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Drinking water contamination news. Fracking causes rumbles in California. [Rt.Com]

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Californias unregulated fracking problem

Fracking rumbles California

A gas flare burns at a fracking site (REUTERS/Stringer)
California is one of the largest oil and gas producing states in the US. As the Golden State cashes in on the boom, the oil and gas industry is increasingly using fracking.

Last year about a quarter of all the oil and gas wells drilled in California were fracked and with no regulation in place, companies are rushing to dig some more. California is prone to droughts and earthquakes, leaving residents worried about how fracking could affect their water supply and the potential for an earth shaking disaster.

Southern California is known for its pristine coastline, but just a few miles away from the ocean lays a one-thousand acre oil field, right in the middle of Los Angeles.

“I didn’t buy here thinking this was going to happen in my backyard. I would have had second thoughts about living here,” said Gary Gless, a Los Angeles resident who lives just a few miles from the Inglewood Oil Field.

Gless and his neighbors are seeing their dream homes crack before their eyes and they blame the increased production at the oil fields next door.

When homeowners moved in, they say they were assured the wells were dry. Following recent methane leaks, however, residents found out that drilling picked up, and that the exploration company, PXP, is actually using fracking to extract oil.

“Fracking is happening completely unregulated in the state of California,” said Brenna Norton, an organizer with Food and Water Watch. “Oil and gas companies don’t have to say where they frack or what chemicals they are injecting into water, possibly close to your drinking water,” Norton added.

Fracking, or hydraulic fracturing, is the process of pumping high-pressure water, chemicals and solids into the ground to fracture the rock, and extract fuel that would otherwise be unavailable.

PXP, which operates the largest urban oil field in America, is conducting its own study as to what sort of effects fracking will have on this neighborhoodBut neighbors here are worried they will never have true answers about what is really happening underneath their homes.

“Wastewater injection from fracking is linked to earthquakes and property damage. The US geological survey linked wastewater wells from fracking to earthquakes,” said Norton.

The concern over seismic activity is especially high in the Los Angeles area because of the oil field’s proximity to the Newport-Inglewood fault, which according to the Federal Emergency Management Agency, has the potential of a 7.4 magnitude earthquake.

“In many places where you have large amounts of water injected in broken rock, it tends to move either on the surface or in depth,” said Dr. Tom Williams, a retired geologist and oil industry insider.

That movement, experts say, could pose a danger to an area all too familiar with disaster.

In 1963, the Baldwin Hills Reservoir collapsed, killing five people and destroying 60 homes. Geologists concluded that decades of extraction in the neighboring oil field led to the rupture in the dam.

Today, cracked foundations and buckling roadways have neighbors worried about losing their homes.

“The foundation, I don’t know what is going on under my house. If we do get an earthquake, I’m sure that with all these cracks it will probably rip it all open,” said Los Angeles resident Rosa Tatum.

“The state couldn’t afford any type of damage, not just from the earthquakes but the millions of gallons of contaminated water that they’ll be pumping into the ground,” said Gless.

The oil and gas industry has launched a public relations campaign claiming fracking is safe since it has been happening for decades.

“1.2 million times that fracking has occurred in this country there has not been a single incident of reported of water contamination,” said Dave Quast, from Energy in Depth, an advocacy group for the oil and gas industry.

Quast’s claims come after US Environmental Protection Agency report in Wyoming, in which federal regulators said fracking was the probable cause of tainted water supplies.

The industry has also launched an offensive to confront regulation and criticism.

“These fossil fuel giants influence policy enormously. They spent $747 million lobbying Congress to get this Safe Water Drinking Act exemption. That is a contamination of our democracy,” said Josh Fox, director of the Oscar nominated documentary, “Gasland”

The efforts of big oil and gas have only emboldened the anti-fracking movement on the west coast of the US, as activists and community members attempt to ban the controversial drilling technique in California.

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    Fracking
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    Save the Water™ Questions and Answers: Can fracking in the USA be cleaned up? [Kevin Bullis/Technology Review]

    Savethewater Questions and Answers


    Questions and Answers
    Vol.III
    No.19

     

    Despite many successful water projects, billions of people still lack adequate water and sanitation

    savethewater”,   “save the water”, “what is contaminated water”, “dirty water”, “water research”, “water”, “clean water”, “safe water”, “drinking water”, “water treatment”, “water testing”, “water analysis”, “bacteria”, “fluoride”, “pesticides”, “herbicides”, “organic chemicals”, “arsenic”, “ inorganic chemicals”,  “tap water”

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    Question: Can fracking be cleaned up?


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    Save the water. Can fracking be stopped

    Fracking site: Trucks at a well in Pennsylvania pump high-pressure fracking fluid down the well to free natural gas from the shale formation far below the surface.Les Stone/ Corbis

    The International Energy Agency says yes, but it will take tougher regulations that force producers to apply the latest technologies.

      Tuesday, June 5, 2012/By Kevin Bullis

    Fracking, aka hydraulic fracturing, a process for freeing natural gas locked in shale deposits, has caused a boom in natural-gas production in the United States. But some experts worry that the practice results in contaminated drinking water and the release of methane, prompting some localities to limit shale-gas production.

    A new analysis by the International Energy Agency says technologies exist—or are in development—that could largely address these concerns. If they’re adopted, fracking could be more widely accepted by governments around the world, leading to lower greenhouse-gas emissions and lower energy prices. It they’re not, governments could balk, and coal would maintain its dominant place in electricity generation.

    The most well-known issue associated with fracking is concern over water use and contamination. Fracking consumes large amounts of water; roughly 20 million liters under high pressure are sent down each well to create the fractures in the rock that free the natural gas. That water use is a huge concern in places such as Texas and some areas of China that have large shale-gas resources and are prone to droughts.

    Disposal of that wastewater is another concern. Fracking also has the potential to contaminate drinking water supplies and increase air pollution. And there are concerns that it could actually increase greenhouse-gas emissions due to methane leaks.

    But the IEA report concludes that fracking, like many other practices in industries that involve hazardous chemicals, can be made relatively safe with regulation. The IEA estimates that the measures needed to make fracking safer would add about 7 percent to the cost of an average well.

    Significant levels of methane, the main component of natural gas, have been found in drinking-water supplies near some fracking sites. Some environmentalists have suggested that the fracking process, which creates fractures in shale, could create a path for natural gas and other chemicals to reach aquifers and mix with drinking water.

    But according to the IEA report, that doesn’t seem to be the problem in most cases. Fracking usually takes place hundreds of meters below aquifers, and it’s easy to stop the propagation of fractures. Cracking the rock requires high pressures. Stop applying the pressure, and the rock fracturing stops. However, some fracking sites are relatively near to the level of drinking water, and the IEA suggests it might make sense to ban the procedure at such locations.

    The IEA says the contaminated water is most likely the result of producers building substandard natural-gas wells, which are lined with metal casings and cement to keep the natural gas from contaminating aquifers. But in some cases, producers have done a poor job of cementing, allowing channels for natural gas to form. “Whenever there was a gas leakage, it came out because the cement was not well done,” says Franz-Josef Ulm, a civil and environmental engineering professor at MIT. That problem could be solved by cementing properly and then carefully monitoring the well’s integrity. “When it comes to cementing, the solutions are out there. The question is whether they are being applied,” Ulm says.

    New technology could greatly reduce the amount of pressure needed for fracking, making it far easier to build safe wells, Ulm says. Researchers are learning that shale is particularly fracture-resistant because of the presence of a small amount of organic material that binds together inorganic particles. Targeting these materials by applying a special solvent could weaken the shale and make it far easier to free the natural gas.

    There are also opportunities to reduce water use by using fluids other than water—such as propane (which brings its own environmental challenges)—or mixing carbon dioxide or nitrogen with water to create foams. Eventually it may be possible to mix small amounts of water with solid particles designed to easily flow, Ulm says.

    Another contamination fear involves the chemicals that fracking companies add to the water. The biggest concern isn’t the chemicals once they’re mixed with the water, since they’re so dilute, but rather the handling of the chemicals in concentrated form. Spills on the surface could soak into the ground and contaminate drinking water. The solution is to line the area where chemicals are handled with plastic and monitor any leaks. Researchers are also developing less-toxic chemicals, or techniques to eliminate the need for them.

    Yet even if these chemicals can be dealt with, wastewater remains a challenge. The water that flows back to the surface is contaminated not only with the chemicals originally mixed in at the surface, but also with chemicals, heavy metals, and, in some cases, naturally occurring radioactive materials from deep underground.

    As the water returns to the surface, natural gas and other hydrocarbons that were released by the fracking come with it. In many cases, that gas is allowed to escape into the atmosphere until the water stops flowing. The main component of natural gas—methane—is a greenhouse gas many times more powerful than carbon dioxide, so this practice could offset any greenhouse-gas emissions reductions that would come from burning natural gas rather than coal. However, simple technology exists to capture the natural gas at this stage.

    Implementing these technologies will likely require regulation. “It can’t just be counting on companies to adopt best practices, because you’ll only have a certain percentage of the well operators doing it,” says Mark Boling, president of V+ Development Solutions, which is part of Southwestern Energy, a natural-gas producer. “You have to go the rest of the way and get regulations in place so that you have a level playing field and everyone is required to do the same thing.”

    If done right, those regulations could drive innovation by creating a market for new technologies. Ulm recommends caps on emissions that give companies flexibility to choose the best technology. The IEA calls for a combination of such caps, and in some cases specific technology requirements. “With such regulations, you could force innovation to be implemented at a high pace. Technology is what it will take to make shale gas a sustainable resource,” Ulm says.

    Definitions From Wikipedia

    Save the Water™ does not represent or endorse the definitions posted herein or reliability of any advice, opinion, statement, or other information furnished by the author. It is meant for further research by you the reader.

    Hydraulic fracturing

    From Wikipedia, the free encyclopedia
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    Hydraulic fracturing
    Process type Mechanical
    Industrial sector(s) Mining
    Main technologies or sub-processes Fluid pressure
    Product(s) Natural gas
    Petroleum
    Inventor Floyd Farris; J.B. Clark (Stanolind Oil and Gas Corporation)
    Year of invention 1947

    Hydraulic fracturing is the propagation of fractures in a rock layer caused by the presence of a pressurized fluid. Some hydraulic fractures form naturally, as in the case of veins or dikes, and are a means by which gas and petroleum from source rocks may migrate to reservoir rocks. Induced hydraulic fracturing or hydrofracking, commonly known as fracking, is a technique used to release petroleum, natural gas (including shale gas, tight gas and coal seam gas), or other substances for extraction.[a][1] This type of fracturing creates fractures from a wellbore drilled into reservoir rock formations.

    The first use of hydraulic fracturing was in 1947, though the fracking technique which made the shale gas extraction economical was first used in 1997 in the Barnett Shale in Texas.[1][2][3] The energy from the injection of a highly-pressurized fracking fluid creates new channels in the rock which can increase the extraction rates and ultimate recovery of fossil fuels.

    Proponents of fracking point to the vast amounts of formerly inaccessible hydrocarbons the process can extract.[4] Detractors 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.[5] For these reasons hydraulic fracturing has come under scrutiny internationally, with some countries suspending or even banning it.

    Geology

    Mechanics

    Fracturing in rocks at depth is suppressed by the confining pressure, due to the load caused by the overlying rock strata. This is particularly so in the case of ‘tensile’ (Mode 1) fractures, which require the walls of the fracture to move apart, working against this confining pressure. Hydraulic fracturing occurs when the effective stress is reduced sufficiently by an increase in the pressure of fluids within the rock, such that the minimum principal stress becomes tensile and exceeds the tensile strength of the material.[6][7] Fractures formed in this way will typically be oriented perpendicularly to the minimum principal stress and for this reason, induced hydraulic fractures in wellbores are sometimes used to determine stress orientations.[8] In natural examples, such as dikes or vein-filled fractures, their orientations can be used to infer past stress states.[9]

    Veins

    Most vein systems are a result of repeated hydraulic fracturing during periods of relatively high pore fluid pressure. This is particularly clear in the case of ‘crack-seal’ veins, where the vein material can be seen to have been added in a series of discrete fracturing events, with extra vein material deposited on each occasion.[10] One mechanism to explain such examples of long-lasting repeated fracturing is the effects of seismic activity, in which the stress levels rise and fall episodically and large volumes of fluid may be expelled from fluid-filled fractures during earthquakes. This process is referred to as ‘seismic pumping’.[11]

    Dikes

    High-level minor intrusions such as dikes propagate through the crust in the form of fluid-filled cracks, although in this case the fluid is magma. In sedimentary rocks with a significant water content the fluid at the propagating fracture tip will be steam.[12]

    History

    Fracturing as a method to stimulate shallow, hard rock oil wells dates back to the 1860s. It was applied by oil industries in 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 a well stimulation was introduced in the 1930s. Due to acid etching, created fractures would not close completely and therefore enhanced productivity. The same phenomenon was discovered with water injection and squeeze cementing operations.[13]

    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.[13][1] 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.[13] Since then, hydraulic fracturing has been used to stimulate approximately a million oil and gas wells.[14]

    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. [15]

    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 federal government initiated both the Eastern Gas Shales Project, a set of dozens of public-private hydro-fracturing pilot demonstration projects, and the Gas Research Institute, a gas industry research consortium that received approval for research and funding from the Federal Energy Regulatory Commission.[16] 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’ that made the shale gas extraction economical.

    In 2011, France became the first nation to ban the hydraulic fracturing.[18][19]

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    Save the Water™ Questions and Answers: Can frack toxins migrate to aquifers?Study shows more immediate drilling danger. Predicts frack toxins can migrate to aquifers within years

    Savethewater Questions and Answers


    Questions and Answers
    Vol.III
    No.18

     

    Despite many successful water projects, billions of people still lack adequate water and sanitation

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    Updated May 3, 2012
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    Predicts frack toxins can migrate to aquifers within years

    Save the Water™ does not represent or endorse the postings herein or reliability of any advice, opinion, statement, or other information furnished by the author.

    Save the water fracking fluidsStudy shows more immediate drilling danger

    Published May 3, 2012 at 6:01 am (Updated May 3, 2012)

    NEW YORK — A new study has raised fresh concerns about the safety of gas drilling in the Marcellus Shale, concluding that fracking chemicals injected into the ground could migrate toward drinking water supplies far more quickly than experts have previously predicted, the investigative news site, ProPublica.com reports.

    More than 5,000 wells were drilled in the Marcellus between mid-2009 and mid-2010, according to the study, which was published in the journal Ground Water two weeks ago. Operators inject up to 4 million gallons of fluid, under more than 10,000 pounds of pressure, to drill and frack each well.

    Scientists have theorized that impermeable layers of rock would keep the fluid, which contains benzene and other dangerous chemicals, safely locked nearly a mile below water supplies. This view of the earth’s underground geology is a cornerstone of the industry’s argument that fracking poses minimal threats to the environment.

    But the study, using computer modeling, concluded that natural faults and fractures in the Marcellus, exacerbated by the effects of fracking itself, could allow chemicals to reach the surface in as little as “just a few years.”

    “Simply put, are not impermeable,” said the study’s author, Tom Myers, an independent hydrogeologist whose clients include the federal government and environmental groups.

    “The Marcellus shale is being fracked into a very high permeability,” he said. “Fluids could move from most any injection process.”

    The research for the study was paid for by Catskill Mountainkeeper and the Park Foundation, two upstate New York organizations that have opposed gas drilling and fracking in the Marcellus.

    Much of the debate about the environmental risks of gas drilling has centered on the risk that spills could pollute surface water or that structural failures would cause wells to leak.

    Though some scientists believed it was possible for fracking to contaminate underground water supplies, those risks have been considered secondary. The study in Ground Water is the first peer-reviewed research evaluating this possibility.

    The study did not use sampling or case histories to assess contamination risks. Rather, it used software and computer modeling to predict how fracking fluids would move over time. The simulations sought to account for the natural fractures and faults in the underground rock formations and the effects of fracking.

    The models predict that fracking will dramatically speed up the movement of chemicals injected into the ground. Fluids traveled distances within 100 years that would take tens of thousands of years under natural conditions. And when the models factored in the Marcellus’ natural faults and fractures, fluids could move 10 times as fast as that.

    Where man-made fractures intersect with natural faults, or break out of the Marcellus layer into the stone layer above it, the study found, “contaminants could reach the surface areas in tens of years, or less.”

    The study also concluded that the force that fracking exerts does not immediately let up when the process ends. It can take nearly a year to ease.

    As a result, chemicals left underground are still being pushed away from the drill site long after drilling is finished. It can take five or six years before the natural balance of pressure in the underground system is fully restored, the study found.

    Myers’ research focused exclusively on the Marcellus, but he said his findings may have broader relevance. Many regions where oil and gas is being drilled have more permeable underground environments than the one he analyzed, he said.

    “One would have to say that the possible travel times for a similar thing in Arkansas or Northeast Texas is probably faster than what I’ve come up with,” Myers said.

    Ground Water is the journal of the National Ground Water Association, a non-profit group that represents scientists, engineers and businesses in the groundwater industry.

    Several scientists called Myers’ approach unsophisticated and said that the assumptions he used for his models didn’t reflect what they knew about the geology of the Marcellus Shale. If fluids could flow as quickly as Myers asserts, said Terry Engelder, a professor of geosciences at Penn State University who has been a proponent of shale development, fracking wouldn’t be necessary to open up the gas deposits.

    “This would be a huge fracture porosity,” Engelder said. “So I read this and I say, ‘Golly, does this guy really understand anything about what these shales look like?’ The concern then arises from using a model rather than observations.”

    Myers likened the shale to a cracked window, saying that samples showing it didn’t contain fractures were small in size and were akin to only examining an intact section of glass, while a broader, scaled out view would capture the faults and fractures that could leak.

    Both scientists agreed that direct evidence of fluid migration is needed, but little sampling has been done to analyze where fracking fluids go after being injected underground.

    Myers says monitoring systems could be installed around gas well sites to measure for changes in water quality, a measure required for some gold mines, for example. Until that happens, Myers said, theoretical modeling has to substitute for hard data.

    “We were trying to use the basic concepts of groundwater and hydrology and geology and say can this happen?” he said. “And that had basically never been done.”

    — Abrahm Lustgarten
    Editors note: View stories in the ProPublica series at www.propublica.org/series/fracking.

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    History of the Tribal PWSS and UIC Programs

    In 1974 the United States Congress passed legislation, the Safe Drinking Water Act (SDWA), designed to maintain and improve the quality of the nation’s drinking waters. Two major regulatory programs were created in the SDWA: the Public Water System Supervision (PWSS) and the Underground Injection Control (UIC) programs.

    Congress authorized EPA to delegate responsibilities to states for implementing and enforcing national standards within their jurisdiction. States must apply to EPA if they want this “primacy” responsibility and must develop PWSS or UIC programs that meet national requirements. EPA is still responsible for developing national regulations, overseeing state primacy programs and implementing programs in states without primacy.

    Because of their unique status, Indian tribes were not eligible to assume primacy in the original Act. Instead EPA regions were responsible for primary enforcement authority of PWSS and UIC programs on Tribal lands. This changed in 1986 when the Amendments to the SDWA added provisions that allow federally recognized tribes to assume primacy for the PWSS and UIC programs. Section 1451 (“Indian Tribes”) of SDWA authorizes the EPA to treat Indian tribes in a manner similar to states and to assign primary enforcement responsibility (primacy) to qualified tribes.

    The PWSS and UIC programs are very complex and costly to operate. For many tribes (especially those that do not have a large number of public water systems or underground injection wells), the costs and resources required to achieve and maintain a regulatory program may far exceed the benefits from achieving primacy. Due to such difficulties, currently the only tribe that has sought and obtained primacy for the PWSS program is the Navajo Nation. There are a few tribes that are pursuing primacy in the PWSS and UIC programs.

    Today´s Tribal Direct Implementation Program

    States and tribes that do not obtain PWSS and UIC program delegation continue to be directly implemented by the EPA region in which the State or reservation is located. All EPA regions, excluding Region III (which has no federally recognized tribes), operate tribal PWSS and UIC programs to manage public water systems or underground injection wells on Indian lands.

    EPA’s 1997 inventory shows that there are nearly 1000 public water systems (740 community water systems, 90 nontransient noncommunity water systems and 130 transient noncommunity water systems) that the EPA regional offices manage on Indian lands serving a population of nearly 500,000. There are also over 5,300 injection wells (one Class I well, 4,300 Class II wells, 0 Class III wells and 1,042 Class V wells) on tribal lands that are managed by regional UIC staff.

    As the primary enforcement authority for tribal public water systems, EPA regions are responsible for enforcing against those systems that do not comply with federal drinking water regulations. A formal enforcement action is taken as a last measure. EPA regions dedicate a great deal of resources to provide tribes with technical assistance to help their systems or wells comply with federal standards. Regional staff visit reservations as often as possible to provide compliance assistance on site. Many Regions also fund circuit rider programs which enable other qualified persons the opportunity to provide technical assistance and training directly to tribes.

    For more information on the Tribal PWSS and UIC programs, please contact your program representative.

    Source water assessment and protection programs

    Source Water Assessment and Protection Programs

    The Safe Drinking Water Act (SDWA) Amendments of 1996 required states to develop and implement source water assessment programs (SWAPs) to analyze existing and potential threats to the quality of the public drinking water throughout the state. Using these programs, most states have completed source water assessments for every public water system — from major metropolitan areas to the smallest towns. Even schools, restaurants, and other public facilities that have wells or surface water supplies have been assessed. A source water assessment is a study and report, unique to a water system, that provides basic information about the water used to provide drinking water. States are working with local communities and public water systems to identify protection measures to address potential threats to sources of drinking water.

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    Wellhead Protection Program

    The Wellhead Protection Program (WHPP) is a pollution prevention and management program used to protect underground sources of drinking water. The national WHPP was established under section 1428 of the 1986 SDWA amendments. The law specified that certain program activities, such as delineation, contaminant source inventory, contingency planning and source management, be incorporated into state WHPPs, which are approved by EPA prior to implementation. All states have EPA-approved state WHPPs. Although section 1428 applies only to states, a number of tribes are implementing the program as well.

    WHPPs provided the foundation for many of the state source water assessment programs required under the 1996 SDWA amendments. Most states also use the wellhead protection program as a foundation for assessing and protecting ground water systems. State WHPPs vary greatly. For example, some states require community water systems to develop management plans, while others rely on education and technical assistance to encourage voluntary action. Other states have mandatory requirements for wellhead protection at the local level. Guidance, publications and other resources are available on state source water web sites.

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    Many states have also developed programs that are focused specifically on ground water protection. Several states developed formal Comprehensive State Ground Water Protection Programs (CSGWPP), which were designed as a management tool for states to use to integrate all programs that affect ground water quality, thus allowing better decisions to be made. Although most states are no longer pursuing formal approval of a CSGW pp, virtually all states are pursuing at least some of the individual elements necessary for comprehensive ground water protection. Within EPA, the source water protection program is working with the underground storage tank program to address potential threats to ground water posed by leaking tanks.

    Publications and resources

    Sole source aquifer protection program

    Sole Source Aquifer Protection Program

    A sole source aquifer supplies 50 percent or more of the drinking water for a given aquifer service area for which there are no reasonably available alternative sources, should the aquifer become contaminated. Designation as a sole source aquifer protects an area’s ground water resources by requiring EPA to review any proposed projects within the designated area that are receiving federal financial assistance.

    Watershed-based protection program

    Watershed-Based Protection Program

    The goal of source water protection is to protect the drinking water resource by protecting and preserving the environmental quality of the watershed above the intake (or the aquifer around the well). The assessment is the first step in the process to protect the resource. Once a watershed has been assessed to determine its current condition and the extent of the threats to the system, a watershed plan can be developed and implemented.

    EPA’s Office of Water has numerous programs that focus on watershed protection under the Clean Water Act (CWA). The Act includes programs such as the Nonpoint Source Program, National Estuary Program, the Total Maximum Daily Load (TMDL) Program, and the National Pollution Discharge Elimination System (NPDES) program. Each of these programs encourage states to develop programs to promote watershed-based protection, and they have elements that support watershed-based planning and implementation. The federal programs are generally implemented at the state level.

    EPA,Federal /non-governmental programs

    EPA, Federal / Non-governmental Programs

    There is no single federal program for implementing source water protection plans and activities. However, many federal, tribal, regional, and local programs have tools and resources that can be used to focus on protecting drinking water. Source water protection can benefit, and benefit from, other EPA programs, other federal programs and non-governmental programs:

    • Other programs can use source water assessments and identified protection areas to set priorities for ongoing prevention efforts.
    • Identifying source water protection areas increases federal, state and local managers’ awareness of other programs where participation might increase the protection of human health.
    • Protecting sources of drinking water can help various federal programs, states, organizations and communities meet other environmental and social goals, such as green space conservation, stormwater planning, management of nonpoint source pollution and brownfields redevelopment.
    • The benefits that EPA and other federal programs can provide to state and local source water assessment and protection efforts are potentially very large. These include information, technical and financial resources, and communication networks and enforcement authorities.

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    Fracking water contamination : Natural gas fracking fizzles in Michigan – EPA Fracking Directory – [Detroit News - Jim Lynch]

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    Fracking water contamination:  Natural gas fracking fizzles in Michigan - EPA Fracking Directory - [Detroit News - Jim Lynch]

    Natural gas fracking fizzles in Michigan

    Pollution concerns, falling prices slow drilling

    May 25, 2012 at 12:37 pm / By Jim Lynch / The Detroit News
    Fracking, the practice of pumping chemical-laced water underground to fracture the rock, has been practiced in Michigan for decades. (Photo by Heather Rousseau)

    Just two years ago Michigan was well on its way to becoming Pennsylvania West — following in that state’s footsteps as the next hotbed of natural gas exploration and production.

    Since that time, the plummeting price of natural gas and concerns over the technology used to extract it — hydraulic fracturing — have brought the expected boom to a standstill.

    “There is so much gas that we already (know) can be produced cheaply that exploring new areas and trying to commercialize them has ground to a halt everywhere,” industry analyst Amber McCullagh said.

    Despite that lull in production, the debate over natural gas has never been more intense — a high-stakes battle that could dictate the future terms of gas production when prices rebound.

    That fight is playing out in Michigan’s Legislature as well as the courts. Lawmakers have a spate of bills to consider that put restrictions on hydraulic fracturing, or “fracking.” One citizens’ group based in Charlevoix is trying to give voters the option of banning the practice outright. A new lawsuit filed in Ingham County seeks to force Michigan’s Department of Environmental Quality to apply regulations on the books for injection wells to hydraulic fracturing.

    And the debate over how best to deal with fracking has caused a divide in the environmental community as well. Efforts to enact a ban on the process are considered unrealistic by some, while anything short of a ban is considered a sellout by others.

    Fracking has been practiced in Michigan for decades. By pumping chemical-laced water underground to fracture the rock, energy companies can pump out the natural gas no longer trapped. More recent twists on the technology — such as drilling horizontally after reaching the shale depth and using millions of gallons of water — have increased productivity and opened up new areas in Michigan to development.

    “Michigan has a strong stake in continued responsible development and greater use of this homegrown energy source,” said Robert Sumner, director of communications for America’s Natural Gas Alliance, in a written response to questions. “For both power generation and transportation, natural gas is a far cleaner alternative than the dominant forms of energy we use today.That means cleaner air in Michigan communities.”

    Environmental issues in Pennsylvania

    But the expanded use of horizontal fracking also has heightened the level of concern over natural gas production. Environmental issues in Pennsylvania and earthquake concerns from as close by as Ohio have painted a target on the extraction process.

    And the battle has already claimed one — sort of. Steven Losher, a 47-year-old Barry County resident, traveled to Lansing on May 8 to watch as the Michigan Department of Natural Resources auctioned off oil and mineral rights to state lands — some of which were near his home.

    Losher, who was there because of concerns over fracking in his southwest county, wound up being arrested when he was thought to be part of the Occupy movement that was demonstrating outside.

    “When you look at what’s happened in other states … it seems after even cursory research that everywhere horizontal fracking has been occurring, there have been problems,” said Losher, who will be arraigned June 5. “And some of those problems have been hellish.”

    A single test well, brought online by Calgary, Alberta-based Encana Corp. in early 2010, was the first domino here, putting the fracking debate in the spotlight. The initial production from that well in Missaukee County — in the natural gas deposit called the Collingwood Shale — brought energy companies to the state, scrambling to secure oil and mineral rights on as much land as possible. The county is east of Cadillac.

    But a second test well produced less robust results and the dropping market price for natural gas brought exploratory efforts to a standstill.

    “Essentially, producers were victims of their own success,” said McCullagh, a senior analyst of North American gas research at Houston-based Wood Mackenzie.

    “Costs for producing natural gas declined significantly and overall production increased rapidly. … As a result, the price for natural gas declined from $12 to $13 per million British thermal unit in 2005 to an average of $4 in 2011.”

    Last month, U.S. natural gas prices traded at less than $2 per million British thermal units for the first time since 2002.

    The Collingwood Shale roughly spans the northern portion of the Lower Peninsula and reaches in to the easternmost portions of the Upper Peninsula. The gas deposits sit as deep as 10,000 feet below the surface.

    Encana’s first well was the initial hydraulic fracturing project to be used in the shale. So far, three wells in Michigan have utilized the horizontal drilling technique.

    Seventeen years ago, Joanne Cromley and her husband relocated from the Chicago area to Michigan with a specific goal in mind. They purchased 240 acres of land near Afton, in Cheboygan County, with the intention of letting it “go wild.”

    In August 2010, a letter arrived alerting the couple that the state had included their property’s oil and mineral rights in an auction. While the couple owned the land, the state had the right to offer up its drilling rights, creating the possibility a company could come in and mine on their land in pursuit of natural gas.

    Today, Cromley serves as the co-chairman of Don’t Frack Michigan — a citizens’ group attempting to ban fracking in the state. The task at-hand, he said, is education and pushing for a no-compromise solution. “I think that a lot of people have been put to sleep in the sense that there are some environmental organizations that say we can do this through regulation,” she said. “I don’t think we can.”

    For groups like Don’t Frack Michigan, or the similarly titled Ban Michigan Fracking, the bills currently in the Legislature are eyed with suspicion, if not derision.

    LuAnne Kozma is among the Ban Michigan Fracking members collecting petition signatures to place the fracking question before voters. They have until July 9 to collect 322,000 of them in order to have a ban option on the November ballot.

    Her grassroots group puts quotes around the word “reform” when discussing the package of proposed laws targeting natural gas extraction. They leave the door to energy companies open for fracking in the future and that, she said, is a risk she isn’t willing to take.

    Other groups, including the Michigan Environmental Council, see a future that includes fracking in a tightly regulated environment.

    “We all use natural gas,” he said. “This is a product that is part of our everyday lives. To the extent that if falls into that category, we should figure out the best way to deal with it.”

    jlynch@detnews.com

    (313) 222-2034

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    Water contamination news: Fracking – The other side of the fracking issue – Whats fracking all about? Fracking defined – Part 2.

    Fracking Questions and Answers


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    Water contamination – Fracking

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    Site Setup

    Consistent with the Energy Policy Act of 2005, the U.S. Environmental Protection Agency (EPA) published a final rule in 2006 that exempts stormwater discharges of sediment from construction activities at oil and gas exploration and production operations from the requirement to obtain a National Pollutant Discharge Elimination System (NPDES) ‡ stormwater permit as long as stormwater runoff to waters under the jurisdiction of the CWA are not contaminated with oil, grease, or hazardous substances. With this exemption, EPA specifically encouraged the oil and natural gas industry to develop and implement Best Management Practices (BMPs) to minimize the discharges of pollutants, including sediment, in stormwater both during and after construction activities. In an effort to meet the expectations of EPA under this rulemaking — to incorporate successful voluntary stormwater management practices into day-to-day operations – the American Petroleum Institute (API) and the Independent Petroleum Association of America (IPAA), industry associations, and company representatives (referred to as the Stormwater Technical Workgroup (SWTW)), built upon the 2004 guidance document entitled Reasonable and Prudent Practices for Stabilization (RAPPS) of Oil and Natural Gas Construction Sites. Through field validation of the RAPPS, gap identification, and concerted program improvements, the SWTW developed a voluntary guidance document that, if implemented correctly, will serve as a readily applicable tool for operators to use in order to efficiently and effectively maximize control of stormwater discharges at oil and natural gas exploration and production activities throughout the contiguous U.S.Fracking

    fracking

     
     
     
     
     
     
     
     

    Historical perspective

    Hydraulic fracturing is not new. The first commercial application of hydraulic fracturing as a well treatment technology designed to stimulate the production of oil or gas likely occurred in either the Hugoton field of Kansas in 1946 or near Duncan Oklahoma in 1949. In the ensuing sixty plus years, the use of hydraulic fracturing has developed into a routine technology that is frequently used in the completion of gas wells, particularly those involved in what’s called “unconventional production,” such as production from so-called “tight shale” reservoirs. The process has been used on over 1 million producing wells. As the technology continues to develop and improve, operators now fracture as many as 35,000 wells of all types (vertical and horizontal, oil and natural gas) each year.

    Hydraulic fracturing has had an enormous impact on America’s energy history, particularly in recent times.
    The ability to produce more oil and natural gas from older wells and to develop new production once thought impossible has made the process valuable for US domestic energy production.
    Without hydraulic fracturing, as much as 80 percent of unconventional production from such formations as gas shales would be, on a practical basis, impossible.

    This technique uses a specially blended liquid which is pumped into a well under extreme pressure causing cracks in rock formations underground. These cracks in the rock then allow oil and natural gas to flow, increasing resource production.

    Hydraulic Fracturing: The Process

    What Is Hydraulic Fracturing?

    Contrary to many media reports, hydraulic fracturing is not a “drilling process.” Hydraulic fracturing is used after the drilled hole is completed. Put simply, hydraulic fracturing is the use of fluid and material to create or restore small fractures in a formation in order to stimulate production from new and existing oil and gas wells. This creates paths that increase the rate at which fluids can be produced from the reservoir formations, in some cases by many hundreds of percent.

    Process includes steps to…

    The process includes steps to protect water supplies. To ensure that neither the fluid that will eventually be pumped through the well, nor the oil or gas that will eventually be collected, enters the water supply, steel surface or intermediate casings are inserted into the well to depths of between 1,000 and 4,000 feet. The space between these casing “strings” and the drilled hole (wellbore), called the annulus, is filled with cement. Once the cement has set, then the drilling continues from the bottom of the surface or intermediate cemented steel casing to the next depth. This process is repeated, using smaller steel casing each time, until the oil and gas-bearing reservoir is reached (generally 6,000 to 10,000 ft). A more detailed look at casing and its role in groundwater protection is available HERE.

    With these and other precautions taken, high volumes of fracturing fluids are pumped deep into the well at pressures sufficient to create or restore the small fractures in the reservoir rock needed to make production possible.

    What’s in Hydraulic Fracturing Fluid?

    Water and sand make up 98 to 99.5 percent of the fluid used in hydraulic fracturing. In addition, chemical additives are used. The exact formulation varies depending on the well. To view a chart of the chemicals most commonly used in hydraulic fracturing and for a more detailed discussion of this question, click HERE.

    Why is Hydraulic Fracturing Used?

    Experts believe 60 to 80 percent of all wells drilled in the United States in the next ten years will require hydraulic fracturing to remain operating. Fracturing allows for extended production in older oil and natural gas fields. It also allows for the recovery of oil and natural gas from formations that geologists once believed were impossible to produce, such as tight shale formations in the areas shown on the map below. Hydraulic fracturing is also used to extend the life of older wells in mature oil and gas fields.

    How is Hydraulic Fracturing Done?*

    The placement of hydraulic fracturing treatments underground is sequenced to meet the particular needs of the formation. The sequence noted below from a Marcellus Shale in Pennsylvania is just one example. Each oil and gas zone is different and requires a hydraulic fracturing design tailored to the particular conditions of the formation. Therefore, while the process remains essentially the same, the sequence may change depending upon unique local conditions. It is important to note that not all of the additives are used in every hydraulically fractured well; the exact “blend” and proportions of additives will vary based on the site-specific depth, thickness and other characteristics of the target formation.

    1. An acid stage, consisting of several thousand gallons of water mixed with a dilute acid such as hydrochloric or muriatic acid: This serves to clear cement debris in the wellbore and provide an open conduit for other frac fluids by dissolving carbonate minerals and opening fractures near the wellbore.

    2. A pad stage, consisting of approximately 100,000 gallons of slickwater without proppant material: The slickwater pad stage fills the wellbore with the slickwater solution (described below), opens the formation and helps to facilitate the flow and placement of proppant material.

    3. A prop sequence stage, which may consist of several substages of water combined with proppant material (consisting of a fine mesh sand or ceramic material, intended to keep open, or “prop” the fractures created and/or enhanced during the fracturing operation after the pressure is reduced): This stage may collectively use several hundred thousand gallons of water. Proppant material may vary from a finer particle size to a coarser particle size throughout this sequence.

    4. A flushing stage, consisting of a volume of fresh water sufficient to flush the excess proppant from the wellbore.

    Other additives commonly used in the fracturing solution employed in Marcellus wells include:

    • A dilute acid solution, as described in the first stage, used during the initial fracturing sequence. This cleans out cement and debris around the perforations to facilitate the subsequent slickwater solutions employed in fracturing the formation.

    • A biocide or disinfectant, used to prevent the growth of bacteria in the well that may interfere with the fracturingoperation: Biocides typically consist of bromine-based solutions or glutaraldehyde.

    • A scale inhibitor, such as ethylene glycol, used to control the precipitation of certain carbonate and sulfate minerals

    • Iron control/stabilizing agents such as citric acid or hydrochloric acid, used to inhibit precipitation of iron compounds by keeping them in a soluble form

    • Friction reducing agents, also described above, such as potassium chloride or polyacrylamide-based compounds, used to reduce tubular friction and subsequently reduce the pressure needed to pump fluid into the wellbore: The additives may reduce tubular friction by 50 to 60%. These friction-reducing compounds represent the “slickwater” component of the fracing solution.

    • Corrosion inhibitors, such as N,n-dimethyl formamide, and oxygen scavengers, such as ammonium bisulfite, are used to prevent degradation of the steel well casing.

    • Gelling agents, such as guar gum, may be used in small amounts to thicken the water-based solution to help transport the proppant material.

    • Occasionally, a cross-linking agent will be used to enhance the characteristics and ability of the gelling agent to transport the proppant material. These compounds may contain boric acid or ethylene glycol. When cross-linking additives are added, a breaker solution is commonly added later in the frac stage to cause the enhanced gelling agent to break down into a simpler fluid so it can be readily removed from the wellbore without carrying back the sand/ proppant material.

    Fractures: Their orientation and length

    Certain predictable characteristics or physical properties regarding the path of least resistance have been recognized since hydraulic fracturing was first conducted in the oilfield in 1947. These properties are discussed below:

    Fracture orientation

    Hydraulic fractures are formed in the direction perpendicular to the least stress. Based on experience, horizontal fractures will occur at depths less than approximately 2000 ft. because the Earth’s overburden at these depths provides the least principal stress. If pressure is applied to the center of a formation under these relatively shallow conditions, the fracture is most likely to occur in the horizontal plane, because it will be easier to part the rock in this direction than in any other. In general, therefore, these fractures are parallel to the bedding plane of the formation.

    As depth increases beyond approximately 2000 ft., overburden stress increases by approximately 1 psi/ft., making the overburden stress the dominant stress This means the horizontal confining stress is now the least principal stress. Since hydraulically induced fractures are formed in the direction perpendicular to the least stress, the resulting fracture at depths greater than approximately 2000 ft. will be oriented in the vertical direction.

    In the case where a fracture might cross over a boundary where the principal stress direction changes, the fracture would attempt to reorient itself perpendicular to the direction of least stress. Therefore, if a fracture propagated from deeper to shallower formations it would reorient itself from a vertical to a horizontal pathway and spread sideways along the bedding planes of the rock strata.

    Fracture length/ height

    The extent that a created fracture will propagate is controlled by the upper confining zone or formation, and the volume, rate, and pressure of the fluid that is pumped. The confining zone will limit the vertical growth of a fracture because it either possesses sufficient strength or elasticity to contain the pressure of the injected fluids or an insufficient volume of fluid has been pumped.. This is important because the greater the distance between the fractured formation and the USDW, the more likely it will be that multiple formations possessing the qualities necessary to impede the fracture will occur. However, while it should be noted that the length of a fracture can also be influenced by natural fractures or faults as shown in a study that included microseismic analysis ‡ of fracture jobs conducted on three wells in Texas, natural attenuation of the fracture will occur over relatively short distances due to the limited volume of fluid being pumped and dispersion of the pumping pressure regardless of intersecting migratory pathways.

    The following text and graphs are excerpts from an article written by Kevin Fisher of Pinnacle, a Halliburton Company for the July 2010 edition of the American Oil and Gas Reporter.

    “The concerns around groundwater contamination raised by Congress are primarily centered on one fundamental question: Are the created fractures contained within the target formation so that they do not contact underground sources of drinking water? In response to that key concern, this article presents the first look at actual field data based on direct measurements acquired while fracture mapping more than 15,000 frac jobs during the past decade.

    Extensive mapping of hydraulic fracture geometry has been performed in unconventional North American shale reservoirs since 2001. The microseismic and tiltmeter technologies used to monitor the treatments are well established, and are also widely used for nonoil field (sic) applications such as earthquake monitoring, volcano monitoring, civil engineering applications, carbon capture and waste disposal. Figures 1 and 2 are plots of data collected on thousands of hydraulic fracturing treatments in the Barnett Shale in the Fort Worth Basin in Texas and in the Marcellus Shale in the Appalachian Basin.

    < img class="alignleft"src="http://fracfocus.org/sites/default/files/fracture-height-graph-barnett.gif" alt="fracking" width="495" height="249" />

    Figure 1. Barnett Shale

    More fracs have been mapped in the Barnett than any other reservoir. The graph illustrates the fracture top and bottom for all mapped treatments performed in the Barnett since 2001. The depths are in true vertical depth. Perforation depths are illustrated by the red-colored band for each stage, with the mapped fracture tops and bottoms illustrated by colored curves corresponding to the counties where they took place.

    The deepest water wells in each of the counties where Barnett Shale fracs have been mapped, according to United States Geological Survey (http://nwis.waterdata.usgs.gov/nwis ‡), are illustrated by the dark blue shaded bars at the top of Figure 1. As can be seen, the largest directly measured upward growth of all of these mapped fractures still places the fracture tops several thousands of feet below the deepest known aquifer level in each county.

    fracking

    Figure 2 Marcellus Shale

    The Marcellus data show a similarly large distance between the top of the tallest frac and the location of the deepest drinking water aquifers as reported in USGS data (dark blue shaded bars at the top of Figure 2). Because it is a newer play with fewer mapped frac stages at this point and encompasses several states, the data set is not as comprehensive as that from the Barnett. However, it is no less compelling in providing evidence of a very good physical separation between hydraulic fracture tops and water aquifers.

    Almost 400 separate frac stages are shown, color coded by state. As can be seen, the fractures do grow upward quite a bit taller than in the Barnett, but the shallowest fracture tops are still ±4,500 feet, almost one mile below the surface and thousands of feet below the aquifers in those counties.

    The results from our extensive fracture mapping database show that hydraulic fractures are better confined vertically (and are also longer and narrower) than conventional wisdom or models predict. Even in areas with the largest measured vertical fracture growth, such as the Marcellus, the tops of the hydraulic fractures are still thousands of feet below the deepest aquifers suitable for drinking water. The data from these two shale reservoirs clearly show the huge distances separating the fracs from the nearest aquifers at their closest points of approach, conclusively demonstrating that hydraulic fractures are not growing into groundwater supplies, and therefore, cannot contaminate them.”

    * Pennsylvania Department of Environmental Protection
    “Hydraulic Fracturing Overview.” 07/20/2010.
    http://www.dep.state.pa.us/dep/deputate/minres/oilgas/new_forms/marcellus/Reports/DEP%20Fracing%20overview.pdf ‡ (4/11/2011).

    Fracturing Fluid Management

    Fluid Storage – “Pits”

    From the time the first oil and gas wells were drilled, “pits” have been used to hold drilling fluids and wastes. Pits can be excavated holes in the ground, or they can be above ground containment systems such as steel tanks. Pits are used for storage of produced water, for emergency overflow, temporary storage of oil, burn off of waste oil, and for temporary storage of the fluids used to complete and treat the well.

    The containment of fluids within a pit is the most critical element in the prevention of contamination of shallow ground water. The failure of a tank, pit liner, or the line carrying fluid (“flowline”) can result in a release of contaminated materials directly into surface water and shallow ground water. Environmental clean-up of these accidentally released materials can be a costly and time consuming process. Therefore, prevention of releases is vitally important.

    For pits constructed from ground excavation, pit lining may be necessary to prevent infiltration of fluids into the subsurface of the ground, depending upon the fluids being placed in the pit, the duration of the storage and the soil conditions. Typically, pit liners are constructed of compacted clay or synthetic materials like polyethylene or treated fabric that can be joined using special equipment.
    Read more at FracFocus

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    Water contamination news: Fracking – Using diesel fuel in oil and gas hydraulic fracturing.

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    Water contamination news – Fracking

    Using diesel fuel in oil and gas hydraulic fracturing.

    Kansas City infoZine / Saturday, May 05, 2012 ::

    EPA Releases Draft clarifying means of compliance to 2005 Amendments of Safe Drinking Water Act

    Washington, D.C. – infoZine – The U.S. Environmental Protection Agency (EPA) has released draft underground injection control (UIC) program permitting guidance for class II wells that use diesel fuels during hydraulic fracturing activities. EPA developed the draft guidance to clarify how companies can comply with a law passed by Congress in 2005, which exempted hydraulic fracturing operations from the requirement to obtain a UIC permit, except in cases where diesel fuel is used as a fracturing fluid.

    The draft guidance outlines for EPA permit writers, where EPA is the permitting authority, requirements for diesel fuels used for hydraulic fracturing wells, technical recommendations for permitting those wells, and a description of diesel fuels for EPA underground injection control permitting. The draft guidance describes diesel fuels for these purposes by reference to six chemical abstract services registry numbers. The agency is requesting input on this description.

    While this guidance undergoes public notice and comment, decisions about permitting hydraulic fracturing operations that use diesel fuels will be made on a case-by-case basis, considering the facts and circumstances of the specific injection activity and applicable statutes, regulations and case law, and will not cite this draft guidance as a basis for decision.

    EPA will take public comment on the draft guidance for 60 days upon publication in the Federal Register to allow for stakeholder input before it is finalized.

    More information: The EPA Offers the following information

    Hydraulic Fracturing Under the Safe Drinking Water Act


    Natural gas plays a key role in our nation’s clean energy future and the process known as hydraulic fracturing is one way of accessing that vital resource. Hydraulic fracturing is used by gas producers to stimulate wells and recover natural gas from sources such as coalbeds and shale gas formations. Hydraulic fracturing is also used for other applications including oil recovery. Over the past few years, several key technical, economic, and energy policy developments have spurred increased use of hydraulic fracturing for gas extraction over a wider diversity of geographic regions and geologic formations. Along with the expansion of hydraulic fracturing, there have been increasing concerns about its potential impacts on drinking water resources, public health, and environmental impacts in the vicinity of these facilities.

    Draft Guidance: Permitting Guidance for Oil and Gas Hydraulic Fracturing Activities Using Diesel Fuels

    EPA has developed draft Underground Injection Control (UIC) Class II permitting guidance for oil and gas hydraulic fracturing activities using diesel fuels. This document describes information useful in permitting the underground injection of oil- and gas-related hydraulic fracturing using diesel fuels where EPA is the permitting authority. EPA’s goal is to improve compliance with the Safe Drinking Water Act (SDWA) requirements and strengthen environmental protections consistent with existing law.

      For help with accessibility, please contact Sherri Comerford

    comerford.sherri@epa.gov

      , (202) 564-4369
  • Fact Sheet (PDF) (2 pp, 2MB, About PDF), EPA 816-K-12-001
  • Opportunities to participate in public meetings and/or webinars will be published in the Federal Register and on the Outreach section of this website.
  • The Agency invites comment, particularly on the following topics presented in the Federal Register Noice.

    • The draft guidance is open for comment for 60 days after publication in the Federal Register. To comment, use one of the following methods, and specify Docket ID No. EPA-HQ-OW-2011-1013:
    • Online: Go to www.regulations.gov, and follow the on-line instructions for submitting comments.
    • Email: OW-Docket@epa.gov@epa.gov.
    • Mail: Permitting Guidance for Oil and Gas Hydraulic Fracturing Activities Using Diesel Fuels – Draft, Environmental Protection Agency, Mailcode: 4606M, 1200 Pennsylvania Ave., NW, Washington, DC 20460.
    • Hand Delivery: Office of Water (OW) Docket, EPA/DC, EPA West, Room 3334, 1301 Constitution Ave., NW, Washington, DC. Such deliveries are only accepted during the Docket’s normal hours of operation, and special arrangements should be made for deliveries of boxed information.

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    Water contamination news: Fracking – Study has raised concerns about the safety of gas drilling in the Marcellus Shale.

    Water contamination news: fracking - Study has raised concerns about the safety of gas drilling in the Marcellus Shale

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    Water contamination news: fracking - Study has raised concerns about the safety of gas drilling in the Marcellus Shale

     

    Despite many successful water projects, billions of people still lack adequate water and sanitation

     
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    Water contamination news

    New study predicts fracking fluids will seep into aquifers within years.

    This story was originally published by ProPublica.

    As part of its continuing advocacy to protect NYC’s water supply from contamination, the WCC submitted comments to  Hon. Joe Martens, Commissioner of the New York State Department of Environmental Conservation on the issue of hydrofracking in New York State

    A new study has raised fresh concerns about the safety of gas drilling in the Marcellus Shale, concluding that fracking chemicals injected into the ground could migrate toward drinking water supplies far more quickly than experts have previously predicted.

    More than 5,000 wells were drilled in the Marcellus between mid-2009 and mid-2010, according to the study, which was published in the journal Ground Water two weeks ago. Operators inject up to 4 million gallons of fluid, under more than 10,000 pounds of pressure, to drill and frack each well.

    Scientists have theorized that impermeable layers of rock would keep the fluid, which contains benzene and other dangerous chemicals, safely locked nearly a mile below water supplies. This view of the earth’s underground geology is a cornerstone of the industry’s argument that fracking poses minimal threats to the environment.

    But the study, using computer modeling, concluded that natural faults and fractures in the Marcellus, exacerbated by the effects of fracking itself, could allow chemicals to reach the surface in as little as “just a few years.”

    “Simply put, [the rock layers] are not impermeable,” said the study’s author, Tom Myers, an independent hydrogeologist whose clients include the federal government and environmental groups.

    “The Marcellus shale is being fracked into a very high permeability,” he said. “Fluids could move from most any injection process.”

    The research for the study was paid for by Catskill Mountainkeeper and the Park Foundation, two upstate New York organizations that have opposed gas drilling and fracking in the Marcellus.

    Much of the debate about the environmental risks of gas drilling has centered on the risk that spills could pollute surface water or that structural failures would cause wells to leak.

    Though some scientists believed it was possible for fracking to contaminate underground water supplies, those risks have been considered secondary. The study in Ground Water is the first peer-reviewed research evaluating this possibility.

    The study did not use sampling or case histories to assess contamination risks. Rather, it used software and computer modeling to predict how fracking fluids would move over time. The simulations sought to account for the natural fractures and faults in the underground rock formations and the effects of fracking.

    The models predict that fracking will dramatically speed up the movement of chemicals injected into the ground. Fluids traveled distances within 100 years that would take tens of thousands of years under natural conditions. And when the models factored in the Marcellus’ natural faults and fractures, fluids could move 10 times as fast as that.

    Where man-made fractures intersect with natural faults, or break out of the Marcellus layer into the stone layer above it, the study found, “contaminants could reach the surface areas in tens of years, or less.”

    The study also concluded that the force that fracking exerts does not immediately let up when the process ends. It can take nearly a year to ease.

    As a result, chemicals left underground are still being pushed away from the drill site long after drilling is finished. It can take five or six years before the natural balance of pressure in the underground system is fully restored, the study found.

    Myers’ research focused exclusively on the Marcellus, but he said his findings may have broader relevance. Many regions where oil and gas is being drilled have more permeable underground environments than the one he analyzed, he said.

    “One would have to say that the possible travel times for a similar thing in Arkansas or Northeast Texas is probably faster than what I’ve come up with,” Myers said.

    Ground Water is the journal of the National Ground Water Association, a non-profit group that represents scientists, engineers and businesses in the groundwater industry.

    Several scientists called Myers’ approach unsophisticated and said that the assumptions he used for his models didn’t reflect what they knew about the geology of the Marcellus Shale. If fluids could flow as quickly as Myers asserts, said Terry Engelder, a professor of geosciences at Penn State University who has been a proponent of shale development, fracking wouldn’t be necessary to open up the gas deposits.

    “This would be a huge fracture porosity,” Engelder said. “So I read this and I say, ‘Golly, does this guy really understand anything about what these shales look like?’ The concern then arises from using a model rather than observations.”

    Myers likened the shale to a cracked window, saying that samples showing it didn’t contain fractures were small in size and were akin to only examining an intact section of glass, while a broader, scaled out view would capture the faults and fractures that could leak.

    Both scientists agreed that direct evidence of fluid migration is needed, but little sampling has been done to analyze where fracking fluids go after being injected underground.

    Myers says monitoring systems could be installed around gas well sites to measure for changes in water quality, a measure required for some gold mines, for example. Until that happens, Myers said, theoretical modeling has to substitute for hard data.

    “We were trying to use the basic concepts of groundwater and hydrology and geology and say can this happen?” he said. “And that had basically never been done.”

    This story was originally published by ProPublica.http://www.propublica.org/article/new-study-predicts-frack-fluids-can-migrate-to-aquifers-within-years/single#republish#ixzz1uDGSWKIA” target=”_blank”>Read more:

    Proppants and fracking fluids

    Last updated June 5th 2012 From Wikipedia, the free encyclopedia

    A proppant is a material that will keep a induced hydraulic fracture open, during or following a fracturing treatment, while the fracking fluid itself varies in composition depending on the type of fracturing used, and can be gel, foam or slickwater-based.

    Proppants and fracking fluids: click

    Proppants and fracking fluids

    Last updated June 5th 2012 From Wikipedia, the free encyclopedia

    A proppant is a material that will keep a induced hydraulic fracture open, during or following a fracturing treatment, while the fracking fluid itself varies in composition depending on the type of fracturing used, and can be gel, foam or slickwater-based. In addition, there may be unconventional fracking fluids. 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. In addition, fluids may be used in low-volume well stimulation of high-permeability sandstone wells (20k to 80k gallons per well) to the high-volume operations such as shale gas and tight gas that use millions of gallons of water per well.

    Conventional wisdom has often vascillated about the relative superiority of gel, foam and slickwater fluids with respect to each other, which is in turn related to proppant choice. For example, Zuber, Kuskraa and Sawyer (1988) found that gel-based fluids seemed to achieve the best results for coalbed methane operations, [1], but as of 2012, slickwater treatments are more popular.

    Ignoring proppant, slickwater fracturing fluids are mostly water, generally 99% or more by volume, but gel-based fluids can see polymers and surfactants comprising as much as 7 vol% of a gel-based fluid, ignoring other additives. [2] Other common additives include hydrochloric acid (low pH can etch certain rocks, dissolving limestone for instance), friction reducers, biocides, and emulsifiers.

    Radioactive tracer isotopes are sometimes included in the hydrofracturing fluid to determine the injection profile and location of fractures created by hydraulic fracturing.[3] Patents describe in detail how several tracers are typically used in the same well. Wells are hydraulically fractured in different stages.[4] Tracers with different half-lives are used for each stage.[4][5] Their half-lives range from 40.2 hours (Lanthanum-140) to 5.27 years (Cobalt-60).[6] Amounts per injection of radionuclide are listed in the The US Nuclear Regulatory Commission (NRC) guidelines.[7]The NRC guidelines also list a wide range or radioactive materials in solid, liquid and gaseous forms that are used as field flood or enhanced oil and gas recovery study applications tracers used in single and multiple wells.[7]

    Except for diesel-based additive fracturing fluids, noted by the American Environmental Protection Agency to have a higher proportion of volatile organic compounds and carcinogenic BTEX, use of fracturing fluids in hydraulic fracturing operations was explicitly excluded from regulation under the American Clean Water Act in 2005, a legislative move that has since attracted controversy for being the product of special interests lobbying.

    Proppant permeability and mesh size

    Proppants used should be permeable or permittive to gas under high pressures; the interstitial space between particles should be sufficiently large, yet have the mechanical strength to withstand closure stresses to hold fractures open after the fracturing pressure is withdrawn. Large mesh proppants have greater permeability than small mesh proppants at low closure stresses, but will mechanically fail (i.e. get crushed) and produce very fine particulates (“fines”) at high closure stresses such that smaller-mesh proppants overtake large-mesh proppants in permeability after a certain threshold stress.[8]

    Though sand is a common proppant, untreated sand is prone to significant fines generation; fines generation is often measured in wt% of initial feed. A commercial newsletter from Hexion cites untreated sand fines production to be 23.9% compared with 8.2% for lightweight ceramic and 0.5% for their product. [9] One way to maintain an ideal mesh size (i.e. permeability) while having sufficient strength is to choose proppants of sufficient strength; sand might be coated with resin, or a different proppant material might be chosen altogether– popular alternatives include ceramic, glass, and sintered bauxite.

    Proppant weight and strength

    Increased strength often comes at a cost of increased density, which in turn demands higher flow rates, viscosities or pressures during fracturing, which translates to increased fracturing costs, both environmentally and economically. [10] Lightweight proppants conversely are designed to be lighter than sand (~2.5 g/cc) and thus allow pumping at lower pressures or fluid velocities. Light proppants are less likely to settle. Porous materials can break the strength-density trend, or even afford greater gas permeability. Proppant geometry is also important; certain shapes or forms amplify stress on proppant particles making them especially vulnerable to crushing (a sharp discontinuity can classically allow infinite stresses in linear elastic materials). [11]

    Proppant deposition and post-treatment behaviours

    Proppant mesh size also impacts fracture length: proppants can be “bridged out” if the fracture width decreases to less than twice the size of the diameter of the proppant. [21] As proppants are deposited in a fracture, proppants can resist further fluid flow or the flow of other proppants, inhibiting further growth of the fracture. In addition, closure stresses (once external fluid pressure is released) may cause proppants to reorganise or “squeeze out” proppants, even if no fines are generated, resulting in smaller effective width of the fracture and decreased permeability. Some companies try to cause weak bonding at rest between proppant particles in order to prevent such reorganisation. [9] The modelling of fluid dynamics and rheology of fracturing fluid and its carried proppants is a subject of active research by the industry.

    Proppant costs

    Though good proppant choice positively impacts output rate and overall ultimate recovery of a well; commercial proppants are also constrained by cost. Transport costs from supplier to site form a significant component of the cost of proppants.

    References

    1. ^ Mader, Detlef (1989). Hydraulic proppant fracturing and gravel packing. Amsterdam: Elsevier. ISBN 0-444-87352-X. http://books.google.com/books?id=FyGcOI42oBMC&pg=PA473&lpg=PA473.
    2. ^ Hodge, Richard. “Crosslinked and Linear Gel Comparison”. EPA HF Study Technical Workshop. Environmental Protection Agency. http://www.epa.gov/hfstudy/cross-linkandlineargelcomposition.pdf. Retrieved 8 February 2012.
    3. ^ Reis, John C. (1976). Environmental Control in Petroleum Engineering. Gulf Professional Publishers.
    4. ^ a b [1] Scott III, George L. (03-June-1997) US Patent No. 5635712: Method for monitoring the hydraulic fracturing of a subterranean formation. US Patent Publications.
    5. ^ [2] Scott III, George L. (15-Aug-1995) US Patent No. US5441110: System and method for monitoring fracture growth during hydraulic fracture treatment. US Patent Publications.
    6. ^ [3] Gadeken, Larry L., Halliburton Company (08-Nov-1989). Radioactive well logging method.
    7. ^ a b Jack E. Whitten, Steven R. Courtemanche, Andrea R. Jones, Richard E. Penrod, and David B. Fogl (Division of Industrial and Medical Nuclear Safety, Office of Nuclear Material Safety and Safeguards (June 2000). “Consolidated Guidance About Materials Licenses: Program-Specific Guidance About Well Logging, Tracer, and Field Flood Study Licenses (NUREG-1556, Volume 14)”. US Nuclear Regulatory Commission. http://www.nrc.gov/reading-rm/doc-collections/nuregs/staff/sr1556/v14/#_1_26. Retrieved 19 April 2012. “labeled Frac Sand…Sc-46, Br-82, Ag-110m, Sb-124, Ir-192″
    8. ^ “Physical Properties of Proppants”. CarboCeramics Topical Reference. CarboCeramics. http://archive.carboceramics.com/English/tools/topical_ref/tr_physical.html. Retrieved 24 January 2012.
    9. ^ a b “Critical Proppant Selection Factors”. Fracline. Hexion. http://www.momentivefracline.com/critical-proppant-selection-factors.
    10. ^ Rickards, Allan; et al (May 2006). “High Strength, Ultralightweight Proppant Lends New Dimensions to Hydraulic Fracturing Applications”. SPE Production & Operations 21 (2): 212–221. http://www.spe.org/ejournals/jsp/journalapp.jsp?pageType=Preview&jid=EPF&mid=SPE-84308-PA.
    11. ^ Guimaraes, M. S.; et al. (2007). “Aggregate production: Fines generation during rock crushing”. Journal of Mineral Processing. http://pmrl.ce.gatech.edu/papers/Guimaraes_2007a.pdf.

     

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    Water contamination news: – Archives EPA study says hydraulic fracturing likely contaminated drinking water In Wyoming town.

     Environmental Protection Agency announced Thursday that it suspects hydraulic fracturing in a shallow natural gas well in Wyoming contaminated a town’s drinking water, Drinking water contamination news. Save the water  Volume 3

     Environmental Protection Agency announced Thursday that it suspects hydraulic fracturing in a shallow natural gas well in Wyoming contaminated a town’s drinking water,Save the water,current post

    Update
    Vol.III
    Archives
    Originally Posted
    NewsOK.com
    CHRIS CASTEEL
    December 9, 2011
    July 14
    2012

     Environmental Protection Agency announced Thursday that it suspects hydraulic fracturing in a shallow natural gas well in Wyoming contaminated a town’s drinking water


    The material posted is
    courtesy of
    NewsOK.com
    CHRIS CASTEEL
    Save the Water™
    Water Research
    Education Dept.
    and is shared as
    educational material only

     

     Environmental Protection Agency announced Thursday that it suspects hydraulic fracturing in a shallow natural gas well in Wyoming contaminated a town’s drinking water,Drinking water contamination news



    ,Contaminated drinking Water

     


     
     
     

    Rating for savethewater.org

    EPA study says hydraulic fracturing likely contaminated drinking water in Wyoming town

    WASHINGTON — The Environmental Protection Agency announced Thursday that it suspects hydraulic fracturing in a shallow natural gas well in Wyoming contaminated a town’s drinking water. After three years of study, the agency concluded that chemicals found in the aquifer and in individual wells were consistent with those used in hydraulic fracturing.

    The agency issued a report that will be open for public comment and scientific review. If it is finalized with the same conclusions, it could provide the first documented case in which “fracking” contaminated groundwater.

    “Alternative explanations were carefully considered to explain individual sets of data,” the draft report says. “However, when considered together with other lines of evidence, the data indicates likely impact to ground water that can be explained by hydraulic fracturing.”

    Inhofe comments

    Sen. Jim Inhofe, R-Tulsa, said the agency’s findings were premature and political, while an environmental group called the study “a huge blow to the oil and gas industry.”

    Hydraulic fracturing, which has been used for more than 50 years on oil and gas wells, involves pumping water, sand and a small amount of chemicals into a well to create cracks in shale formations.

    The process, in tandem with horizontal drilling, has been used increasingly by the industry to produce oil and gas that was previously considered too difficult to recover. It has come under increasing scrutiny and criticism as its use has expanded, and some have charged that it poses a threat to groundwater.

    Though there have been incidents in which “flowback” water used in a well was improperly handled, the industry has countered criticisms of hydraulic fracturing by saying there had not been a documented case in which the process itself caused contamination.

    The EPA study in Pavillion, Wyo., began in 2008 after residents complained that their water smelled and tasted bad. The residents lived near a gas field controlled by Encana, a Canadian energy company.

    According to the EPA, the agency constructed two monitoring wells to sample water in the aquifer.

    “EPA’s analysis of samples taken from the agency’s deep monitoring wells in the aquifer indicates detection of synthetic chemicals, like glycols and alcohols consistent with gas production and hydraulic fracturing fluids, benzene concentrations well above Safe Drinking Water Act standards and high methane levels,” the agency said in a statement.

    Contaminants migrate

    “Given the area’s complex geology and the proximity of drinking water wells to ground water contamination, EPA is concerned about the movement of contaminants within the aquifer and the safety of drinking water wells over time.”

    Water in private wells tested by the EPA contained compounds “consistent with migration from areas of gas production,” the agency said.

    The Environmental Protection Agency noted, however, that the fracturing in Pavillion is taking place “in and below the drinking water aquifer and in close proximity to drinking water wells — production conditions different from those in many other areas of the country.”

    Industry experts have often said that most fracturing occurs a mile or more below the surface, while groundwater is close to the surface, and that there is no way that fracking water or gas could migrate to drinking water from those depths.

    Inhofe has been of the most vocal defenders in Congress of hydraulic fracturing and has been following the EPA’s work in Pavillion and its national study of fracking. Thursday he said the EPA draft report was part of President Barack Obama’s “war on fossil fuels.”

    “EPA’s conclusions are not based on sound science but rather on political science,” Inhofe said.

    “Its findings are premature, given that the agency has not gone through the necessary peer-review process, and there are still serious outstanding questions regarding EPA’s data and methodology.”

    Wenonah Hauter, executive director of Food and Water Watch, said the draft report “illustrates the dangers of moving forward with a technology before we know the facts. It is also a huge blow to the oil and gas industry, who has continued to insist that fracking is safe.”

    A 30-day peer-review process led by a panel of independent scientists also will be conducted.

    via EPA study says hydraulic fracturing likely contaminated drinking water in Wyoming town | NewsOK.com.
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