion.
    adjudication
    a court proceeding to determine all rights to the use of water on a particular stream system or ground water basin.
    abandoned well
    a well which is no longer used. In many places, abandoned wells must be filled with cement or concrete grout to prevent pollution of ground water bodies.
    administrative order
    a legal document signed by U.S. EPA directing an individual, business, or other entity to take corrective action or refrain from an activity. It describes the violations and actions to be taken, and can be enforced in court. Such orders may be issued, for example, as a result of an administrative complaint ordering the respondent to pay a penalty for violations of the Clean Water Act.
    administrative order on consent
    a legal agreement signed by U.S. EPA and an individual, business, or other entity through which the violator agrees to pay for correction of Clean Water Act violations, take the required corrective or cleanup actions, or refrain from an activity. It describes the actions to be taken, may be subject to a comment period, applies to civil actions, and can be enforced in court.
    adsorption
    the adhesion of a substance to the surface of a solid or liquid. Adsorption is often used to extract pollutants by causing them to be attached to such adsorbents as activated carbon or silica gel. Hydrophobic, or water-repulsing adsorbents, are used to extract oil from waterways in oil spills.
    advanced wastewater treatment
    any treatment of sewage that goes beyond the secondary or biological water treatment stage and includes the removal of nutrients such as phosphorus and nitrogen and a high percentage of suspended solids.
    aerated lagoon
    a holding and/or treatment pond that speeds up the natural process of biological decomposition of organic waste by stimulating the growth and activity of bacteria that degrade organic waste.
    aeration
    the mixing or turbulent exposure of water to air and oxygen to dissipate volatile contaminants and other pollutants into the air.
    aeration tank
    a chamber used to inject air into water.
    aerobic treatment
    process by which microbes decompose complex organic compounds in the presence of oxygen and use the liberated energy for reproduction and growth. Such processes include extended aeration, trickling filtration, and rotating biological contactors.
    aerobic
    life or processes that require, or are not destroyed by, the presence of oxygen.
    aggradation
    a progressive build up of a channel bed with sediment over several years due to a normal sequence of scour and deposition, as distinguished from the rise and fall of the channel bed during a single flood.
    aggressive water
    water which is soft and acidic and can corrode plumbing, piping, and appliances.
    algae
    simple rootless plants that grow in sunlit waters in proportion to the amount of available nutrients. They can affect water quality adversely by lowering the dissolved oxygen in the water. They are food for fish and small aquatic animals.
    algal bloom
    a phenomenon whereby excessive nutrients within a river, stream or lake cause an explosion of plant life which results in the depletion of the oxygen in the water needed by fish and other aquatic life. Algae bloom is usually the result of urban runoff (of lawn fertilizers, etc.). The potential tragedy is that of a “fish kill,” where the stream life dies in one mass extinction.
    algicide
    substance or chemical used specifically to kill or control algae.
    alkaline
    the condition of water or soil that contains a sufficient amount of alkali substance to raise the pH above 7.0.
    alkalinity
    the measurement of constituents in a water supply which determine alkaline conditions. The alkalinity of water is a measure of its capacity to neutralize acids. 
    allogenic recharge
    recharge that occurs in a sinking stream, entering an aquifer through sinkholes or fault planes. 
    alluvial
    relating to, composed of, or found in alluvium.
    alluvium
    sediments deposited by erosional processes, usually by streams.
    alvusion
    a sudden or perceptible change in a river’s margin, such as a change in course or loss of banks due to flooding.
    ambient background concentration
    a representative concentration of the water quality in a receiving water body, determined from monitoring. The statistic or data used to determine the value from the range of data is dependent on the purpose of the monitoring and the application of the data.
    ambient medium
    material surrounding or contacting an organism (e.g., outdoor air, indoor air, water, or soil through which chemicals or pollutants can reach the organism.
    amprometric titration
    a way of measuring concentrations of certain substances in water using the electric current that flows during a chemical reaction.
    anabranch
    a secondary channel of a stream which leaves and then rejoins the main channel. The two channels are separated by stable, vegetated lands.
    anaerobic
    a life or process that occurs in, or is not destroyed by, the absence of oxygen.
    anistropic aquifer
    an aquifer in which permeability varies with direction of flow. The Edwards is a highly anistropic aquifer. Modeling flow in such aquifers is very problematic.
    annular space
    the space between two concentric cylindrical objects, one of which surrounds the other, such as the space between the walls of a drilled hole and a casing.
    anti-degradation clause
    part of federal and water quality requirements prohibiting deterioration where pollution levels are above the legal limit.
    appropriative rights
    “first in time, first in right” principle of allocating water rights based. Usually involves a user being allowed to take water from a particular source without regard to the contiguity of the land to the source.
    aquatic
    growing in, living in, or frequenting water.
    aquatic life use
    a beneficial use designation in which the water body provides suitable habitat for survival and reproduction of desirable fish, shellfish, and other aquatic organisms.
    aquiclude
    a formation which, although porous and capable of absorbing water slowly, will not transmit water fast enough to furnish an appreciable supply for a well or a spring.
    aqueous
    something made up of water.
    aqueous solubility
    the maximum concentration of a chemical that will dissolve in pure water at a reference temperature.
    aquiculture
    the raising or fattening of fish in enclosed ponds.
    aquifer
    a geologic formation that will yield water to a well in sufficient quantities to make the production of water from this formation feasible for beneficial use; permeable layers of underground rock or sand that hold or transmit groundwater below the water table.
    aquitard
    geological formation that may contain groundwater but is not capable of transmitting significant quantities of it under normal hydraulic gradients. May function as confining bed.
    armoring
    the formation of an erosion-resistant layer of relatively large particles on a streambed or bank resulting from removal of finer particles by erosion.
    artesian aquifer
    a geologic formation in which water is under sufficient hydrostatic pressure to rise above the top of the aquifer in the subsurface. Artesian aquifers are confined aquifers.
    artesian well
    a water well drilled into a confined aquifer where enough hydraulic pressure exists for water rise in the well to a height above the top of the aquifer in the subsurface. 
    artesian zone
    a zone where water is confined in an aquifer under pressure so that the water will rise in the well casing or drilled hole above the bottom of the confining layer overlying the aquifer.
    assay
    a test for a specific chemical, microbe, or effect.
    assemblage
    an organism group of interacting species in a given ecosystem, for example, a fish assemblage or a benthic macroinvertebrate assemblage.
    assimilation
    the ability of a water body to purify itself of pollutants.
    assimilative capacity
    the capacity of a natural body of water to receive and dilute wastewaters or toxic materials without damage to aquatic life or humans who consume the water.
    attenuation
    the process whereby the magnitude of a flood event is reduced by slowing, modifying, or diverting the flow of water.
    autogenic recharge
    recharge that occurs by falling directly on an aquifer’s outcrop at the surface.
    average annual recharge
    amount of water entering the aquifer on an average annual basis. Averages mean very little for the Edwards because the climate of the region and structure of the aquifer produce a situation in which the area is usually water rich or water poor.

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    Water Resource Term B

    B

    background level
    the concentration of a substance in an environmental media (water or soil) that occurs naturally or is not the result of human activities.
    backpressure
    a pressure that can cause water to backflow into the water supply when a user’s wastewater system is at a higher pressure than the public system.
    backsiphonage
    reverse seepage of water in a distribution system.
    backwashing
    reversing the flow of water through a home treatment device filter or membrane to clean and remove deposits.
    bank
    the sloping land bordering a stream channel that forms the usual boundaries of a channel. The bank has a steeper slope than the bottom of the channel and is usually steeper than the land surrounding the channel. Right and left banks are named facing downstream.
    bank-full capacity
    the rate of water flow that completely fills a channel; the flow rate at which the water surface is level with the flood plain.
    bank stability
    occurs when the channel bank configuration does not change significantly over time.
    bar screen
    in wastewater treatment, a device used to remove large solids from the incoming wastewater stream.
    barrage
    any artificial obstruction placed in water to increase water level or divert it. Usually the idea is to control peak flow for later release.
    base flows
    the component of a flow regime that represents normal flow conditions between precipitation events. Base flows provide a range of suitable habitat conditions that support the natural biological community of a specific river sub-basin.
    bathymetric
    related to the measurement of water depth within a water body.
    bed forms
    three-dimensional configurations of bed material, which are formed in streambeds by the action of flowing water.
    bed load
    the particles in a stream channel that mainly move by bouncing, sliding, or rolling on or near the bottom of the stream.
    bed stability
    occurs when the average elevation of the streambed does not change significantly over time. Aggradation and degradation are the two forms of bed instability.
    beneficial use
    the amount of water necessary when reasonable intelligence and diligence are used for a stated purpose; Texas law recognizes the following uses as beneficial: (1) domestic and municipal uses, (2) industrial uses, (3) irrigation, (4) mining, (5) hydroelectric power, (6) navigation, (7) recreation, (8) stock raising, (9) public parks, and (10) game preserves.
    benthic
    pertaining to the bottom of a body of water, on or within the bottom substrate material.
    Best Management Practice (BMP)
    methods or measures designed and selected to reduce or eliminate the discharge of pollutants from point and nonpoint source discharges. As used in the stormwater context, BMPs are a schedule of activities, prohibitions of practices, maintains procedures and other management practices to prevent or reduce the pollution of waters of the state. BMPs include treatment requirements, operating procedures and practices to control plant site runoff, spills or leaks, sludge or waste disposal, or drainage from raw material storage.
    bioaccumulation
    uptake and retention of substances by an organism from its surrounding medium (usually water) and from food.
    bioassay
    a test to determine the relative strength of a substance by comparing its effect on a test organism with that of a standard preparation.
    bioassessment
    monitoring the aquatic environment to determine the health of a stream.
    biodiversity
    the variety of plant, animal, and microorganism species present in the ecosystem and the community structures the form.
    biogeochemical cycling
    the flow of chemical substances to and from the major environmental reservoirs (atmosphere, hydrosphere, lithosphere, and biosphere).
    biological integrity
    the ability to support and maintain balanced, integrated functionality in the natural habitat of a given region. The concept is applied primarily in drinking water management.
    biological oxidation
    decomposition of complex organic materials by microorganisms. Occurs in self-purification of water bodies and in activated sludge wastewater treatment.
    biomonitoring
    a test used to evaluate the relative potency of a chemical by comparing its effect on a living organism with the effect of a standard population on the same type of organism.
    bioremediation
    a process that uses living organisms to remove pollutants.
    biosolids
    a nutrient-rich organic material resulting from the treatment of wastewater. Biosolids contain nitrogen and phosphorus along with other supplementary nutrients in smaller doses, such as potassium, sulfur, magnesium, calcium, copper and zinc. Soil that is lacking in these substances can be reclaimed with biosolids use. The application of biosolids to land improves soil properties and plant productivity, and reduces dependence on inorganic fertilizers.
    biosphere
    the earth and all its ecosystems.
    biota
    the plant (flora) and animal life (fauna) of a region or ecosystem.
    blackwater
    wastewater from toilet, latrine, and agua privy flushing and sinks used for food preparation or disposal of chemical or chemical-biological ingredients.
    blinds
    water samples containing a chemical of known concentration given a fictitious company name and slipped into the sample flow of the lab to test the impartiality of the lab staff.
    bloom
    a proliferation of algae and/or higher aquatic plants in a body of water; often related to pollution or excessive nutrients, especially when they accelerate growth.
    blowdown
    the water drawn from boiler systems and cold water basins of cooling towers to prevent the buildup of solids.
    bog
    a type of wetland that accumulates appreciable peat deposits. They depend primarily on precipitation for their water source, and are usually acidic and rich in plant matter with a conspicuous mat or living green moss.
    boiling point
    the temperature at which a liquid boils. It is the temperature at which the vapor pressure of a liquid equals the pressure on its surface. If the pressure of the liquid varies, the actual boiling point varies. For water it is 212 degrees Fahrenheit or 100 degrees Celsius.
    BOD
    Biochemical Oxygen Demand. A measure of the amount of oxygen required to neutralize organic wastes.  The BOD of a wastewater is a characteristic reflecting treatability or stage of decomposition.  Compare COD and CBOD.
    boundary conditions
    definition or statement of conditions or phenomena at the boundaries of a model; water levels, flows, and concentrations that are specified at the boundaries of the area being modeled.
    brackish
    mixed fresh and salt water.
    breakpoint chlorination
    addition of chlorine to the point where all organic matter and ammonia compounds have been destroyed and any additional chlorine becomes a free chlorine residual available for disinfection.
    brine
    highly salty and heavily mineralized water containing heavy metal and organic contaminants.
    buoyancy
    the tendency of a body to float or rise when immersed in a fluid; the power of a fluid to exert an upward force on a body placed in it.

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    Water Resource Term C

    C

    calcium carbonate
    CACO3 – a white precipitate that forms in water lines, water heaters and boilers in hard water areas; also known as scale.
    calorie
    amount of energy required to raise the temperature of 1 gram of water 1 degree Celsius.
    calibration
    to check, adjust, or determine by comparison that a computer model will produce results that meet or exceed some defined criteria within a specified degree of confidence.
    canopy
    the overhanging cover formed by branches and foliage.
    capillary action
    movement of water through very small spaces due to molecular forces called capillary forces.
    capillary forces
    forces that cause ground water to rise above the surface of the saturated zone into the spaces between soil particles in the unsaturated zone.
    capillary zone
    soil area above the water table where water can rise up slightly through the cohesive force of capillary action. 
    carbamates
    a class of new-age pesticides that attack the nervous system of organisms.
    carbon adsorption
    a treatment system that removes contaminants from ground water or surface water by forcing it through tanks containing activated carbon treated to attract the contaminants.
    carbonates
    the collective term for the natural inorganic chemical compounds related to carbon dioxide that exist in natural waterways.
    casing
    a tubular structure intended to be watertight installed in the excavated or drilled hole to maintain the well opening and, along with cementing, to confine the ground waters to their zones of origin and prevent the entrance of surface pollutants.
    cavern
    a large underground opening in rock (usually limestone) which occurred when some of the rock was dissolved by water. In some igneous rocks, caverns can be formed by large gas bubbles.
    CBOD
    Carbonaceous Biochemical Oxygen Demand.  A BOD test in which a nitrification inhibitor is added, so that only the carbonaceous oxygen demanding compounds are measured. 
    cement grout
    a mixture of water and cement in the ratio of not more than 5-6 gallons of water to a 94 pound sack of portland cement which is fluid enough to be pumped through a small diameter pipe.
    CERCLA
    Comprehensive Environment Response, Compensation and Liability Act. Also known as SUPERFUND. The Act gave EPA the authority to clean up abandoned, leaky hazardous waste sites.
    certificate of water right
    an official document which serves as court evidence of a perfected water right.
    CFU
    colony forming units.  Concentrations of water quality indicator organisms such as fecal coliform bacteria are measured in cfu/100 ml.
    channel
    a natural or artificial watercourse that continuously or intermittently contains water, with definite bed and banks that confine all but overbanking streamflows.
    channelization
    natural or intentional straightening and/or deepening of streams so water moves faster and causes less flooding.  Channelization can sometimes exacerbate flooding in other downstream areas.
    check dam
    a small dam constructed in a gully or other small water course to decrease the streamflow velocity, minimize channel erosion, promote deposition of sediment and to divert water from a channel.
    chemical weathering
    attack and dissolving of parent rock by exposure to rainwater, surface water, oxygen, and other gases in the atmosphere, and compounds secreted by organisms. 
    Chezy’s equation
    the empirical equation used to estimate the hydraulic conditions of flow within a channel cross section. Alternative to Manning’s equation.
    Chezy’s roughness
    a coefficient in Chezy’s equation that accounts for energy loss due to the friction between the channel and the water.
    chlorination
    the adding of chlorine to water or sewage for the purpose of disinfection or other biological or chemical results.
    chlorine contact chamber
    the part of a wastewater treatment plant where treated water is disinfected by chlorine.
    chlorine demand
    the difference between the amount of chlorine added to water, sewage, or industrial wastes and the amount of residual chlorine remaining at the end of a specific contact period.
    chute spillway
    the overall structure which allows water to drop rapidly through an open channel without causing erosion. Usually constructed near the edge of dams.
    circulate
    to move in a circle, circuit or orbit; to flow without obstruction; to follow a course that returns to the starting point.
    cistern
    a tank used to collect rainwater runoff from the roof of a house or building.
    clarification
    the clearing action that occurs during wastewater treatment when solids settle out. Clarification is often aided by centrifugal action or chemically induced coagulation.
    clarifier
    a tank in which solids settle to the bottom and are subsequently removed as sludge.
    Clean Water Act
    federal legislation enacted in 1972 to restore and maintain the chemical, physical and biological integrity of the surface waters of the United States. The stated goals of the Act are that all waters be fishable and swimmable.
    climatic cycle
    the periodic changes climate displays, such as a series of dry years following a series of years with heavy rainfall.
    climatic year
    a period used in meteorological measurements. The climatic year in the U.S. begins on October 1.
    climate
    generalized weather at a given place on earth over a fairly long period; a long term average of weather. 
    cloudburst
    a torrential downpour of rain, which by it spottiness and relatively high intensity suggests the bursting and discharge of water from a cloud all at once.
    coagulation
    in water treatment, the use of chemicals to make suspended solids gather or group together into small flocs.
    COD
    Chemical Oxygen Demand.  A measure of the oxygen equivalent of the organic matter content of a sample that is susceptible to oxidation by a strong chemical oxidation.  Differs from the BOD test in that COD uses oxygen derived from chemicals, while BOD uses oxygen derived from air dissolved in water. 
    cohesion
    a molecular attraction by which the particles of a body are united throughout the mass whether like or unlike. 
    cold vapor
    method to test water for the presence of mercury.
    coliform bacteria
    non-pathogenic microorganisms used in testing water to indicate the presence of pathogenic bacteria.
    collector well
    a well located near a surface water supply used to lower the water table and thereby induce infiltration of surface water through the bed of the water body to the well.
    colloids
    finely divided solids which will not settle but which may be removed by coagulation or biochemical action.
    combined sewer
    a sewer system that carries both sanitary sewage and stormwater runoff. When sewers are constructed this way, wastewater treatment plants have to be sized to deal with stormwater flows and oftentimes some of the water receives little or no treatment.
    Combined Sewer Overflow (CSO)
    the discharge of a mixture of storm water and domestic waste when the flow capacity of a sewer system is exceeded during rainstorms.
    community water system
    In Texas, a public water system which has a potential to serve at least 15 residential service connections on a year-round basis or serves at least 25 residents on a year-round basis.
    completion
    sealing off access of undesireable water to the well bore by proper casing and/or cementing procedures.
    composite sample, weighted
    a sample composed of two or more portions collected at specific times and added together in volumes related to the flow at time of collection. 
    concentration
    amount of a chemical or pollutant in a particular volume or weight of air, water, soil, or other medium.
    condensation
    the change of state from a gas to a liquid. 
    conduit
    a natural or artificial channel through which fluids may be conveyed.
    cone of depression
    natural depression in the water table around a well during pumping.
    confined aquifer
    an aquifer that lies between two rock layers of very low permeability. Most confined aquifers also are artesian aquifers. 
    confining bed or unit
    a body of impermeable or distinctly less permeable material stratigraphically adjacent to one or more aquifers.
    confluent growth
    in coliform testing, abundant or overflowing bacterial growth which makes accurate measurement difficult or impossible.
    conjunctive management
    integrated management and use of two or more water resources, such as an aquifer and a surface water body.
    connate water
    water trapped in the pore spaces of a sedimentary rock at the time it was deposited. It is usually highly mineralized.
    connectivity
    refers to the movement and exchange of water, nutrients, sediments, organic matter, and organisms within a riverine ecosystem. Connectivity occurs laterally (between the stream and its floodplain), longitudinally (along the stream), vertically (between the stream and groundwater), and temporally.
    conservation
    to protect from loss and waste. Conservation of water may mean to save or store water for later use.
    constituent
    an informal term used to describe a detectable element or component or attribute of waste or effluent.>
    consolidated formation
    naturally occurring geologic formations that have been lithified (turned to stone). The term is sometimes used interchangeably with the term “bedrock.” Commonly, these formations will stand at the edges of a bore hole without caving.
    consumptive use
    the quantity of water not available for reuse. Evapotranspiration, evaporation, incorporation into plant tissue, and infiltration into groundwater are some of the reasons water may not be available for reuse.
    contact recreation
    activities involving a significant risk of ingestion of water, such as wading by children, swimming, water skiing, diving and surfing.
    contamination
    the introduction into water of sewage or other foreign matter that will render the water unfit for its intended use.
    control variables
    large-scale environmental factors that control patterns found in local geomorphic features. For example, geology, soils, land use, hydrology, channel features, and valley characteristics.
    conveyance loss
    water loss in pipes, channels, conduits, and ditches by leakage or evaporation.
    cooling tower
    large tower used to transfer the heat in cooling water from a power or industrial plant to the atmosphere either by direct evaporation or by convection and conduction.
    correlative rights
    rights that are coequal or that relate to one another, so that any one owner cannot take more than his share.
    creek
    a small stream of water which serves as the natural drainage course for a drainage basin. The term is relative according to size. Some creeks in a humid region would be called rivers if they occurred in an arid area.
    crest
    the top of a dam, dike, or spillway, which water must reach before passing over the structure; the summit or highest point of a wave; the highest elevation reached by flood waters flowing in a channel.
    critical low flow
    low flow conditions below which some standards do not apply. The impacts of permitted discharges are analyzed at critical low-flow.
    cross-connection
    any actual or potential connection between a drinking water system and an unapproved water supply or other source of contamination.
    cross-contamination
    a condition created when a drill hole, boring, or improperly constructed well forms a pathway for fluid movement between a saturated zone which contains pollutants and a formerly separated saturated zone containing uncontaminated groundwater. Also, where potable water supplies and sanitary services are interconnected.
    cubic foot per second (CFS)
    the rate of discharge representing a volume of one cubic foot passing a given point during 1 second. This rate is equivalent to approximately 7.48 gallons per second, or 1.98 acre-feet per day.
    current
    the portion of a stream or body of water which is moving with a velocity much greater than the average of the rest of the water. The progress of the water is principally concentrated in the current.
    current velocity
    the velocity of water flow in a stream, measured in units of length per unit of time, such as feet per second (fps).
    cutoff
    where the stream cuts through the neck of a meander bend.
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    Water Resource Term D

    D

    dam
    a structure of earth, rock, or concrete designed to form a basin and hold water back to make a pond, lake, or reservoir.
    dead end
    the end of a water main that is not connected to other parts of the distribution system.
    decomposable waste
    waste that under suitable natural conditions can be transformed through biological and chemical processes into compounds that do not impair water quality.
    deionized water
    water free of inorganic chemicals.
    delta
    an alluvial deposit made of rock particles (sediment, and debris) dropped by a stream as it enters a body of water.
    demand
    the number of units of something that will be purchased at various prices at a point in time. 
    dense non-aqueous phase liquid (DNAPL)
    non-aqueous phase liquids, such as chlorinated hydrocarbon solvents or petroleum fractions, with a specific gravity greater than 1.0 that sink through the water column until they reach a confining layer. Because they are at the bottom of aquifers instead of floating on the water table, typical monitoring wells do not indicate their presence.
    density
    a measure of how heavy a specific volume of a solid, liquid, or gas is in comparison to water.
    dental fluorosis
    disorder caused by excessive absorption of fluorine and characterized by brown staining of teeth.
    depletion curve
    in hydraulics, a graphical representation of water depletion from storage stream channels, surface soil, and groundwater. A depletion curve can be drawn for base flow, direct runoff, or total flow.
    deposit
    something dropped or left behind by moving water, as sand or mud.
    deposition
    the laying down of material by erosion or transport by water or air.
    desalination
    the process of salt removal from sea or brackish water.
    detection limit
    the lowest level that can be determined by a specific analytical procedure or test method.
    detention time
    the time required for a volume of water to pass through a tank at a given rate of flow; in storage reservoirs, the length of time water will be held before being used.
    detergent
    synthetic washing agent that helps remove dirt and oil. Some contain compounds toxic to bacteria that are useful in the wastewater treatment process; other contain nutrients such as phosphorous that may encourage algae growth when they are in wastewater that reaches receiving waters.
    detritus
    decaying organic matter (mostly leaves and other matter from vegetation).
    dewater
    remove or separate a portion of the water in a sludge or slurry to dry the sludge so it can be handled and disposed; remove or drain the water from a tank, trench, or aquifer.
    diatomaceous
    consisting of or abounding in diatoms, a class of unicellular or colonial algae having a silicified cell wall that persists as a skeleton after death.
    digester
    in wastewater treatment, a unit in which anaerobic bacterial action is induced and accelerated in order to break down and stabilize organic matter removed from the treatment process.
    diluting water
    distilled water that has been stabilized, buffered, and aerated. Used in the BOD test.
    dilution ratio
    the critical low flow of the receiving water at the point of recycled water discharge divided by the flow of the discharge.  Is used in the biomonitoring test to simulate in-stream conditions that organisms will be exposed to during critical low-flow times.
    discharge
    the volume of water that passes a given point within a given period of time. It is an all-inclusive outflow term, describing a variety of flows such as from a pipe to a stream, or from a stream to a lake or ocean.
    discharge permit
    a permit issued by a state or the federal government to discharge effluent into waters of the state or the United States. In many states both State and federal permits are required.
    discharger
    any person who discharges waste that could affect the quality of state waters. The term includes any person who owns, or is responsible for the operation of, a waste management unit such as a wastewater treatment plant.
    disinfectant
    a chemical or physical process that kills or inactivates pathogenic organisms in water.  Chlorine is the most commonly used disinfectant for recycled water, potable water supplies, wells, and swimming pools.  Other disinfectants include ozone, bromine, iodine, chlorine dioxide, heat, and ultraviolet light.
    disinfection
    the killing of the larger portion of the harmful and objectionable bacteria in the sewage. Usually accomplished by introduction of chlorine, but more and more facilities are using exposure to ultraviolet radiation, which renders the bacteria sterile.
    disinfection byproducts
    halogenated organic chemicals formed when water is disinfected.
    dispersion
    the movement and spreading of contaminants out and down in an aquifer.
    displacement
    distance by which portions of the same geological layer are offset from each other by a fault.
    dissolve
    the process by which solid particles mix molecule by molecule with a liquid and appear to become part of the liquid.
    dissolved oxygen (DO)
    amount of oxygen gas dissolved in a given quantity of water at a given temperature and atmospheric pressure. It is usually expressed as a concentration in parts per million or as a percentage of saturation.
    dissolved solids
    inorganic material contained in water or wastes. Excessive dissolved solids make water unsuitable for drinking or industrial uses. 
    distillation
    water treatment method where water is boiled to steam and condensd in a separate reservoir. Contaminants with higher boiling points than water do not vaporize and remain in the boiling flask.
    distilled water
    water that has been treated by boiling and condensation to remove solids, inorganics, and some organic chemicals.
    diversion
    to remove water from a water body. Diversions may be used to protect bottomland from hillside runoff, divert water away from active gullies, or protect buildings from runoff.
    downgradient
    the direction that groundwater flows; similar to “downstream” for surface water.
    draft
    the act of drawing or removing water from a tank, reservoir or groundwater supply.
    drainage area
    of a stream at a specified location is that area, measured in a horizontal plane, enclosed by a topographic divide from which direct surface runoff from precipitation normally drains by gravity into the stream above the specified location.
    drainage reuse
    reuse of agricultural drainage on salt-tolerant crops.
    drainage well
    a well drilled to carry excess water off agricultural fields. Because they act as a drain from the surface to the groundwater below, drainage wells can contribute to groundwater pollution.
    drawdown
    the drop in the water table or level of groundwater when water is being pumped from a well; the amount of water used from a tank or reservoir; the drop in the water level of a tank or reservoir.
    dredging
    removal of mud from the bottom of water bodies. This can disturb the ecosystem and cause silting that kills aquatic life. Dredging of contaminated mud can expose biota (the flora and fauna of a  region) to heavy metals and other toxics. Dredging activities may be subject to regulation under state and federal laws.
    driller’s well log
    a log kept at the time of drilling showing the depth, thickness, character of the different strata penetrated, location of water-bearing strata, depth, size, and character of casing installed.
    dripstone
    deposits of calcium carbonate that include stalactites, stalagmites, columns, and cave pearls.
    drought
    although there is no universally accepted definition of drought, it is generally the term applied to periods of less than average precipitation over a certain period of time. In south Texas ranchers say drought begins as soon as it stops raining.
    duplicates
    two separate samples with separate containers taken at the same time at the same place.

    E

    ecoregion
    a geographic area over which the macroclimate is sufficiently uniform to permit development of similar ecosystems on sites with similar geophysical properties.
    ecosphere
    total of all the ecosystems on the planet, along with their interactions; the sphere of air, water, and land in which all life is found.
    ecosystem
    the interacting system of a biological community and its non-living environmental surroundings; a complex system composed of a community of fauna and flora, taking into account the chemical and physical environment with which the system is interrelated.
    ecotone
    a transition zone between two distinctly different ecosystems or communities.
    eddy viscosity
    a model parameter that reproduces the effects of turbulent mixing in fluid flow.
    Edwards Aquifer
    an arch-shaped belt of porous, water bearing limestones composed of the Comanche Peak, Edwards, and Georgetown formations trending from west to east to northeast through Kinney, Uvalde, Medina, Bexar, Comal, Hays, Travis, and Williamson counties.
    Edwards outcrop
    where the Edwards and associated limestone formations are found at the surface. This area is also referred to as the Recharge Zone.
    effective porosity
    the portion of pore space in saturated permeable material where the movement of water takes place.
    effective precipitation
    the part of precipitation which produces runoff; a weighted average of current and antecedent precipitation “effective” in correlating with runoff. It is also that part of the precipitation falling on an irrigated area which is effective in meeting the requirements of consumptive use.
    effluent
    any substance, particularly a liquid, that enters the environment from a point source. Generally refers to wastewater from a sewage treatment or industrial plant.
    effluent limitation
    restrictions established by a a regulating agency such as a State or the EPA in an NPDES permit on quantities, rates, and concentrations in wastewater discharges.
    electrodialysis
    a process which uses an electrical current and an arrangement of permeable membranes to separate soluble minerals from water. It is often used to desalinate salt or brackish water.
    electrofishing
    a biological collection method that uses electric current to facilitate capturing fishes.
    embeddedness
    a measure of the degree that gravel and larger substrates are surrounded by fine particles (silt and sand).
    endangered species
    one having so few individual survivors that the species could soon become extinct in all or part of its region.
    endemism
    the characteristic of being confined to or indigenous in, a certain area or region.
    enrichment
    the addition of nutrients such as nitrogen and phosphorous from wastewater effluent or agricultural runoff to surface water. Enrichment greatly increases the growth potential for algae and other aquatic plants.
    enteric viruses
    a category of viruses related to human excreta found in waterways.
    entrain
    to trap bubbles in water either mechanically through turbulence or chemically through a reaction.
    environment
    aggregate of external conditions that influence the life of an individual organism or population.
    environmental indicator
    a measurement, statistic or value that provides evidence of the effects of environmental management programs or of the state or condition of the environment.
    Environmental Impact Statement (EIS)
    a document that analyzes the effects of major federal projects on the environment. Required by the National Environmental Policy Act.  It must be filed with the President and the Council on Environmental Quality, and made available to the public.
    EPA
    Environmental Protection Agency.  The federal regulatory agency responsible for protecting environmental quality throughout the nation. Also acts in an oversight role to state environmental agencies that carry out federal laws.
    epilimnion
    warm, less dense top layer in a stratified lake.
    erosion
    the wearing away of the land surface by wind, water, ice or other geologic agents. Erosion occurs naturally from weather or runoff but is often intensified by human land use practices.
    escarpment
    the topographic expression of a fault.
    estuarine waters
    deepwater tidal habitats and tidal wetlands that are usually enclosed by land but have access to the ocean and are at least occasionally diluted by freshwater runoff from the land (such as bays, mouths of rivers, salt marshes, lagoons).
    estuarine zone
    area near the coastline that consists of estuaries and coastal saltwater wetlands.
    estuary
    thin zone along a coastline where freshwater system(s) and river(s) meet and mix with a salty ocean (such as a bay, mouth of a river, salt marsh, lagoon).
    euphotic zone
    surface layer of an ocean, lake, or other body of water through which light can penetrate. Also known as the zone of photosynthesis.
    eutrophic
    having a large or excessive supply of plant nutrients (nitrates and phosphates).
    eutrophication (natural)
    an excess of plant nutrients from natural erosion and runoff from the land in an aquatic ecosystem supporting a large amount of aquatic life that can deplete the oxygen supply.
    evaporation
    the change by which any substance is converted from a liquid state and carried of in vapor. 
    evapotranspiration
    combination of evaporation and transpiration of water into the atmosphere from living plants and soil.
    external cost
    cost of production or consumption that must be borne by society; not by the producer.
    extinction
    complete disappearance of a species because of failure to adapt to environmental change.
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    Water Resource Term F

    F

    facultative bacteria
    bacteria that can live under aerobic or anaerobic conditions.
    fecal coliform
    the portion of the coliform bacteria group which is present in the intestinal tracts and feces of warm-blooded animals. A common pollutant in water.
    fen
    a type of wetland that accumulates peat deposits, but not as much as a bog. Fens are less acidic than bogs, deriving most of their water from groundwater rich in calcium and magnesium.
    fermentation, anaerobic
    process in which carbohydrates are converted in the absence of oxygen to hydrocarbons (such as methane).
    field capacity
    the amount of water held in soil against the pull of gravity.
    filter
    a device used to remove solids from a mixture or to separate materials. Materials are frequently separated from water using filters.
    filtration
    the mechanical process which removes particulate matter by separating water from solid material, usually by passing it through sand.
    finite difference
    a method of solving the governing equations of a numerical model by dividing the spatial domain into a mesh of nodes. Solution of the governing equations is approximated from values at the node locations.
    finite element
    a method of solving the governing equations of a numerical model by dividing the spatial domain into elements in each of which the solution of the governing equations is approximated by a continuous function.
    finite volume
    a method of solving the governing equations of a numerical model by dividing the spatial domain into a mesh of nodes and corresponding volumes around each node. Solution of the governing equations is obtained from approximation of the fluxes across the boundaries of adjacent volumes.
    “first in time, first in right”
    phrase indicating that older water rights have priority over more recent rights if there is not enough water to satisfy all rights.
    fixed ground water
    water held in saturated material that it is not available as a source of water for pumping.
    flashiness
    a measure of a river or stream’s tendency to carry a high percentage of its flow volume in large, infrequent events rather than more moderate flows that occur frequently.
    flocculation
    large scale treatment process involving gentle stirring whereby small particles in flocs are collected into larger particles so their weight causes them to settle to the bottom of the treatment tank.
    flood
    an overflow or inundation that comes from a river or other body of water and causes or threatens damage. It can be any relatively high streamflow overtopping the natural or artificial banks in any reach of a stream. It is also a relatively high flow as measured by either gage height or discharge quantity.
    flood frequency
    how often, on average, a discharge of a given magnitude occurs at a particular location on a stream. Usually expressed as the probability that the discharge will exceed some size in a single year (for example, the 100 year flood has a 1 percent probability of being equaled or exceeded in any one year).
    floodplain
    land next to a river that becomes covered by water when the river overflows its banks .
    flora
    plant population of a region.
    flow
    the rate of water discharged from a source expressed in volume with respect to time.
    flow augmentation
    the addition of water to meet flow needs.
    flow duration curve
    a measure of the range and variability of a stream’s flow. The flow duration curve represents the percent of time during which specified flow rates are exceeded at a given location. This is usually presented as a graph of flow rate (discharge) versus percent of time that flows are greater than, or equal to, that flow.
    flow meter
    a gauge indicating the velocity and/or volume of a flowing liquid.
    flow-sensitive habitats
    habitats that show hydraulic response to relatively small changes in streamflow. Responses may be reflected in changes in depth, velocity patterns, wetted width and/or habitat area. Example are shallow-water, edge, and riffle habitats.
    flowing artesian well
    a special case of an artesian well where a water well drilled into a confined aquifer has enough hydraulic pressure for the water to rise to a height above ground surface and to flow at the surface without pumping.
    flume
    a natural or artificially made channel that diverts water.
    flush
    to open a cold-water tap to clear out all the water which may have been sitting for a long time in the pipes; to force large amounts of water through a system to clean out piping or tubing and storage or process tanks.
    foodweb
    a model structure used to represent the links between organisms within an environment, based upon the order in which various organisms consume one another.
    forebay
    the water behind a dam.
    forfeited water right
    a water right canceled because of several consecutive years of nonuse.
    freeboard
    the vertical distance between the lowest point along the top of a surface impoundment dike, berm, levee, treatment works or other similar feature and the surface of the liquid contained therein.
    free ground water
    water in interconnected pore spaces in the zone of saturation down to the first impervious barrier, moving under the control of the water table slope.
    freezing
    the change of a liquid into a solid as temperature decreases. For water, the freezing point is 32 F or 0 C.
    fresh water
    water containing less than 1,000 parts per million (ppm) of dissolved solids of any type.
    fresh water inflow requirements
    freshwater flows required to maintain the natural salinity, nutrient, and sediment delivery in a bay or estuary that supports their unique biological communities and ensures a healthy ecosystem.
    fresh:salt water interface
    the region where fresh water and salt water meet. In the Edwards region, it is commonly referred to as the “bad water line”, although it is zone and not a line.
    frost
    a covering of minute ice crystals on a cold surface.
    Froude number
    a dimensionless number comparing inertial and gravitational forces. Used to quantify the resistance of an object moving through water, and compare objects of different sizes. Froude numbers greater than 1 correspond to supercritical flow, less than 1 to subcritical flow.
    furrow irrigation
    irrigation method in which water travels through the field by means of small channels between each group of rows.
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    Water Resource Term G

    G

    gaging station
    the site on a stream, lake or canal where hydrologic data is collected.
    gallon
    A unit of volume. A U.S. gallon contains 231 cubic inches, 0.133 cubic feet, or 3.785 liters. One U.S. gallon of water weighs 8.3 lbs.
    game fish
    a species such as trout, salmon, or bass, caught for sport.
    gas chromatograph
    an instrument that identifies the molecular composition and concentrations of various chemicals in water and soil samples.
    geohydrology
    a term which denotes the branch of hydrology relating to subsurface or subterranean waters; that is, to all waters below the surface.
    geologic erosion
    normal or natural erosion caused by geological processes acting over long geologic periods and resulting in the wearing away of mountains, the building up of floodplains, coastal plains, etc.
    geopressured reservoir
    a geothermal reservoir consisting of porous sands containing water or brine at high temperature or pressure.
    geyser
    a periodic thermal spring that results from the expansive force of super heated steam.
    giardia lamblia
    a protozoa found in the feces of infected humans and animals that can cause severe gastrointestinal ailments. It is a common contaminant of surface waters.
    glacier
    a huge mass of land ice that consists of recrystallized snow and moves slowly downslope or outward.
    grab sample
    a sample taken at a given place and time. 
    granular activated carbon
    pure carbon heated to promote “active” sites which can adsorb pollutants. Used in some home water treatment systems to remove certain organic chemicals and radon.
    grassed waterway
    natural or constructed watercourse or outlet that is shaped or graded and planted in suitable vegetation for the disposal of runoff water without erosion.
    greywater
    wastewater from clothes washing machines, showers, bathtubs, handwashing, lavatories and sinks that are not used for disposal of chemical or chemical-biological ingredients.
    groundwater
    water within the earth that supplies wells and springs; water in the zone of saturation where all openings in rocks and soil are filled, the upper surface of which forms the water table.
    groundwater hydrology
    the branch of hydrology that deals with groundwater; its occurrence and movements, its replenishment and depletion, the properties of rocks that control groundwater movement and storage, and the methods of investigation and utilization of ground water.
    groundwater law
    the common law doctrine of riparian rights and the doctrine of prior appropriation as applied to ground water.
    groundwater recharge
    the inflow to a ground water reservoir.
    groundwater reservoir
    an aquifer or aquifer system in which ground water is stored. The water may be placed in the aquifer by artificial or natural means.
    groundwater runoff
    the portion of runoff which has passed into the ground, has become ground water, and has been discharged into a stream channel as spring or seepage water.
    groundwater storage
    the storage of water in groundwater reservoirs.
    guild
    a group of species or organisms that use the same environmental resources (habitat, food source, etc.) or life history strategy (such as reproduction) in the same way.
    gully
    a deeply eroded channel caused by the concentrated flow of water.
    gully reclamation
    use of small dams of manure and straw; earth, stone,or concrete to collect silt and gradually fill in channels of eroded soil.
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    Water Resource Term H

    H

    habitat
    the native environment or specific surroundings where a plant or animal naturally grows or lives. Habitat includes physical factors such as temperature, moisture, and light together with biological factors such as the presence of food or predator organisms.
    habitat indicator
    a physical attribute of the environment measured to characterize conditions necessary to support an organism, population, or community in the absence of pollutants. For example, salinity of estuarine waters or substrate type in streams or lakes.
    hail
    a form of precipitation which forms into balls or lumps of ice over 0.2 inch in diameter. Hail is formed by alternate freezing and melting as precipitation is carried up and down in highly turbulent air currents.
    hardpan
    a shallow layer of earth material which has become relatively hard and impermeable, usually through the deposition of minerals. In the Edwards region hardpans of clay are common.
    hard water
    water containing a high level of calcium, magnesium, and other minerals. Hard water reduces the cleansing power of soap and produces scale in hot water lines and appliances.
    hardness (water)
    condition caused by dissolved salts of calcium, magnesium, and iron, such as bicarbonates, carbonates, sulfates, chlorides, and nitrates.
    hardwood bottomland
    hardwood forested lowlands adjacent to some rivers, especially valuable for wildlife breeding, nesting, and habitat.
    head
    the pressure of a fluid owing to its elevation, usually expressed in feet of head or in pounds per square inch, since a measure of fluid pressure is the height of a fluid column above a given or known point.
    headgate
    the gate that controls water flow into irrigation canals and ditches. A watermaster regulates the headgates during water distribution and posts headgate notices declaring official regulations.
    heat of vaporization
    the amount of heat necessary to convert a liquid (water) into vapor.
    heavy water
    water in which all the hydrogen atoms have been replaced by deuterium.
    herbicide
    a chemical used to kill nuisance plants. Herbicides can contain pollutants found in runoff.
    heterogenic aquifer
    an aquifer that has a variety of forms or characteristics, such as differering permeabilities. The Edwards is highly heterogenic. 
    high flow pulses
    the component of an instream flow regime that represents short-duration, in-channel, high flow events following storm events. They maintain important physical habitat features and longitudinal connectivity along the river channel.
    holding pond
    a small basin or pond designed to hold sediment laden or contaminated water until it can be treated to meet water quality standards or be used in some other way.
    holding time
    the maximum amount of time a sample may be stored before analysis.
    homogenous aquifer
    an aquifer that has similar forms or characteristics throughout, such as a uniform gravel aquifer. The Edwards is not homogenous, it is highly heterogenic.
    hydraulic conductivity
    the rate at which water can move through a permeable medium.
    hydraulic control
    a feature in a stream (such as a constriction or a weir) that controls the upstream water surface elevation.
    hydraulic gradient
    the direction of groundwater flow due to changes in the depth of the water table.
    hydraulic model
    a computer model of a segment of river used to evaluate hydraulic conditions. 
    hydraulic roughness
    an estimate of the resistance to flow due to energy loss caused by friction between the channel and the water. Chezy’s and Manning’s roughness are two different ways to express this parameter.
    hydrocarbons
    chemical compounds that consist entirely of carbon and hydrogen; also referred to as volatile organic compound.
    hydroelectric plant
    electric power plant in which the energy of falling water is used to spin a turbine generator to produce electricity.
    hydrogeology
    the geology of groundwater, with particular emphasis on the chemistry and movement of water.
    hydrograph
    a chart that measures the amount of water flowing past a point as a function of time.
    hydrologic balance
    an accounting of all water inflow to, water outflow from, and changes in water storage within a hydrologic unit over a specified period of time.
    hydrologic basin
    the drainage area upstream from a given point on a stream.
    hydrologic cycle
    natural pathway water follows as it changes between liquid, solid, and gaseous states; biogeochemical cycle that moves and recycles water in various forms through the ecosphere. Also called the water cycle.
    hydrologic model
    a computer model of a watershed used to evaluate how precipitation contributes to flow in streams. 
    hydrologic unit
    is a geographic area representing part or all of a surface drainage basin or distinct hydrologic feature.
    hydrology
    the science dealing with the properties, distribution, and circulation of water.
    hydrolysis
    the decomposition of organic compounds by interaction with water.
    hydrometer
    an instrument used to measure the density of a liquid.
    hydropneumatic
    a water delivery system, usually small, that maintains water pressure in the distribution system by means of pressure in a compressed air tank.
    hydropower
    electrical energy produced by falling water.
    hygroscopic nuclei
    piece of dust or other particle around which water condenses in the atmophere. These tiny droplets then collide and coalesce, with as many as 10,000 nuclei contributing to formation of a raindrop.
    hydrosphere
    region that includes all the earth’s liquid water, frozen water, floating ice, frozen upper layer of soil, and the small amounts of water vapor in the Earth’s atmosphere.
    hydrostatic head
    a measure of pressure at a given point in a liquid in terms of the vertical height of a column of the same liquid which would produce the same pressure.
    hydrostatic pressure
    pressure exerted by or existing within a liquid at rest with respect to adjacent bodies.
    hypolimnion
    bottom layer of cold water in a lake. 
    hyporheic zone
    the zone under a river or stream comprising substrate whose interstices are filled with water.
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    Water Resource Term I

    I

    ice
    a solid form of water.
    imhoff cone
    a clear, cone-shaped container used to measure the volume of settleable solids in a specific volume of water.
    immiscibility
    the inability of two or more substances or liquids to readily dissolve into one another, such as soil and water.
    impaired water body
    a water body that has been determined under state and federal law as not meeting water quality standards, or having the potential to do so in the future.
    imperiled species
    declining, rare, or uncommon species; species federally listed as threatened or endangered, or candidates for such; and species with limited distributions.
    impermeable
    material that does not permit fluids to pass through.
    impervious
    the quality or state of being impermeable; resisting penetration by water or plant roots. Impervious ground cover like concrete and asphalt affects quantity and quality of runoff.
    impoundment
    a body of water such as a pond, confined by a dam, dike, floodgate or other barrier. It is used to collect and store water for future use.
    Index of Biotic Integrity
    a multi-metric measure of biological condition developed from collection of data for fish or other organisms. It consists of metrics in three broad categories: species composition, trophic composition, and organism abundance and condition.
    in-line filtration
    a pretreatment method in which chemicals are mixed by flowing water; commonly used in pressure filtration installations.
    in-situ flushing
    introduction of large volumes of water, at times supplemented with cleaning compounds, into soil, waste, or groundwater to flush hazardous contaminants from a site.
    in-situ oxidation
    technology that oxidizes contaminants dissolved in groundwater, converting them into insoluble compounds.
    in-situ stripping
    treatment system that removes or strips volatile organic compounds from contaminated groundwater or surface water by forcing an air stream through the water and causing the compounds to evaporate.
    in-situ vitrification
    technology that treats contaminated soil in place at high temperatures, at 3,000 degrees Fahrenheit or more.
    inchoate water right
    an unperfected water right.
    indicator organisms
    microorganisms, such as coliforms, whose presence is indicative of pollution or of more harmful microorganism.
    indicator parameters
    measurable physical or chemical characteristics or attributes of water or soil-pore moisture used to indicate the possible presence of waste constituents, or the effects of waste constituents on waters.
    indicator tests
    tests for a specific contaminant, group of contaminants, or constituent which signals the presence of something else (ex., coliforms indicate the presence of pathogenic bacteria).
    infiltration
    the penetration of water through the ground surface into sub-surface soil or the penetration of water from the soil into sewer or other pipes through defective joints, connections, or manhole walls.
    infiltration rate
    the quantity of water that can enter the soil in a specified time interval.
    inflow
    entry of rainwater into a sewer system from sources other than infiltration, such as basement drains, manholes, storm drains, and street washing.
    influent
    water, wastewater, or other liquid flowing into a reservoir, basin, or treatment plant.
    initial dilution
    the process that results in the rapid and irreversible turbulent mixing of effluent and receiving water around the point of discharge.
    injection well
    as defined by the U.S. EPA, any bored, drilled or driven shaft, dug pit or hole in the ground into which waste or fluid is discharged, and any associated subsurface appurtenances, the depth of which is greater than the largest surface dimension of the shaft, pit or hole.
    injection zone
    a geological formation receiving fluids through a well.
    inland freshwater wetlands
    swamps, marshes, and bogs found inland beyond the coastal saltwater wetlands.
    instream cover
    overhanging or instream structure, such as tree roots, undercut streambanks, boulders, or aquatic vegetation that offer protection for aquatic organisms.
    instream use
    use of water that does not require withdrawal or diversion from its natural watercourse; for example, the use of water for navigation, recreation, and support of fish and wildlife.
    interbasin transfer
    the physical transfer of water from one watershed to another; regulated by the Texas Water Code.
    interceptor sewer
    very large sewer lines that collect the flow from main and trunk lines and carry them to treatment plants.
    interface
    the common boundary between two substances such as water and a solid, water and a gas, or two liquids such as water and oil.
    interfacial tension
    the strength of the film separating two immiscible fluids (e.g., oil and water) measured in dynes per, or millidynes per, centimeter.
    intermittent stream
    one that flows periodically. 
    interstate water
    according to law, interstate waters are defined as (1) rivers, lakes and other waters that flow across or form a part of state or international boundaries; (2) waters of the Great Lakes; (3) coastal waters whose scope has been defined to include ocean waters seaward to the territorial limits and waters along the coastline (including inland streams) influenced by the tide.
    interstices
    the void or empty portion of rock or soil occupied by air or water.
    inert waste
    waste that does not contain hazardous waste or soluble pollutants at concentrations in excess of applicable water quality objectives, and does not contain significant quantities of decomposable waste.
    irrigation efficiency
    the percentage of water applied, and which can be accounted for, in the soil moisture increase for consumptive use.
    irrigation return flow
    water which is not consumptively used by plants and returns to a surface or ground water supply. Under conditions of water right litigation, the definition may be restricted to measurable water returning to the stream from which it was diverted.
    irrigation water
    water which is applied to assist crops in areas or during times where rainfall is inadequate.
    isotherm
    line that connects points of equal temperature.
    isohyet
    line that connects points of equal rainfall.
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    Water Resource Term J

    J

    jar test
    a laboratory procedure that simulates a water treatment plant’s coagulation/flocculation units with differing chemical doses, mix speeds, and settling times to estimate the minimum or ideal coagulant dose required to achieve certain water quality goals.
    jet stream
    a long narrow meandering current of high-speed winds near the tropopause blowing from a generally westerly direction and often exceeding a speed of 250 miles per hour.
    jetteau
    a jet of water.
    jetter
    one (as a geyser) that sends out a jet.
    jetty
    a structure (as a pier or mole of wood or stone) extending into a sea, lake, or river to influence the current or tide or to protect a harbor.
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    Water Resource Term K

    K

    kalema
    a violent surf that occurs on the coast of the Guinea region, West Africa.
    kame
    a short ridge, hill, or mound of stratified drift deposited by glacial meltwater.
    kame terrace
    a terrace of stratified sand and and gravel deposited by streams between a glacier and an adjacent valley wall.
    kelp beds
    significant aggregations of a large, fast growing marine algae throughout the water column.
    key habitats
    flow-sensitive habitats as well as habitats that support key species.
    key species
    species that are targeted for instream flow assessment or more generally taxa of interest; may include lotic-adapted species, imperiled species, sport fishes, or other species related to study objectives.
    kinetic energy
    energy possessed by a moving object or water body.
    kilogram
    one thousand grams.
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    Water Resource Term L

    L

    laboratory water
    purified water used in the laboratory as a basis for making up solutions or making dilutions. Water devoid of interfering substances.
    lag time
    the time from the center of a unit storm to the peak discharge or center of volume of the corresponding unit hydrograph.
    lagoon
    a shallow pond where sunlight, bacterial action, and oxygen work to purify wastewater. Lagoons are typically used for the storage of wastewaters, sludges, liquid wastes, or spent nuclear fuel.
    lake
    an inland body of water, usually fresh water, formed by glaciers, river drainage etc. Usually larger than a pool or pond.
    land application
    discharge of wastewater onto the ground for treatment or reuse.
    landscape impoundment
    body of reclaimed water which is used for aesthetic enjoyment or which otherwise serves a function not intended to include contact recreation.
    Langelier Saturation Index (LSI)
    an index reflecting the equilibrium pH of a water with respect to calcium and alkalinity; used in stabilizing water to control both corrosion and scale deposition.
    leachate
    water containing contaminants which leaks from a disposal site such as a landfill or dump.
    leachate collection system
    a system that gathers leachate and pumps it to the surface for treatment.
    leaching
    extraction or flushing out of dissolved or suspended materials from the soil, solid waste, or another medium by water or other liquids as they percolate down through the medium to groundwater.
    lentic system
    a nonflowing or standing body of fresh water, such as a lake or pond. 
    levee
    a natural or man-made earthen obstruction along the edge of a stream, lake, or river. Usually used to restrain the flow of water out of a river bank.
    limestone
    rock that consists mainly of calcium carbonate and is chiefly formed by accumulation of organic remains.
    limiting factor
    factor such as temperature, light, water, or a chemical that limits the existence, growth, abundance, or distribution of an organism.
    limnology
    scientific study of physical, chemical, and biological conditions in lakes, ponds, and streams.
    Lindane
    a pesticide that causes adverse health effects when present in domestic water supplies and is toxic to freshwater fish and aquatic life.
    liner
    a relatively impermeable barrier designed to keep leachate inside a landfill; an insert or sleeve for sewer pipes to prevent leakage or infiltration.
    liquid
    a state of matter, neither gas nor solid, that flows and takes the shape of its container.
    littoral zone
    area on or near the shore of a body of water.
    lotic-adapted species
    species for which all or part of their life history is dependent on flowing water.
    lotic system
    a flowing body of fresh water, such as a river or stream.
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    Water Resource Term M

    M

    macrointervebrate
    an animal without a backbone, large enough to be seen without magnification and unable to pass through a 0.595 mm mesh.
    macrophyte
    macroscopic plants in the aquatic environment. The most common macrophytes are the rooted vascular plants that are usually arranged in zones in aquatic ecosystems and restricted in their area by the extent of illumination through the water and sediment deposition along the shoreline.
    Manning’s equation
    an empirical equation used to estimate the average hydraulic conditions of flow within a channel cross section.
    Manning’s roughness
    a coefficient in Manning’s equation that accounts for energy loss due to the friction between the channel and the water. Many hydraulic models use this coefficient to estimate resistance to flow.
    mariculture
    cultivation of fish and shellfish in estuarine and coastal areas.
    marsh
    an area periodically inundated and treeless and often characterized by grasses, cattails, and other monocotyledons
    MCL – Maximum Contaminant Level
    the maximum level of a contaminant allowed in water by federal law. Based on health effects and currently available treatment methods.
    mean column velocity
    the average velocity of fluid flow measured in a column extending from the surface of the water to the bed of the channel. Often referred to simply as “velocity” or “current velocity”. 
    meander bend
    a windings or sinuous section of a stream channel. May become an oxbow lake if cut off from the mainstem.
    median particle size
    value for which half the particles in a sample have a greater diameter and half a lesser diameter.
    median streamflow
    the rate of discharge of a stream for which there are equal numbers of greater and lesser flow occurrences during a specified period.
    melting
    the changing of a solid into a liquid.
    meltwater
    water that comes from the melting ice of a glacier or a snowbank.
    mesohabitat
    basic structural elements of a river or stream such as pools, backwaters, runs, glides, and riffles.
    mesotrophic
    reservoirs and lakes that contain moderate quantities of nutrients and are moderately productive in terms of aquatic animal and plant life.
    meteoric water
    groundwater which originates in the atmosphere and reaches the zone of saturation by infiltration and percolation.
    method blank
    laboratory grade water taken through the entire analytical procedure to determine if samples are being accidentally contaminated by chemicals in the lab
    methyl tertiary butyl ether (MTBE)
    an additive originally put in gasoline to reduce air pollution, but later found to be a source of groundwater pollution.
    methoxychlor
    pesticide that causes adverse health effects when found in domestic water supplies. It is also toxic to aquatic life.
    methyl orange alkalinity
    A measure of the total alkalinity in a water sample in which the color of methyl orange reflects the change in level.
    micrograms per liter – Ug/L
    micrograms per liter of water. One thousands micrograms per liter is equivalent to 1 milligram per liter. This measure is equivalent to parts per billion (ppb)
    microhabitat
    zones of similar physical characteristics within a mesohabitat unit, differentiated by aspects such as substrate type, water velocity, and water depth.
    migration
    the movement of oil, gas, contaminants, water, or other liquids through porous and permeable rock.
    milligrams per liter – mg/L
    milligrams per liter of water. This measure is equivalent to parts per million (ppm).
    minimum streamflow
    the specific amount of water reserved to support aquatic life, to minimize pollution, or for recreation. It is subject to the priority system and does not affect water rights established prior to its institution.
    mixed liquor
    a mixture of activated sludge and water containing organic matter undergoing treatment in an aeration tank.
    mixing zone
    a limited volume of receiving water that is allocated for diluting a wastewater discharge without causing adverse effects to the overall water body.
    moisture content
    the amount of water lost from soil upon drying to a constant weight, expressed as the weight per unit of dry soil or as the volume of water per unit bulk volume of the soil.
    moisture holding capacity
    the amount of liquid that can be held against gravity, by waste materials or soil, without generating free liquid.
    molecule
    the smallest division of a compound that still retains or exhibits all the properties of the substance.
    modified Wentworth scale
    a specific scale used to classify substrate particles by their diameter. Categories in this scale include boulder, cobble, pebble, gravel, sand, silt, and clay.
    monitoring well
    a well used to obtain water quality samples or measure groundwater levels.
    monomictic
    lakes and reservoirs that are relatively deep, do not freeze over during winter, and undergo a single stratification and mixing cycle during the year (usually in the fall).
    mudballs
    round material that forms in filters and gradually grows when not removed by backwashing.
    multiple use
    Use of bodies of water for more than one purpose, such as recreational purposes, fishing, and water supply.
    municipal discharge
    discharge of effluent from treatment plants that receive wastewater from households, commercial establishments, and industries.
    municipal sewage
    sewage from a community which may be composed of domestic sewage, industrial wastes or both.
    municipal sludge
    semi-liquid residue remaining from the treatment of municipal water and wastewater.
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    Water Resource Term N

    N

    National Estuary Program
    a program established under the Clean Water Act Amendments of 1987 to conserve and manage estuaries, restore and maintain their chemical, physical, and biological integrity, and control point and nonpoint pollution sources.
    National Municipal Plan
    a U.S. EPA policy created in 1984 to bring all publicly owned treatment works (POTWs) into compliance with Clean Water Act requirements.
    National Oil and Hazardous Substances Contingency Plan
    the federal regulation that guides determination of the sites to be corrected under the Superfund program, and the program to prevent or control spills into surface waters or elsewhere.
    National Pollutant Discharge Elimination System (NPDES)
    a provision of the Clean Water Act that prohibits discharge of pollutants into waters of the United States unless a permit is issued that complies with the Clean Water Act. In Texas, the Texas Commission on Environmental Quality (TCEQ) administers the NPDES program and issues TPDES permits.
    National Priorities List (NPL)
    EPA’s list of the most serious uncontrolled or abandoned hazardous waste sites identified for possible long-term remedial action under Superfund. The list is based primarily on the score a site receives from the Hazard Ranking System. EPA is required to update the NPL at least once a year. A site must be on the NPL to receive money for remedial action from the Superfund Trust Fund.
    National Response Team (NRT)
    representatives of 13 federal agencies that, as a team, coordinate federal responses to nationally significant incidents of pollution and provide advice and technical assistance to the responding agencies.
    National Response Center
    The 24-hour a day federal operations center receives notifications of all releases of oil and hazardous substances into the environment. Operated by the U.S. Coast Guard, the Center evaluates all reports and notifies the appropriate agency.
    natural flow
    the rate of water movement past a specified point on a natural stream. The flow comes from a drainage area in which there has been no stream diversion caused by storage, import, export, return flow, or change in consumptive use caused by man-controlled modifications to land use. Natural flow rarely occurs in a developed country.
    natural resource
    any form of matter or energy obtained from the environment that meets human needs.
    naturalized conditions
    an estimate of natural conditions obtained by attempting to remove effects of human activities from a set of measured conditions.
    Navier-Stokes equations
    a set of equations that describe the physics governing the motion of a fluid. In addition to applications in hydraulic studies of rivers and streams, these equations are used to model weather, ocean currents, and aerodynamics.
    nephelometric
    method of measuring turbidity in a water sample by passing light through the sample and measuring the amount of light deflected.
    NIPDWR
    National Interim Primary Drinking Water Regulations.
    nitrate
    a compound containing nitrogen that can exist in water as a dissolved gas. It can have harmful effects on humans and animals. Nitrates in water can cause severe illness in infants and domestic animals. A plant nutrient and inorganic fertilizer, nitrate is found in septic systems, animal feed lots, agricultural fertilizers, manure, industrial wastewaters, sanitary landfills, and garbage dumps.
    nitrogen
    a plant nutrient that can cause an overabundance of bacteria and algae when high amounts are present, leading to a depletion of oxygen and fish kills. Several forms occur in water, including ammonia, nitrate, nitrite or elemental nitrogen. High levels of nitrogen in water are usually caused by agricultural runoff or improperly operating wastewater treatment plants. 
    non-aqueous phase liquid (NAPL)
    contaminants that remain undiluted as the original bulk liquid in the subsurface, such as spilled oil.
    nonconsumptive use
    using water in a way that does not reduce the supply. Examples include hunting, fishing, boating, water-skiing, swimming, and some power production. 
    noncontact recreation
    recreational pursuits not involving a significant risk of water ingestion, including fishing, commercial and recreational boating, and limited body contact incidental to shoreline activity. 
    nondegradation
    an environmental policy that does not allow any lowering of naturally occurring water quality regardless of pre-established health standards.
    nonporous
    something which does not allow water to pass through it.
    nonpoint source
    source of pollution in which wastes are not released at one specific, identifiable point but from a number of points that are spread out and difficult to identify and control. 
    nonpotable
    not suitable for drinking. 
    nonthreshold pollutant
    substance or condition harmful to a particular organism at any level or concentration.
    NTU
    nephlometric turbidity units.
    nutrient
    as a pollutant, any element or compound, such as phosphorous or nitrogen, that fuels abnormally high organic growth in aquatic ecosystems. 
    nutrient cycle
    the cyclic conversions of nutrients from one form to another within biological communities. For example, the production and release of molecular oxygen from water during photosynthesis by plants and the subsequent reduction of atmospheric oxygen to water by the respiratory metabolism of other biota.
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    Water Resource Term O

    O

    oligotrophic
    having a low supply of plant nutrients. 
    on-site sewage treatment
    any individual residential sewage treatment and wastewater dispersal system, such as a septic system.
    open system
    system in which energy and matter are exchanged between the system and its environment, for example, a living organism.
    operable unit
    a term used by the Superfund program to describe a discrete action that comprises an incremental step toward comprehensively addressing site problems. The cleanup of a site can be divided into a number of operable units, depending on the complexity of the problems associated with the site. Operable units may address geographical portions of a site, specific site problems, or initial phases of an action, or may consist of any set of actions performed over time or any actions that are concurrent but located in different parts of a site. A typical operable unit would be removal of drums and tanks from the surface of a site.
    organic chemicals
    chemicals containing carbon.
    organism
    any form of animal or plant life.
    organism abundance and condition
    that portion of an Index of Biotic Integrity that is a metric measuring species abundance and condition, including proportion of individuals as hybrids and proportion of individuals with disease, tumors, physical damage, or physical anomalies.
    organotins
    chemical compounds used in antifoulant paints to protect the hulls of boats and ships, buoys, and pilings from marine organisms such as barnacles.
    orogeny
    period of mountain-building.
    orographic precipitation
    rainfall that occurs as a result of warm, humid air being forced to rise by topographic features such as mountains. Precipitation on the Edwards Plateau is slightly higher because of the orographic effect of the escarpment and hills.
    osmosis
    the passage of a liquid from a weak solution to a more concentrated solution across a semi-permeable membrane that allows passage of the solvent (water) but not the dissolved solids.
    outcrop
    exposed at the surface. The Edwards limestone outcrops in its recharge zone.
    outfall
    the place where a wastewater treatment plant discharges treated water into the environment.
    outwash
    a deposit of sand and gravel formed by streams of meltwater flowing from a glacier.
    overbank flows
    the component of an instream flow regime that represents infrequent, high flow events that exceed the normal channel. These flows maintain riparian areas and provide lateral connectivity between the river channel and active flood plain. They may also provide life-cycle cues for various species.
    overdraft
    pumping water from a groundwater basin or aquifer in excess of the supply flowing into the basin; results in a depletion or “mining” of the groundwater in the basin.
    overflow rate
    one of the guidelines for design of the settling tanks and clarifiers in a treatment plant.
    overland flow
    a land application technique that cleanses wastewater by allowing it to flow over a sloped surface. As the water flows over the surface, contaminants are absorbed and the water is collected at the bottom of the slope for reuse.
    oxbow
    a U-shaped bend in a river or stream that may or may not be cut off from the mainstem.
    oxbow lake
    a U-shaped water body formed when a meander bend is cut off from the mainstem of a river or stream to create a lake.
    oxygen demanding waste
    organic water pollutants that are usually degraded by bacteria if there is sufficient dissolved oxygen (DO) in the water.
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    Water Resource Term P

    P

    pathogen
    microorganisms which can cause disease.
    peak flow
    in a wastewater treatment plant, the highest flow expected to be encoutered under any operational conditions, including periods of high rainfall and prolonged periods of wet weather.
    Peclet number
    the relationship between properties of the mesh, fluid velocity, and eddy viscosity for a hydraulic computer model.
    pentachorophenol
    toxic substance usually used as a wood preservative.
    perched water table
    groundwater standing unprotected over a confined zone.
    perchloroethylene
    a chlorinated solvent commonly used in dry cleaning. Also known as tetrachloroethylene.
    percolation
    the movement of water through the subsurface soil layers, usually continuing downward to the groundwater or water table reservoirs.
    percolating waters
    waters passing through the ground beneath the Earth’s surface without a definite channel.
    perfected water right
    a water right which indicates that the uses anticipated by an applicant, and made under permit, were made for beneficial use. Usually it is irrevocable unless voluntarily canceled or forfeited due to several consecutive years of nonuse.
    perennial stream
    one that flows all year round. 
    permeability
    the ability of a water bearing material to transmit water. It is measured by the quantity of water passing through a unit cross section, in a unit time, under 100 percent hydraulic gradient.
    petroleum derivatives
    chemicals formed when gasoline breaks down in contact with water.
    pH
    numeric value that describes the intensity of the acid or basic (alkaline) conditions of a solution. The pH scale is from 0 to 14, with the neutral point at 7.0. Values lower than 7 indicate the presence of acids and greater than 7.0 the presence of alkalis (bases). Technically speaking, pH is the logarithm of the reciprocal (negative log) of the hydrogen ion concentration (hydrogen ion activity) in moles per liter.
    phenolphthalein alkalinity
    the alkalinity in a water sample measured by the amount of standard acid needed to lower the pH to a level of 8.3 as indicated by the change of color of the phenolphthalein from pink to clear.
    phenols
    organic compounds that are byproducts of petroleum refining; tanning; and textile, dye, and resin manufacturing. Low concentrations cause taste and odor problems in water; higher concentrations can kill aquatic life and humans.
    phosphorous
    a plant nutrient that can cause an overabundance of bacteria and algae when high amounts are present, leading to a depletion of oxygen and fish kills. High levels of phosphorous in water are usually caused by agricultural runoff or improperly operating wastewater treatment plants.
    phreatic zone
    the area in an aquifer in which relatively all pores and fractures are saturated with water. The phreatic zone may fluctuate with changes of season and during wet and dry periods.
    phreatophytes
    plants that send their roots into or below the capillary zone to use ground water.
    physical weathering
    breaking down of parent rock into bits and pieces by exposure to temperature and changes and the physical action of moving ice and water, growing roots, and human activities such as farming and construction.
    physiographic province
    an area with similar characteristics based on geology, soil type, and topography.
    phytoplankton
    free-floating, mostly microscopic aquatic plants.
    piezometer
    a nonpumping well, generally of small diameter, for measuring the elevation of a water table.
    piezometric surface
    the imaginary surface to which groundwater rises under hydrostatic pressure in wells or springs.
    plankton
    microscopic floating plant and animal organisms of lakes, rivers, and oceans.
    plate tectonics
    refers to the folding and faulting of rock and flow of molten lava involving lithospheric plates in the earth’s crust and upper mantle.
    plug
    cement, grout, or other material used to fill and seal a hole drilled for a water well.
    plug flow
    type of flow that occurs in tanks, basins, or reactors when a slug of water moves through without ever dispersing or mixing with the rest of the water flowing through.
    plume
    the area taken up by contaminant(s) in an aquifer.
    pluvial
    pertaining to precipitation.
    point source
    source of pollution that involves discharge of wastes from an identifiable point, such as a smokestack or sewage treatment plant. 
    point velocity
    velocity measured at a single point in the water column of flowing water.
    pollution
    undesireable change in the physical, chemical, or biological characteristics of the air, water, or land that can harmfully affect the health, survival, or activities of human or other living organisms.
    polychlorinated biphenyls (PCBs)
    toxic industrial chemical compound substances that were used in the manufacture of plastics and as insulating fluids in electrical transformers and capacitors. Banned since 1979, PCBs continue to be found in fish/animals.
    pond
    a body of water usually smaller than a lake and larger than a pool either naturally or artificially confined.
    porous
    something which allows water to pass through it. 
    potable
    suitable, safe, or prepared for drinking. 
    potentiometric surface
    the surface to which water in an aquifer can rise by hydrostatic pressure. For karst aquifers like the Edwards, the potentiometric surface is not an especially meaningful concept. Every well is different, because of the complexity of the underground formation with many conduits, caverns, and different units separated by faults. The potentiometric surface is a more relevant measure when the aquifer involved is homogenous, such as one composed of gravel.
    ppb – parts per billion
    number of parts of a chemical found in one billion parts of a solid, liquid, or gaseous mixture. Equivalent to micrograms per liter (Ug/L).
    ppm – parts per million
    number of parts of a chemical found in one million parts of a solid, liquid, or gaseous mixture. Equivalent to milligrams per liter (mg/L).
    precipitate
    a solid which has come out of an aqueous solution. (ex., iron from groundwater precipitates to a rust colored solid when exposed to air).
    preservative
    a chemical added to a water sample to keep it stable and prevent compounds in it from changing to other forms or to prevent microorganism densities from changing prior to analysis.
    pretreatment
    processes used to reduce, eliminate, or alter the nature of wastewater pollutants from non-domestic sources before they are discharged into publicly owned treatment works (POTWs).
    price at equilibrium
    where supply and demand curves intersect. The price at equilibrium is what allocates resources.
    primary treatment
    mechanical treatment in which large solids are screened out and suspended solids in the sewage settle out as sludge. 
    prior appropriation
    a doctrine of water law that allocates the rights to use water on a first in time, first in right, basis.
    priority date
    the date of establishment of a water right. It is determined by adjudication of rights established before the passage of the Water Code. The rights established by application have the application date as the date of priority.
    profundal zone
    a lake’s deep-water region that is not penetrated by sunlight.
    public water system
    a system for the provision to the public of water for human consumption through pipes or other constructed conveyances.  In Texas, a public water system is one that serves at least 15 service connections or serve at least 25 individuals at least 60 days out of the year.
    publicly-owned treatment works (POTW)
    a wastewater treatment plant that is owned by a state, unit of local government or Indian tribe, usually designed to treat domestic wastewaters. The term also may include devices and systems used by those entities in the storage, treatment, recycling and reclamation of municipal sewage or liquid industrial wastes.
    puddle
    a small pool of water, usually a few inches in depth and from several inches to several feet in its greatest dimension.
    pump
    a device which moves, compresses, or alters the pressure of a fluid, such as water or air, being conveyed through a natural or artificial channel.
    pump station
    mechanical device installed in sewer or water system or other liquidcarrying pipelines to move the liquids to a higher level.
    pumped hydroelectric storage
    storing water for future use in generating electricity. Excess electrical energy produced during a period of low demand is used to pump water up to a reservoir. When demand is high, the water is released to operate a hydroelectric generator.
    pumping test
    a test conducted to determine aquifer or well characteristics.
    purge
    to force a gas through a water sample to liberate volatile chemicals or other gases from the water so their level can be measured.
    purgeable organics
    volatile organic chemicals which can be forced out of the water sample with relative ease through purging.
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    Water Resource Term Q

    Q

    quarry water
    the moisture content of freshly quarried stone, esp. if porous.
    quicksilver water
    a solution of mercury nitrate used in gilding.
    quickwater
    the part of a stream that has a strong current; an artificial current or bubbling patch of water just astern of a moving boat.
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    Water Resource Term R

    R

    rain
    water drops which fall to the earth from the air.
    rain gage
    any instrument used for recording and measuring time, distribution, and the amount of rainfall.
    radionuclide
    a radioactive particle, man-made or natural, with a distinct atomic weight number. Can have a very long life as a soil or water pollutant.
    radius of influence
    the radial distance from the center of a wellbore to the point where there is no lowering of the water table or potentiometric surface; the edge of the cone of depression.
    rating curve
    a graph showing the relationship between water surface elevation and discharge of a stream or river at a given location. Also called a stage-discharge curve.
    reach
    in general, a length of stream with relatively homogenous characteristics.
    recarbonization
    process in which carbon dioxide is bubbled into water being treated to lower the pH.
    receiving waters
    a river, ocean, stream, or other watercourse into which wastewater or treated effluent is discharged.
    recharge
    refers to water entering an underground aquifer through faults, fractures, or direct absorption.
    recharge rate
    the quantity of water per unit of time that replenishes or refills an aquifer.
    recharge zone
    the area where a formation allows available water to enter the aquifer. Generally, that area where the Edwards Aquifer and associated limestones crop out in Kinney, Uvalde, Medina, Bexar, Comal, Hays, Travis, and Williamson counties and the outcrops of other formations in proximity to the Edwards limestone, where faulting and fracturing may allow recharge of the surface waters to the Edwards Aquifer.
    reclaimed water
    domestic wastewater that is under the direct control of a treatment plant owner/operator which has been treated to a quality suitable for a beneficial use.
    recruitment
    survival of young plants and animals from birth to a life stage less vulnerable to environmental change.
    recurrence interval
    average amount of time between events of a given magnitude. For example, there is a 1% chance that a 100-year flood will occur in any given year.
    release
    as defined by the federal Superfund program, any spilling, leaking, pumping, pouring, emitting, emptying, discharging, injecting, escaping, leaching, dumping, or disposing into the environment of a hazardous or toxic chemical or extremely hazardous substance.
    remediation
    methods used to remove or contain a toxic spill or hazardous materials from a Superfund site; a generic term used to describe cleanup activities.
    reserves
    amount of a particular resource in known locations that can be extracted at a profit with present technology and prices.
    reservoir
    a pond, lake, tank, or basin (natural or human made) where water is collected and used for storage. Large bodies of groundwater are called groundwater reservoirs; water behind a dam is also called a reservoir of water.
    residual
    amount of a pollutant remaining in the environment after a natural or technological process has occurred.
    residual chlorine
    the available chlorine which remains in solution after the demand has been satisfied. 
    residual saturation
    saturation level below which fluid drainage will not occur.
    residue
    the dry solids remaining after the evaporation of a sample of water or sludge.
    resilience
    the ability of an ecosystem to maintain or restore biodiversity, biotic integrity, and ecological structure and processes following disturbance.
    Resource Conservation and Recovery Act (RCRA)
    a federal statute that requires the safe management and disposal of waste generated nationwide. RCRA was passed in 1976 as an amendment to the Solid Waste Disposal Act of 1956 and was last amended in 1984. The 1984 amendments are referred to as the Hazardous and Solid Waste Amendments (HSWA). There are three RCRA interrelated programs, which include: 1)the Solid Waste Program (Subtitle D) which sets criteria for municipal solid waste and other non-hazardous waste disposal facilities and prohibits open dumping of solid waste; 2)the Hazardous Waste Program (Subtitle C) which manages hazardous waste from the time it is generated until it is disposed (referred to as cradle to grave); and 3) the Underground Storage Tank Program (Subtitle I), which regulates underground storage, tanks storing petroleum or other hazardous substances.
    response variables
    environmental features of a river channel on a local or site-specific scale, such as channel shape, cross-sectional dimensions, substrate, bank shape, floodplain characteristics, vegetation, and channel patterns.
    retrofitting
    installing modern pollution control devices at facilities without making major changes to the facility’s design.
    return flow
    surface water that returns to the natural environment after diversion for beneficial uses, such as for irrigation.
    reverse osmosis
    a water treatment method whereby water is forced through a semipermeable membrane which filters out impurities.
    right of capture
    the idea that the water under a person’s land belongs to that person and they are free to capture and use as much as they want. Also called the “law of the biggest pump”.
    rill
    a small channel eroded into the soil by surface runoff; can be easily smoothed out or obliterated by normal tillage.
    riparian water right
    the legal right held by an owner of land contiguous to or bordering on a natural stream or lake, to take water from the source for use on the contiguous land.
    riparian zone
    a stream and all the vegetation on its banks.
    river
    a natural stream of water of considerable volume.
    river basin
    the area drained by a river and its tributaries.
    routing parameters
    coefficients that, along with mathematical routing equations, can be used to estimate the attenuation and lag (time delay) associated with the movement of flow through a length of stream channel.
    runoff
    surface water entering rivers, freshwater lakes, or reservoirs.
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    Water Resource Term S

    S

    safe yield
    the annual amount of water that can be taken from a source of supply over a period of years without depleting that source beyond its ability to be replenished naturally in “wet years.”
    saline water
    water containing more than 1,000 parts per million (ppm) of dissolved solids of any type.
    salinity
    amount of dissolved salts in a given volume of water.
    salt water intrusion
    the invasion of fresh surface or ground water by salt water. It may be called seawater intrusion if it comes from the ocean.
    salts
    minerals that cause salinity. Water may pick up salts as it passes through the air, over and under the ground, or as households and industry use it.
    sand filters
    devices that remove suspended solids from a wastewater treatment plant effluent or water treatment plant product.
    sanitary landfill
    landfill that is lined with plastic or concrete or located in clay-rich soils to prevent hazardous substances from leaking into the environment.
    sanitary sewers
    underground pipes that carry off only domestic or industrial waste, not storm water.
    saturated zone
    the area below the water table where all open spaces are filled with water under pressure equal to or greater than that of the atmosphere.
    saturation
    the condition of a liquid when it has taken into solution the maximum possible quantity of a given substance at a given temperature and pressure.
    scour
    the erosive action of running water in streams, which excavates and carries away material from the bed and banks. Or, pertaining to a place on a streambed scoured by running water.
    seal
    the impermeable material, such as cement grout bentonite, or puddling clay placed in the annular space between the borehole wall and the casing of a water well to prevent the downhole movement of surface water or the vertical mixing of artestian waters.
    secondary treatment
    second step in most waste treatment systems, in which bacteria break down the organic parts of sewage wastes; usually accomplished by bringing the sewage and bacteria together in trickling filters or in the activated sludge process. Compare primary treatment, tertiary treatment. 
    sediment
    soil particles, sand, and minerals washed from the land into aquatic systems as a result of natural and human activities.
    sediment trapping efficiency
    the ratio of sediment retained within the reservoir to the sediment inflow to the reservoir.
    sedimentary cycle
    biogeochemical cycle in which materials primarily are moved from land to sea and back again.
    sedimentation
    a large scale water treatment process where heavy solids settle out to the bottom of the treatment tank after flocculation.
    seep
    a spot where water contained in the ground oozes slowly to the surface and often forms a pool; a small spring.
    seepage
    percolation of water through the soil from unlined canals, ditches, laterals, watercourses, or water storage facilities.
    segment
    a water body or portion of a water body that is individually defined and classified. A segment is intended to have relatively homogenous chemical, physical, and hydrological characteristics.
    semi-confined aquifer
    an aquifer partially confined by soil layers of low permeability in which recharge and discharge can still occur.
    senescence
    the aging process. Sometimes used to describe lakes or other bodies of water in advanced stages of eutrophication. Also used to describe plants and animals.
    separate sewer
    a sewer system that carries only sanitary sewage, not stormwater runoff. When a sewer is constructed this way, wastewater treatment plants can be sized to treat sanitary wastes only and all of the water entering the plant receives complete treatment at all times. 
    septic system
    an on-site system designed to treat and dispose of domestic sewage. A typical septic system consists of a tank that receives waste from a residence or business and a system of drainage lines or a pit for disposal of the liquid effluent that remains after decomposition of the solids by bacteria in the tank.
    septic tank
    underground receptacle for wastewater from a home. The bacteria in the sewage decopose the organic wastes, and the sludge settles to the bottom of the tank. The effluent flows out of the tank into the ground through drain lines.
    settleable solids
    in sewage, suspended solids that will settle when the sewage is brought to a quiet state for a reasonable length of time, usually two hours.
    seven-day two-year low flow (7Q2)
    the lowest average streamflow for seven consecutive days within a recurrence interval of two years, as statistically determined from historical data. Used in wastewater discharge modeling and permitting to estimate the impact of an effluent discharge on a water body under low-flow conditions.
    sewage
    The waste and wastewater produced by residential and commercial sources and discharged into sewers.
    sewerage
    the entire system of sewage collection, treatment, and disposal.
    shear stress
    the frictional force per unit area exerted on a streambed by flowing water. An important factor in the movement of bed material and description of habitat for some organisms.
    short circuiting
    when some of the water in tanks or basins flows faster than the rest; shortcircuiting may result in shorter contact, reaction, or settling times than calculated or presumed.
    siltation
    the deposition of finely divided soil and rock particles upon the bottom of stream and river beds and reservoirs.
    sinking
    controlling oil spills by using an agent to trap the oil and sink it to the bottom of the body of water where the agent and the oil are biodegraded.
    skimming
    using a machine to remove oil or scum from the surface of the water.
    sleet
    precipitation which is a mixture of rain and ice.
    slickensides
    a smooth striated polished surface produced on rock by movement along a fault.
    sludge
    solid matter that settles to the bottom of sedimentation tanks in a sewage treatment plant and must be disposed of by digestion or other methods or recycled to the land.
    sludge digester
    tank in which complex organic substances like sewage sludge are biologically dredged. Energy is released and much of the sewage is converted to methane, carbon dioxide, and water.
    slurry
    a watery mixture of insoluble matter resulting from some pollution control techniques.
    snow
    precipitation in the form of branched hexagonal crystals, often mixed with simple ice crystals, which fall more or less continuously from a solid cloud sheet. These crystals may fall either separately or in cohesive clusters forming snowflakes.
    soft water
    any water that does not contain a significant amount of dissolved minerals such as salts of calcium or magnesium.
    soil erodibility
    An indicator of a soil’s susceptibility to raindrop impact, runoff, and other eroding processes.
    soil moisture
    the water contained in the pore space of the unsaturated zone.
    sole-source aquifer
    an aquifer that supplies 50 percent or more of the drinking water of an area.
    solubility
    the amount of mass of a compound that will dissolve in a unit volume of solution.
    solute
    any substance derived from the atmosphere, vegetation, soil, or rock that is dissolved in water.
    soil erosion
    the processes by which soil is removed from one place by forces such as wind, water, waves, glaciers, and construction activity and eventually deposited at some new place.
    species composition
    that portion of an Index of Biotic Integrity that is a metric measuring the number and identity of species.
    specific conductance
    a measure of the ability of a water to conduct an electrical current. Specific conductance is related to the type and concentration of ions in solution and can be used for approximating the dissolved solids concentration in water. In general, for the San Antonio River basin, conductivity * .6 approximates TDS. People monitoring water quality can measure electrical conductivity quickly in the field and estimate TDS without doing any lab tests at all. 
    specific heat
    the amount of heat required to raise the temperature of a kilogram of a substance (water) by 1 degree Celsius.
    specific yield
    the amount of water a unit volume of saturated permeable rock will yield when drained by gravity.
    spillway
    the channel or passageway around or over a dam through which excess water is diverted.
    spray irrigation
    application of finely divided water droplets to crops using artificial means.
    spring
    an issue of water from the earth; a natural fountain; a source of a body or reservoir of water.
    spring melt/thaw
    the process whereby warm temperatures melt winter snow and ice. Because various forms of acid deposition may have been stored in the frozen water, the melt can result in abnormally large amounts of acidity entering streams and rivers, sometimes causing fish kills.
    standard solution
    any solution in which the concentration is known.
    stagnation
    lack of motion in water that holds pollutants in place.
    state revolving funds (SRF)
    a program, capitalized in part by federal funds, that provides low-interest loans for construction of publicly owned wastewater treatment and water recycling facilities, for implementation of nonpoint source and storm drainage pollution control management programs, and for the development and implementation of estuary conservation and management programs.
    static water depth
    the vertical distance from the centerline of the pump discharge down to the surface level of the free pool while no water is being drawn from the pool or water table.
    static water level
    elevation or level of the water table in a well when the pump is not operating; the level or elevation to which water would rise in a tube connected to an artesian aquifer or basin in a conduit under pressure.
    steady-state mass balance
    the mathematical concept that the sum of upstream pollutant loads, each determined by the product of their concentration times flow, equals a resultant downstream load after mixing.
    stockpond
    a pond used primarily for watering livestock.
    STORET
    a national U.S. EPA computerized data base (Storage and Retrieval) containing both surface and groundwater chemistry data.
    stormwater discharge
    precipitation that does not infiltrate into the ground or evaporate due to impervious land surfaces but instead flows onto adjacent land or water areas and is routed into drain/sewer systems.
    stream
    a general term for a body of flowing water.
    stream piracy
    the tendency of one stream to capture the flow of another by eroding a channel that intercepts the other stream’s flow.
    stream power
    a measure of energy available to move sediment, or any other particle in a stream channel. It is affected by discharge and slope.
    stream segment
    refers to the surface waters of an approved planning area exhibiting common biological, chemical, hydrological, natural, and physical characteristics and processes. Segments will normally exhibit common reactions to external stress such as discharge or pollutants.
    streamflow
    the discharge that occurs in a natural channel.
    sub-basin
    in general, a portion of a river basin.
    subcritical flow
    flow characterized by low velocity and a Froude number less than 1. When the Froude number is less than 1, gravitational forces are greater than inertial forces.
    sublimation
    the transition of water directly from the solid state to the gaseous state, without passing through the liquid state; or vice versa. 
    subsidence
    sinking down of part of the earth’s crust due to underground excavation, such as removal groundwater.
    subsistence flows
    the component of an instream flow regime that represents infrequent, naturally occurring low flow events that occur for a seasonal period of time. They maintain water quality criteria and provide sufficient habitat to ensure organism populations capable of recolonizing the river system once normal, base flows return.
    supercritical flow
    flow characterized by high velocity and a Froude number greater than 1. When the Froude number is greater than 1, inertial forces are greater than gravitational forces.
    supercritical water
    a type of thermal treatment using moderate temperatures and high pressures to enhance the ability of water to break down large organic molecules into smaller, less toxic ones. Oxygen injected during this process combines with simple organic compounds to form carbon dioxide and water.
    supply
    a schedule that shows the various quantities of things offered for sale at various prices at a point in time. 
    surface impoundment
    an indented area in the land’s surface, such a pit, pond, or lagoon.
    surface irrigation
    application of water by means other than spraying such that contact between the edible portion of any food crop and the irrigation water is prevented.
    surface water
    water that flows in streams and rivers and in natural lakes, in wetlands, and in reservoirs constructed by humans.
    suspended load
    specific sediment particles maintained in the water column by turbulence and carried with the flow of water.
    suspended solids
    the small solid particles in water that cause turbidity. Particles of suspended sediment tend to settle at the channel bottom, but upward currents in turbulent flow counteract gravitational settling.
    sustainability
    the long-term capacity of an ecosystem to maintain ecological processes and functions, biological diversity, and productivity.
    sustainable management
    method of exploiting a resource that can be carried on indefinitely. Removal of water from an aquifer in excess of recharge is, in the long term, not a sustainable management method.
    sustained overdraft
    long term withdrawal from the aquifer of more water than is being recharged.
    swamp
    a type of wetland dominated by woody vegetation but without appreciable peat deposits. Swamps may be fresh or salt water and tidal or non-tidal.
    synthetic organic chemicals (SOCs)
    man-made organic chemicals. Some SOCs are volatile, while others tend to stay dissolved in water instead of evaporating.
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    Water Resource Term T

    T

    tail water
    the runoff of irrigation water from the lower end of an irrigated field.
    tailings pond
    An excavated or diked area that is intended to contain liquid and solid wastes from mining and milling operations.
    tailrace
    The channel that is downstream of the draft tube that carries the water discharged from a turbine. The draft tube is the discharge section of the turbine.
    technology-based treatment requirements
    NPDES permit requirements based on the application of pollution treatment or control technologies including BTP (best practicable technology), BCT (best conventional technology), BAT (best available technology economically achievable), and NSPS (new source performance standards).
    tertiary treatment
    removal from wastewater of traces or organic chemicals and dissolved solids that remain after primary treatment and secondary treatment.
    thalweg
    the line of maximum depth in a stream. The thalweg is the part that has the maximum velocity and causes cutbanks and channel migration.
    thermal gradient
    temperature difference between two areas.
    thermal pollution
    an increase in air or water temperature that disturbs the climate or ecology of an area.
    thermocline
    fairly thin zone in a lake that separates an upper warmer zone (epilimnion) from a lower colder zone (hypolimnion).
    threatened species
    Under the Federal Endangered Species Act, animal populations may be determined to be either threatened or endangered. Populations listed as threatened are less severely depleted than populations classed as endangered.
    threshold pollutant
    substance that is harmful to a particular organism only above a certain concentration, or threshold level.
    tidal marsh
    low, flat marshlands traversed by channels and tidal hollows, subject to tidal inundation; normally, the only vegetation present is salt-tolerant bushes and grasses.
    TDS – total dissolved solids
    the sum or all inorganic and organic particulate material. TDS is an indicator test used for wastewater analysis and is also a measure of the mineral content of bottled water and groundwater. There is a relationship between TDS and conductivity. In general, for the San Antonio River basin, TDS/.6 approximates conductivity. Or, conductivity * .6 approximates TDS. People monitoring water quality can measure electrical conductivity quickly in the field and estimate TDS without doing any lab tests at all.
    Total Maximum Daily Load (TMDL)
    a calculation of the maximum amount of a pollutant that a waterbody can receive and still meet water quality standards, and an allocation of that amount to the pollutant’s sources.
    toxaphene
    chemical that causes adverse health effects in domestic water supplies and is toxic to fresh water and marine aquatic life.
    toxic hot spot
    location in enclosed bay, estuary, or any adjacent waters that has toxic pollution problems in the water or sediment in excess of applicable standards.
    toxic pollutant
    those pollutants or combinations of pollutants, including disease-causing agents, which after discharge and upon exposure, ingestion, inhalation or assimilation into any organism can, on the basis of information available, cause death, disease, behavioral abnormalities, cancer, genetic mutations, physiological malfunctions or physical deformation in such organism or their offspring. The quantities and exposures necessary to cause these effects can vary widely.
    Toxicity Reduction Evaluation(TRE)
    a study conducted to determine the source(s) of toxicity in a discharge effluent so that these sources can be controlled sufficiently to allow a discharger to comply with their permit limits.
    toxicity test
    the means to determine the toxicity of a chemical or an effluent using living organisms. A toxicity test measures the degree of response of an exposed test organism to a specified chemical or effluent.
    Tragedy of the Commons
    the idea that no one takes responsibility for things that everybody owns.
    transmissivity
    refers to the rate at which limestone allows the transmission of water. Limestone can be highly porous, but not very transmissive if the pores are not connected to each other. Technically speaking, it is the rate at which water is transmitted through a unit width of aquifer under unit hydraulic gradient. Transmissivity is directly proportional to aquifer thickness, thus it is high where the Edwards is thick and low where it is thin, given the same hydraulic conductivity.
    transpiration
    direct transfer of water from the leaves of living plants to the atmosphere.
    transport capacity
    the capacity of a river to carry sediment in suspension or to move sediment along the riverbed.
    treatment
    any method, technique, or process designed to remove solids and/or pollutants from solid waste, waste-streams, and effluents.
    trickle irrigation
    method in which water drips to the soil from perforated tubes or emitters.
    trickling filter
    a treatment system in which wastewater is trickled over a bed of stones or other material covered with bacteria that break down the organic waste and produce clean water.
    tributary
    a stream that contributes its water to another stream or body of water.
    trihalomethanes (THM)
    chemical compounds in which three of the four hydrogen atoms of methane (CH4) are replaced by halogen atoms. Widely used in industry as solvents or refrigerants. THMs are also environmental pollutants, and many are considered carcinogenic. THMs are generally by-products of chlorination of drinking water that contains organic material.
    trophic composition
    that portion of an Index of Biotic Integrity that is a metric measuring the proportion of species and proportions of omnivores, insectivores, and omnivores.
    trophic structure
    the feeding relationships among species within a food web.
    troposphere
    the layer of atmosphere closest to the Earth, extending seven to ten miles above the surface, containing most of the clouds and moisture.
    tube settler
    device using bundles of tubes to let solids in water settle to the bottom for removal by conventional sludge collection means. Sometimes used in sedimentation basins and clarifiers to improve particle removal.
    tuberculation
    development or formation of small mounds of corrosion products on the inside of iron pipe. These tubercles roughen the inside of the pipe, increasing its resistance to water flow.
    turbid
    thick or opaque with matter in suspension. Rivers and lakes may become turbid after a rainfall.
    turbidimeter
    a device that measures the cloudiness of suspended solids in a liquid; a measure of the quantity of suspended solids.
    turbidity
    a cloudy condition in water due to suspended silt or organic matter.
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    Water Resource Term U

    U

    USGS
    United States Geological Survey
    unclassified waters
    those waters for which no classification has been assigned and which have not been identified in Appendix A of 31 Texas Administrative Code, Chapter 307.10 of Title 31 (relating to definitions).
    unconfined aquifer
    an aquifer containing water that is not under pressure; the water level in a well is the same as the water table outside the well. 
    unconsolidated formations
    naturally occurring earth formations that have not been lithified. Alluvium, soil, gravel, clay, and overburden are some of the terms used to describe this type of formation.
    undercurrent
    a current below the upper currents or surface of a fluid body.
    underdrain
    a concealed drain with openings through which the water enters when the water table reaches the level of the drain.
    underflow
    movement of water through subsurface material.
    undertow
    the current beneath the surface that sets seaward or along the beach when waves are breaking on the shore.
    underwater
    under the surface of the water; lying, growing, performed, worn, or operating below the surface of the water, as underwater caverns, underwater operation of a submarine.
    unsaturated zone
    the area above the water table where soil pores are not fully saturated, although some water may be present.
    upflow
    an upward flow.
    urban runoff
    storm water from city streets and adjacent domestic or commercial properties that carries pollutants of various kinds into the sewer systems and receiving waters.
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    Water Resource Term V

    V

    vadose zone
    the zone between land surface and the water table where the moisture content is less than saturation (except in the capillary fringe) and pressure is less than atmospheric. Soil pore space also typically contains air or other gases. The capillary fringe is included in the vadose zone.
    validation
    comparison of computer model results with a set of data that were not used for calibration.
    vapor plumes
    flue gases that are visible because they contain water droplets.
    vegetative controls
    non-point source pollution control practices that utilize vegetative cover to reduce erosion and minimize loss of pollutants.
    vested water right
    the right granted by a state water agency to use either surface or ground water.
    virgin flow
    the streamflow which exists or would exist if man had not modified the conditions on or along the stream or in the drainage basin.
    void
    the pore space or other openings in rock. The openings can be very small to cave size and are filled with water below the water table.
    volatile organic compounes (VOCs)
    a group of chemicals that react in the atmosphere with nitrogen oxides, heat and sunlight to form ozone; VOCs are referred to as hydrocarbons.
    volatility
    the tendency of a liquid to evaporate.
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    Water Resource Term W

    W

    wasteload allocation
    term used in conjunction with the TMDL Program, a WLA is the portion of a receiving water’s loading capacity that is allocated to one of its existing or future point sources of pollution. Discharge limits are usually required for the specific water quality criterion addressed by the TMDL.
    wastewater
    water containing waste including greywater, blackwater or water contaminated by waste contact, including process-generated and contaminated rainfall runoff.
    water
    the liquid that descends from the clouds as rain; forms streams, lakes, and seas, and is a major constituent of all living matter. It is an odorless, tasteless, colorless, very slightly compressible liquid.
    water availability model
    a numerical surface water flow model used to determine the availability of surface water for water right permitting.
    water column
    an imaginary column extending through a water body from its floor to its surface. Ambient water quality monitoring programs may seek to quantify the water quality of a representative water column. Samples may be taken from a point or points throughout the depth of the water column.
    water cycle
    natural pathway water follows as it changes between liquid, solid, and gaseous states; biogeochemical cycle that moves and recycles water in various forms through the ecosphere. Also called the hydrologic cycle.
    water pollution
    degradation of a body of water by a substance or condition to such a degree that the water fails to meet specified standards or cannot be used for a specific purpose.
    water purveyor
    a public utility, mutual water company, county water district, or municipality that delivers drinking water to customers.
    water quality
    the chemical, physical, biological, radiological, and thermal condition of water.
    water quality-based toxics control
    an integrated strategy used in NPDES permitting to assess and control the discharge of toxic pollutants to surface waters. There are two approaches: the whole-effluent approach involves the use of toxicity tests to measure discharge toxicity; the chemical specific approach involves the use of water quality criteria or State standards to limit specific toxic pollutants directly.
    water quality criteria
    scientifically derived ambient limits developed and updated by EPA, under section 304(a)(1) of the Clean Water Act, for specific pollutants of concern. Criteria are recommended concentrations, levels, or narrative statements that should not be exceeded in a waterbody in order to protect aquatic life or human health.
    water quality standards
    laws or regulations, promulgated under Section 303 of the Clean Water Act, that consist of the designated use or uses of a waterbody or a segment of a waterbody and the water quality criteria that are necessary to protect the use or uses of that particular waterbody. Water quality standards also contain an antidegradation statement. Every State is required to develop water quality criteria standards applicable to the various waterbodies within the State and revise them every 3 years.
    water recycling
    the treatment of wastewater making it suitable for reuse.
    water solubility
    the maximum possible concentration of a chemical compound dissolved in water.
    water-soluble substance
    a substance that can readily disperse through the environment.
    water supplier
    one who owns or operates a public water system.
    water surface elevation
    the elevation of a water surface above or below an established reference level, such as sea level.
    water table
    level below the earth’s surface at which the ground becomes saturated with water. The surface of an unconfined aquifer which fluctuates due to seasonal precipitation.
    water table aquifer
    an aquifer confined only by atmospheric pressure (water levels will not rise in the well above the confining bed).
    water well
    any artificial excavation constructed for the purpose of exploring for or producing ground water.
    Water Year
    a division based on a general pattern of annual wet and dry periods rather than a calendar year. In Texas, the Water Year is from October 1 through September 30. The Water Year is designated by the calendar year in which it ends. Thus, the year ending September 30, 2009 is called the 2009 Water Year.
    waterfall
    a sudden, nearly vertical drop in a stream, as it flows over rock.
    waterlogging
    saturation of soil with irrigation water so the water table rises close to the surface.
    watermaster
    An employee of a water department who distributes available water supply at the request of water right holders and collects hydrographic data.
    watershed
    land area from which water drains toward a common watercourse in a natural basin.
    watershed approach
    a coordinated framework for environmental management that focuses public and private efforts on the highest priority problems within hydrologically defined geographic areas.
    watershed management
    sater resource protection, enhancement, and restoration. Ideally, watershed management means developing a solution for each watershed that considers all its problems, includes all stakeholders in defining the problems, proposing solutions, and participating in implementing a common solution.
    weather
    day to day variation in atmospheric conditions. 
    weir
    a wall or plate placed in an open channel to measure the flow of water; a wall or obstruction used to control flow from settling tanks and clarifiers to ensure a uniform flow rate and avoid short-circuiting.
    well
    a bored, drilled, or driven shaft or a dug hole whose depth is greater than the largest surface dimension and whose purpose is to reach underground water supplies or oil or to store or bury fluids below ground.
    wellfield
    area containing one or more wells that produce usable amounts of water or oil.
    well injection
    the subsurface placement of fluids into a well.
    well monitoring
    measurement by on-site instruments or laboratory methods of well water quality.
    well plug
    a seal installed in a borehole or well preventing movement of fluids.
    wellhead protection area
    a protected surface and subsurface zone surrounding a well or well field supplying a public water system to keep contaminants from reaching the well water.
    wetland
    area that is regularly wet or flooded and has a water table that stands at or above the land surface for at least part of the year, such as a bog, pond, fen, estuary, or marsh.
    wettability
    the degree to which a fluid will spread into or coat a solid surface in the presence of other fluids into which it will not dissolve.
    wettable powder
    dry formulation that must be mixed with water or other liquid before it is applied.
    whole-effluent toxicity
    the aggregate toxic effect of an effluent measured directly by a toxicity test.
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    Water Resource Term X

    X

    xeriscape
    creative landscaping for water and energy efficiency and lower maintenance. The seven xeriscape principles are: good planning and design; practical lawn areas; efficient irrigation; soil improvement; use of mulches; low water demand plants; good maintenance.
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    Water Resource Term Y

    Y

    yield
    the quantity of water expressed either as a continuous rate of flow (cubic feet per second, etc.) or as a volume per unit of time. It can be collected for a given use, or uses, from surface or groundwater sources on a watershed.
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    Water Resource Term Z

    Z

    zone of aeration
    a region in the Earth above the water table. Water in the zone of aeration is under atmospheric pressure and will not flow into a well.
    zone of saturation
    the space below the water table in which all the interstices (pore spaces) are filled with water. Water in the zone of saturation is called groundwater.
    zooplankton
    tiny aquatic animals eaten by fish.

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    Water Resource Infographics

    Water education – Ground water contamination Infographic

    Water education – Ground water contamination

    Classroom Infographic presentation for K1-5

    Right click on image and view image to enlarge Groundwater can become contaminated in many ways. If rain water or surface water comes into contact with contaminated soil while seeping into the ground, it can become polluted and can carry the pollution from the soil to the groundwater. Groundwater can also become contaminated when liquid hazardous substances themselves soak down through the soil or rock into the groundwater. Some liquid hazardous substances do not mix with the groundwater but remain pooled within the soil or bedrock. These pooled substances can act as long-term sources of groundwater contamination as the groundwater flows through the soil or rock and comes into contact with them.
    STEM science education for classroom presentation K-5

    If used on educational site please give following credit: Save the Water™, DILOS™ program. STEM science education 2013 -
    sources:
    www.Savethewater.org
    www.epa.gov
    www.legalexaminer.com
    www.precisionnutrition.com
    www.ec.gc.ca
    www.ecwa.org Top of page

    Save the Water Dictionary

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    Special May 10, 2013 Anniversary Edition: 5,450 water education resource and news article directory – STEM science – education research reference guide for students and teachers.

    STW™ anniversary edition: Water education resource and news article directory

    Save the Water™ is committed to the education of present and future generations to insure the protection and conservation of water. Without clean drinking water, no species plant, animal or human can be saved. We must insure that the water is not contaminated to the point where we can no longer drink it.

    You will find 5,450 links to organizations that provide valuable information about water science, research, education and sanitation. The educational resource is extensive, it has been divided into categories listed below so you can navigate to pertinent information according to your needs. (Click on header or image to navigate). Below the education resource section is a directory to the complete STW™ site for research and teaching purposes. Whether you use these resources for research or education, we hope that you become part of the solution that will bring clean healthy water for all people regardless of their social or economic status.


    Junior Resources


    Save The Water And Junior Water Education
     

    General Water Resource Index

    Click here to go to water resource index

    Fracking Infographics

    Click Here to go to Fracking Infograhics

    Tribal Water Resource Directory

    Click here to go to Tribal Resource Directory


    Intermediate Resources


    Animated_book_worm

    Chemical Facts

    Click here to go to chemical facts

    Microscopic Images

    Click here to go to Microscopic images

    Microorganism Videos

    Click here to go to microscope videos


    Senior Teaching Resources


    STEM Senior water resourses

    Water Facts

    Click here to go to water facts

    Fracking Defined

    Click here to go to Fracking defined

    Research and Post Archives

    Click here to go to post archives


    STEM water science education


    Click here to go to STEM water science education


    DILOS™ program

    Click here to go to DILOS program

    STEM K-8 water science videos

    Click here to go to STEM water science videos K-8


    DILOS™ field trip

    Click here to go to Dilos Field Trip

    STEM water infographics

    CLick here to go to STEM water infographics


    DILOS™ K-4 classroom presentation

    Click here to go to DILOS CLASSROOM PRESENTATION

    STEM K-4 water science music videos

    Click here to go to STEM water science music videos

    Directory to STW™ site – 850 pages of global water news, research and education: Click here.

    Directory to STW™ site – 850 pages of global water news, research and education.

    Updated May 10, 2013
    [Most current articles: left column]

    All the Save the Water™ Static Pages

     

    Current Postings / Updated May 10, 2013/ 750 articles and growing daily.

    May 2013

    February 2013

    January 2013

    December 2012

    Current Posts

    November 2012

    Current Postings

      October 2012

    • Contaminated drinking water: Risk of viral acute gastrointestinal illness from nondisinfected drinking water distribution systems.
    • Water news: Clean Water Act turns 40.
    • Water news: India – Pictorial – Chand Baori step well in Rajasthan, India. In a country plagued with a water crisis a wondrous water history lays hidden.
    • Water news: India – WaterFilters.NET provides aid during global water crisis.
    • Haritika / STW™ Humanitarian Partnership
    • Contaminated water: EPA Finalizes cleanup plan for Shenandoah Road Superfund Site in East Fishkill, New York.
    • Drinking water: Drinking water problem – the case against water fluoridation.
    • Water crisis: India – Quenching the thirst of a growing nation.
    • Plant Based Plastics
    • Water contamination: New Report confirms fracking is reckless.
    • Contaminated drinking water: VA denies most compensation claims from toxic water wells – Marine veterans left to their own resources.