Marcellus Shale Gas: Development Potential and Water Management Issues and Laws

Congressional research reportJan 27, 2012

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Marcellus Shale Gas: Development Potential

and Water Management Issues and Laws

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January 27, 2012

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R42333

CRS Report for Congress

Prepared for Members and Committees of Congress

Marcellus Shale Gas: Development Potential and Water Management Issues and Laws

Summary

Until relatively recently, natural gas-rich shale formations throughout the United States were not

considered to have significant resource value because no technologies existed to economically

recover the gas. Development and deployment of advanced drilling and reservoir stimulation

methods have dramatically increased the gas production from these “unconventional gas shales.”

The Marcellus Shale formation potentially represents one of the largest unconventional natural

gas resources in the United States, underlying much of West Virginia and Pennsylvania, southern

New York, eastern Ohio, western Maryland, and western Virginia. Directional drilling and

“hydraulic fracturing” are essential to exploiting these low permeability shale gas resources.

Although oil and gas developers have applied these technologies in conventional oil and natural

gas fields for some time, recent improvements in both technologies have allowed them to be

applied effectively to unconventional gas shales on an industrial scale.

While creating significant economic benefits, development of the Marcellus Shale faces

infrastructure challenges, such as the need for gathering pipelines. Marcellus development also

has generated controversy due to its potential scale and its potential impacts on land and water

resources, communities, public infrastructure, and environmental quality.

Several water quality issues have arisen, including concerns about the potential for hydraulic

fracturing operations to contaminate groundwater and drinking water supplies. The 111th

Congress urged the U.S. Environmental Protection Agency (EPA) to study this issue, and the

agency expects to publish initial research results in 2012 and a final report in 2014. Notably, EPA

does not have the authority to regulate hydraulic fracturing (except where diesel fuel is used).

Additionally, managing the large volumes of wastewater produced during natural gas production

(including flowback from hydraulic fracturing and water produced from the shale formation) has

emerged as a major water quality issue related to Marcellus development. In some areas across

the Marcellus Shale region, the geology may limit the use of underground injection wells (the

most common produced-water disposal practice in oil and gas fields), and wastewater disposal is

posing treatment, quality, and regulatory challenges. Both industry best practices and state

regulations continue to evolve.

Other concerns associated with shale gas development include the contamination of water from

surface spills, migration of methane gas and contaminants into residential water wells from faulty

well construction, siltation of streams from drilling and pad construction activities, and potential

impacts that large water withdrawals might have on water resources, streams, and aquatic life.

The development of the Marcellus Shale on private or state land is subject primarily to state laws

and regulations, including requirements for well construction and operation. Provisions of two

federal water quality laws—the Safe Drinking Water Act (SDWA) and the Clean Water Act

(CWA)—can apply to activities related to wastewater disposal through underground injection and

discharge to surface waters. Additionally, several of the states include watersheds that are subject

to water resource regulations resulting from the adoption of interstate compacts (primarily the

Delaware River Basin Compact and the Susquehanna River Basin Compact).

This report reviews the Marcellus Shale resource, development processes, and related surface

water and groundwater issues. It also discusses related federal and state regulatory authorities and

related developments, and pending federal legislation.

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Marcellus Shale Gas: Development Potential and Water Management Issues and Laws

Contents

Introduction...................................................................................................................................... 1

The Marcellus Shale as a U.S. Natural Gas Province...................................................................... 3

Unconventional Gas Shale Resources in the United States....................................................... 3

Geology of the Marcellus Shale Formation............................................................................... 4

Natural Gas Resource Potential of the Marcellus Shale............................................................ 7

Regional Natural Gas Supply and Demand............................................................................... 8

Shale Gas Well Drilling and Stimulation......................................................................................... 9

Well Construction and Casing ................................................................................................. 11

Hydraulic Fracturing ............................................................................................................... 13

Fracturing Fluids ............................................................................................................... 14

Hydraulic Fracture Process ............................................................................................... 15

Potential Risks to Groundwater............................................................................................... 15

Federal and State Laws and Regulations Affecting Marcellus Shale Gas Development............... 18

Surface Water Quality Protection ............................................................................................ 18

Other Surface Water Quality Issues......................................................................................... 23

Groundwater and Drinking Water Protection .......................................................................... 24

Federal Underground Injection Control Program.............................................................. 26

Underground Injection of Shale Gas Wastewater.............................................................. 28

State Water Quality Laws ........................................................................................................ 29

Water Supply Management ..................................................................................................... 32

State Regulation of Water Resources ................................................................................ 33

Interstate Compacts in the Marcellus Shale Region.......................................................... 35

Congressional Interest.................................................................................................................... 38

Pending Federal Legislation.............................................................................................. 38

Conclusion ..................................................................................................................................... 40

Figures

Figure 1. Marcellus Shale Location and Thickness Across the Region........................................... 5

Figure 2. Marcellus Shale Depth and Transition Between Wet and Dry Gas .................................. 6

Figure 3. Northeast Region Natural Gas Pipeline Network............................................................. 9

Figure 4. Traditional Wells vs. Multi-Well Pad ............................................................................. 10

Figure 5. Typical Well Casing and Horizontal Well Schematic..................................................... 12

Figure 6. New York State Areas Where Shale Development Is to Be Prohibited.......................... 31

Figure 7. Major River Basins and Sub-Basins Overlying the Marcellus Shale............................. 36

Contacts

Author Contact Information........................................................................................................... 44

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Marcellus Shale Gas: Development Potential and Water Management Issues and Laws

Introduction

Until relatively recently, natural gas-rich shale formations throughout the United States were not

considered to have significant resource value because no technologies existed to economically

recover the gas. Development and deployment of advanced drilling and reservoir stimulation

methods have dramatically increased the gas production from these “unconventional gas shales.”

The Marcellus Shale formation of the Appalachian basin, in the northeastern United States,

potentially represents one of the largest unconventional natural gas resources in the United States.

Natural gas prices have fallen significantly in the last five years, but particularly since mid-2008

due in large part to the development of shale gas. Prices briefly exceeded $13 per million Btu

(MBtu) in 2008, but fell below $4 per MBtu by the summer of 2009.1 The Energy Information

Administration (EIA) expects that the Henry Hub spot price for natural gas will average $3.53 per

MBtu in 2012, a drop of $0.47 per MBtu from the 2011 average.2 However, increased drilling

activity in Pennsylvania and West Virginia and industry presence in New York and Maryland

reflect strong interest in the Marcellus Shale. As a result, natural gas reserves in the United States

may show a significant increase.3 Low natural gas prices have raised expectations that demand

for natural gas will increase. Moreover, unlike the natural gas found in some regions, the gas

produced from the eastern portion of the Marcellus formation is of high enough quality that it

requires minimal treatment for injection into transmission pipelines. Multiple gas transmission

pipelines already serve the northeast United States. The Millennium Pipeline project in southern

New York could accommodate increased shale gas production from New York and parts of

Pennsylvania to serve the natural gas needs of the region. West Virginia may face obstacles to

developing additional pipeline capacity and other infrastructure, as its terrain is more rugged. Gas

producers would also have to construct an extensive network of gathering pipelines to bring the

gas out of the fields to market. One study by the Interstate Natural Gas Association of America

estimated that almost 60,000 miles of gathering pipelines would be needed in the Marcellus area.4

Directional drilling and “hydraulic fracturing” are essential to exploiting shale gas resources.

Although oil and gas developers have applied these technologies in conventional oil and natural

gas fields for some time, recent improvements in both technologies have allowed them to be

applied effectively to unconventional gas shales on an industrial scale. As a result, gas

development has expanded in traditional gas producing areas, and has moved into areas that may

have rugged topography, dense vegetation, higher population densities, and where residents may

be less familiar with the oil and gas exploration and production industry.

Shale gas development in the Marcellus region has been particularly controversial. The potential

economic benefits from both the drilling activities and the lease and royalty payments compete

with the public’s concern for environmentally safe drilling practices and protection of

1

See U.S. Department of Energy (DOE), Energy Information Administration (EIA), Natural Gas page,

http://www.eia.doe.gov/oil_gas/natural_gas/info_glance/natural_gas.html.

2

EIA, Short-Term Energy Outlook, December 6, 2011, http://www.eia.doe.gov/emeu/steo/pub/

contents.html#Natural_Gas_Markets.

3

“Reserves are those quantities of petroleum, which, by analysis of geoscience and engineering data, can be estimated

with reasonable certainty to be commercially recoverable ...” in: Society of Petroleum Engineers, Petroleum Resources

Management System, 2007, p. 3, http://www.spe.org/spe-app/spe/industry/reserves/prms.htm.

4

“INGAA: Study Predicts $20 Billion in Pipeline Projects Headed for Marcellus,” Pittsburgh Business Times, May 24,

2011.

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groundwater and surface water resources. Water supply is an important issue because hydraulic

fracturing requires large amounts of fresh water, but contamination of water resources is also a

major concern to many across the region.

As with oil and gas production generally, development of the Marcellus Shale is primarily subject

to state law and regulation, and requirements for well construction and operation differ among the

states. Additionally, provisions of two federal laws—the Safe Drinking Water Act (SDWA) and

the Clean Water Act (CWA)—can apply to some activities, specifically those related to

wastewater disposal through underground injection or discharge to surface waters. The SDWA

exempts from regulation the underground injection of fluids (except diesel fuel) for hydraulic

fracturing.5 Two bills introduced in the 112th Congress (as in the last Congress) would remove the

exemption and explicitly authorize regulation of hydraulic fracturing under the SDWA.6

As exploration and production activities have increased, so has concern that development of the

Marcellus Shale could harm human health and the environment. One concern is that hydraulic

fracturing or faulty well construction might damage groundwater and drinking water wells by

introducing chemicals, natural gas,7 and other contaminants into aquifers. A second issue is the

potential contamination of water wells from surface activities related to gas production.

Accidental spills, leaky surface impoundments, equipment failure, or careless surface disposal of

drilling fluids8 at the natural gas production site could increase the risk of contaminating a nearby

water well or run off to surface water.

Managing the wastewater produced from the fracturing process has emerged as a major water

resource issue in the Marcellus region. Critics maintain that improper treatment and disposal of

the large quantities of water used for, and resulting from, the hydraulic fracturing process may

harm local and regional water supplies and that disposing the “flowback” and brine extracted

from the shale after fracturing may affect the water quality of lakes, rivers, and streams and

potentially damage public wastewater treatment plants and water supplies.

Gas producers have pointed out that virtually all oil and natural gas production, including all the

historical conventional production in the United States, requires wells that penetrate the local

groundwater aquifers. Several shale gas contamination incidents have been attributed to poor well

construction or surface activities that would be associated with any oil or gas drilling and

production operation, and not just with the unique techniques associated with the hydraulic

fracturing process. However, these observations emphasize the importance of good well design

5

The Energy Policy Act (EPAct) of 2005 (P.L. 109-58, §322), amended the SDWA to exempt from the definition of

underground injection the injection of fluids or propping agents (other than diesel fuel) for hydraulic fracturing

purposes. For a discussion of the background of this provision and the EPA underground injection control program and

its role in regulating hydraulic fracturing, see CRS Report R41760, Hydraulic Fracturing and Safe Drinking Water Act

Issues, by (name redacted) and (name redacted).

6

H.R. 1084 and S. 587, the Fracturing Responsibility and Awareness of Chemicals Act (FRAC Act), would amend the

SDWA to repeal the exemption for hydraulic fracturing operations that was established in EPAct 2005, and would

amend the term “underground injection” to include explicitly the injection of fluids used in hydraulic fracturing

operations related to oil and gas production, thus authorizing EPA to regulate this process under the SDWA.

7

Methane is the dominant component of natural gas, but it may also contain lesser amounts of ethane, propane, butane,

and other hydrocarbons.

8

Drilling fluids are composed primarily of water and minerals in a mud used to remove drill cuttings during the drilling

process. Drilling fluids are different from the hydraulic fracturing fluids, which are introduced after the well is drilled.

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and construction for any wells that penetrate local aquifers, regardless of their purpose. (See

“Well Construction and Casing,” below.)

Incidents of well-water contamination have been reported as Marcellus Shale development has

expanded. In one case, Pennsylvania regulators confirmed that methane had migrated from

drilling sites to private drinking water wells, and issued notices of violations to a drilling

company for, among other things, “failure to prevent gas from entering fresh groundwater.”9 In

this case, state regulators attributed the contamination to faulty well construction.10

In some cases of well-water contamination attributed to gas development in various gas

producing areas, the source of contamination remains undetermined. Identifying the cause of

contamination can be difficult for various reasons, including the complexity of hydrogeologic

processes and investigations, and a lack of baseline testing of nearby water wells prior to drilling

and fracturing, as well as the confidential business information status historically given to

fracturing compounds across the states. Major oil and gas producing states have asserted that the

hydraulic fracturing process has not been linked directly to groundwater contamination.11

However, contamination incidents attributed to poor well construction have raised concerns

regarding the adequacy and/or enforcement of state well construction regulations for managing

oil and gas development that increasingly depends on fracturing. This report discusses the

Marcellus Shale resource, technical methods used to develop it, and associated groundwater and

surface water issues.12 The report also discusses relevant federal and state regulatory authorities,

recent developments at the federal and state levels, and pending federal legislation.13

The Marcellus Shale as a U.S. Natural Gas Province

Unconventional Gas Shale Resources in the United States

Unconventional gas shales are fine-grained, organic-rich, sedimentary rocks. The shales are both

the source of and the reservoir for natural gas, unlike conventional petroleum reservoirs. In the

shales, gas freely occupies pore spaces, and organic matter adsorbs gas on its surface.14 The

9

Pennsylvania Department of Environmental Protection (PA DEP), Consent Order and Agreement, November 4, 2009;

http://www.dep.state.pa.us/dep/deputate/minres/oilgas/Final%20COA%20121510.pdf. PA DEP determined that 18

drinking water supplies serving 19 homes in the Dimock, PA, area were affected by drilling activities.

10

John Hanger, Secretary, Pennsylvania Department of Environmental Protection, Letter to Cabot Oil, October 19,

2010, http://wbcitizensvoice.com/pdfs/HangerLetter.pdf.

11

See, for example, the Ground Water Protection Council at http://www.gwpc.org. The GWPC is an association of

state groundwater and underground injection control agencies responsible for protecting and conserving groundwater.

12

Other environmental concerns associated with the development of the Marcellus Shale include potential air quality

impacts, increased truck traffic, and land use changes (including those related to the development of access roads,

gathering pipelines, and drill pads). Although such issues can be significant for state regulators, gas developers, local

communities, and landowners, they are not addressed in this report.

13

This report replaces CRS Report R40894, Unconventional Gas Shales: Development, Technology, and Policy Issues,

coordinated by (name redacted).

14

The Society of Petroleum Engineers describes “unconventional resources” as petroleum accumulations that are

pervasive throughout a large area and that are not significantly affected by hydrodynamic influences. (They are also

called “continuous-type deposits.”) In contrast, conventional petroleum and natural gas occur in porous sandstone and

carbonate reservoirs. Under hydrodynamic pressure exerted by water, the petroleum migrated upward from its organic

source until an impermeable cap-rock (such as shale) trapped it in the reservoir rock. The “gas-cap” that accumulated

(continued...)

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shales’ extremely small pore sizes make them relatively impermeable to gas flow, unless natural

or artificial fractures occur.

Major gas shale basins exist throughout the lower 48 United States. There are at least 21 shale

basins in more than 20 states.15 Based on a recent assessment of natural gas resources, the United

States has a resource base of 1,836 trillion cubic-feet (tcf).16 Shale gas made up an estimated onethird of this resource base, roughly 616 tcf. The U.S. Geological Survey (USGS) estimated in

2011 that the Marcellus Shale holds 84 tcf of undiscovered, technically recoverable natural gas

and 3.4 billion barrels of natural gas liquids. Annual U.S. dry natural gas production has

improved significantly in the last half decade. The 22.4 tcf produced in 2010 matched the peak

production of the early 1970s, due in large part to unconventional resources, particularly gas

shales. In 2009, the United States reclaimed the top spot as the world’s largest natural gas

producer, the first time since 2001. EIA, in its 2011 Annual Energy Outlook reference case,

forecast shale gas production to grow from about 25% of total U.S. natural gas production in

2011 to 46% in 2035.

Geology of the Marcellus Shale Formation

The Marcellus Shale is a sedimentary rock formation deposited over 350 million years ago during

the middle-Devonian period on the geologic timescale. Geologic strata deposited in the

Appalachian basin during this period are more likely to produce gas than oil. Regional oil

production is associated with Pennsylvanian age strata (of the later Carboniferous period). The

black, organic-rich, Marcellus Shale lies beneath much of West Virginia, western and northeastern

Pennsylvania, southern New York, eastern Ohio, and parts of Virginia and Maryland. It is an

estimated 95,000 square miles in areal extent and ranges from 4,000 feet to 8,500 feet in depth,

running deeper the farther north it goes along the cross section.17 The shale’s thickness varies

from 50 feet to 250 feet. Some reports indicate that the shale may be as much as 900 feet thick in

places, however.18 (See Figure 1.)

(...continued)

over the petroleum has been the source of most produced natural gas. After drilling a well into a conventional

petroleum reservoir, the pressure of the gas-cap and oil-dissolved gas may be adequate, initially, to lift the oil to the

surface (i.e., gas drive). Water trapping the petroleum from below also exerts an upward hydraulic pressure (water

drive). Petroleum reservoirs produced by the pressure of their natural gas and water drives are thus termed

“conventional drive.” After a reservoir’s production declines, lifting further petroleum to the surface requires

pumping—giving rise to the term “artificial lift.”

15

Navigant Consulting, North American Natural Gas Supply Assessment, for Clean Skies Foundation, July 4, 2008.

16

Colorado School of Mines, Potential Gas Committee Reports Unprecedented Increase in Magnitude of U.S. Natural

Gas Resource Base, June 18, 2009, http://www.mines.edu/Potential-Gas-Committee-reports-unprecedented-increasein-magnitude-of-U.S.-natural-gas-resource-base.

17

DOE, Office of Fossil Energy and the National Energy Technology Laboratory, Modern Shale Gas Development in

the United States: A Primer, DE-FG26-04NT15455, April 2009, http://fossil.energy.gov/programs/oilgas/publications/

naturalgas_general/Shale_Gas_Primer_2009.pdf.

18

U.S. Geological Survey, Assessment of Undiscovered Natural Gas Resources in Devonian Black Shales,

Appalachian Basin, Eastern U.S.A, Open-File Report 200-1268, 2005.

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Figure 1. Marcellus Shale Location and Thickness Across the Region

Source: Marcellus Center for Outreach and Research (MCOR), Penn State University,

http://www.marcellus.psu.edu.

Typically, thicker shales with greater organic material yield more gas, and thus are more

economically desirable to produce. Shale in northeast Pennsylvania and southeast New York has

these characteristics and produces dry pipeline quality natural gas.19 Shale in western New York

and western Pennsylvania produces a wetter gas that contains natural gas liquids that must be

removed from the gas before it can be piped and used. Natural gas liquids (NGL), such as ethane,

butane and propane, add to gas shale profitability and increase the incentive to produce the shale

when natural gas prices are low. (See Figure 2.)

19

The natural gas received and transported by the major intrastate and interstate mainline transmission systems must

meet the quality standards specified by pipeline companies in the “General Terms and Conditions (GTC)” section of

their tariffs. These quality standards vary from pipeline to pipeline and are usually a function of a pipeline system’s

design, its downstream interconnecting pipelines, and its customer base. In general, these standards specify that the

natural gas be within a specific Btu content range (1,035 Btu per cubic foot, +/- 50 Btu); be delivered at a specified

hydrocarbon dew point temperature level (below which any vaporized gas liquid in the mix will tend to condense at

pipeline pressure); contain no more than trace amounts of certain components such as hydrogen sulfide, carbon dioxide,

nitrogen, water vapor, and oxygen; and be free of particulate solids and liquid water that could damage the pipeline or

its ancillary operating equipment. EIA, Natural Gas Processing: The Crucial Link Between Natural Gas Production

and Its Transportation to Market, http://www.eia.doe.gov/pub/oil_gas/natural_gas/feature_articles/2006/ngprocess/

ngprocess.pdf.

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Figure 2. Marcellus Shale Depth and Transition Between Wet and Dry Gas

Source: Marcellus Center for Outreach and Research (MCOR), Penn State University,

http://www.marcellus.psu.edu.

Note: Natural gas liquids (NGL) that may be present in wet gas include butane, ethane, and propane.

The Utica Shale is an organic-rich black shale source rock that underlies the Marcellus Shale. It

contains both conventional oil and gas resources and unconventional gas resources. The majority

of the oil and natural gas discovered in this petroleum system is located on the east-dipping,

western flank of the Appalachian basin in central and eastern Ohio, northwestern Pennsylvania,

and western New York. Generally, the oil and (or) gas fields produce from a variety of lower

Paleozoic reservoirs at depths of less than 6,000 feet. The total Utica–Lower Paleozoic petroleum

system is estimated to represent an estimated 1.8 billion to 2.4 billion barrels of oil equivalent

(BBOE).20

USGS has identified three principal hydrogeological (groundwater) environments overlying the

Marcellus Shale: (1) glacial sand and gravel aquifers in New York, northern Pennsylvania, and

northeastern Ohio, (2) valley-and-ridge carbonate rock and other aquifers in Pennsylvania and

eastern West Virginia, and (3) Mississippian sandstone aquifers in northern Pennsylvania and

northeastern Ohio. These aquifer systems are important supplies of fresh water for communities

20

USGS, Assessment of Appalachian Basin Oil and Gas Resources: Utica-Lower Paleozoic Total Petroleum System,

Open-File Report 2008–1287, 2008.

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and landowners, especially in rural areas, although most residents of these states generally obtain

their drinking water from surface water sources. Typically, these aquifers are much closer to the

ground surface than the Marcellus Shale, which can be thousands of feet deep; the groundwater

wells in these states may reach only several hundred feet in depth.

The layers of rocks separating most fresh water aquifers from the Marcellus Shale are typically

siltstones and shales layered with minor sandstones and limestone. Siltstones and shales generally

act as barriers to fluid flow. These intervening layers of rocks can be several thousand feet thick

in the eastern and northern portions of the area where the Marcellus Shale is deepest. On the

western and southern portions of the area, the Marcellus Shale is shallower, and separated from

the potentially usable groundwater above by a thinner package of siltstones and shales. An

overarching concern for developing the Marcellus Shale is the potential for affecting the

overlying aquifers.

Natural Gas Resource Potential of the Marcellus Shale

The Marcellus Shale’s resource potential has been the subject of various interpretations. A 2005

USGS estimate placed the shale’s mean undiscovered conventional natural gas resource potential

at nearly 2 tcf, and possibly as high as 12 tcf, considering the total extent of Devonian/Ohio basin

shales (which include the Marcellus formation), with the qualification that not all of the gas may

be economically recoverable. At the time of the 2005 estimate, hydraulic fracturing was not yet

being used to recover gas from shale, and that USGS estimate include no unconventional

resources.

A 2008 estimate by two geoscience professors raised the resource potential to 516 tcf, based on

limited production data from companies using horizontal drilling and hydraulic fracturing to

recover the shale gas.21 In July 2011, EIA released a contractor report reviewing various shale gas

plays throughout the United States.22 The report estimated that ultimate recovery from the current

area under lease (10,622 square miles) could reach 177.9 tcf, and the undeveloped areas (84,271

square miles) could reach 232.4 tcf (for a combined total of 410.3 tcf). EIA also estimated that a

Marcellus well may ultimately produce 2.3 billion cubic feet (bcf) of natural gas, on average.

Assuming $4 per 1,000 cubic feet of gas at the well head (comparable to current prices),

producers might realize $9 million per well.

In August 2011, USGS revised its assessment to include more detailed geologic studies of the

Marcellus Shale using recent shale gas production data to estimate both conventional and

unconventional volumes of undiscovered, technically recoverable shale gas. The new USGS

assessment increased the mean undiscovered estimate to slightly more than 84 tcf.23 Although

considerably higher than its 2008 estimate, it is substantially lower than EIA’s 2011 estimate (and

thus the recent controversy about conflicting government estimates of shale gas in the Marcellus

Shale).

21

Terry Engelder, “Marcellus,” Basin Oil & Gas, August 2009, pp. 18-22, http://www.fwbog.com/.

EIA, Review of Emerging Resources: U.S. Shale Gas and Shale Oil Plays, July 2011.

23

USGS, Assessment of Undiscovered Oil and Gas Resources of the Devonian Marcellus Shale of the Appalachian

Basin Province, 2011; Fact Sheet 2011-3092; August 2011.

22

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Both EIA and USGS have significantly revised their technically recoverable resource (TRR)

estimates for the Marcellus Shale based on newly available information. Using data though 2010,

USGS increased its TRR estimate to 84 tcf from its 2002 estimate of 2 tcf. (USGS assigned a

90% confidence level that the TRR ranges from 43 to 144 tcf.) EIA decreased its estimate for the

Marcellus Shale from 410 tcf to 141 tcf. EIA used more recent drilling and production data

available through 2011 and excluded production experience from the pre-shale era (before

2008).24

The various estimates of the Marcellus resource potential appear to hinge on assumptions made

regarding the success in applying advanced drilling and well stimulation technology. However,

reconciling these estimates exceeds this report’s scope.

Regional Natural Gas Supply and Demand

In 2009, the northeast region consumed roughly 4 tcf of natural gas.25 New York led the region in

consumption, with over 1.14 tcf. The United States as a whole consumed nearly 23 tcf.26 The

northeast region produced roughly 580 bcf of natural gas from more than 121,000 operating gas

wells. Pennsylvania and West Virginia combined made up nearly 89% of the production, with

New York and Virginia making up the balance.27 In summary, the region consumes about seven

times as much natural gas as it currently produces. The 410.3 tcf of gas, estimated by EIA as

technically recoverable from the Marcellus Shale, would be sufficient to supply the region

through the century at the current rate of consumption. The USGS estimate of 84 tcf would

supply the region’s entire natural gas demand for more than 21 years at current rates of

consumption.

Pipelines are needed to collect and distribute natural gas, and the major pipeline infrastructure in

the northeast/mid-Atlantic region is in place to take advantage of Marcellus production. Twenty

interstate natural gas transmission pipelines serve the northeast region of the United States. (See

Figure 3.) This pipeline system delivers natural gas to several intrastate natural gas pipelines and

at least 50 local distribution companies in the region. In addition to the natural gas produced in

the region, several long-distance natural gas transmission pipelines supply the region from the

Southeast into Virginia and West Virginia, and from the Midwest into West Virginia and

Pennsylvania. Canadian imports come into the region principally through New York, Maine, and

New Hampshire. Liquefied natural gas (LNG) supplies also enter the region through import

terminals in Massachusetts, Maryland, and New Brunswick, Canada.

Although the gas-transmission pipeline network needed to supply the northeast United States is in

place, gas producers would need to construct an extensive network of gathering pipelines and

supporting infrastructure to move the gas from the well fields to the transmission pipelines. A lack

of this infrastructure may constrain development in some parts of the Marcellus region.

24

EIA, AEO2012 [Annual Energy Outlook] Early Release Overview, January 2012, http://www.eia.gov/forecasts/aeo/

er/.

25

EIA, Natural Gas Consumption by End Use, http://tonto.eia.doe.gov/dnav/ng/ng_cons_sum_dcu_nus_a.htm.

26

Reported by EIA as 22.84 tcf for 2009, and 24.13 tcf for 2010, http://tonto.eia.doe.gov/dnav/ng/

ng_cons_sum_dcu_nus_a.htm.

27

Ohio lies outside the northeast region but is a significant gas producing state with Devonian and also Marcellus Shale

gas resources. In 2009, Ohio had some 35,000 operating gas wells; the state produced 0.98 tcf and consumed 0.74 tcf of

natural gas.

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Figure 3. Northeast Region Natural Gas Pipeline Network

Source: EIA, Office of Oil & Gas, Natural Gas Division, Gas Transportation Information System,

http://www.eia.doe.gov/pub/oil_gas/natural_gas/analysis_publications/ngpipeline/northeast.html.

Note: Includes Connecticut, Delaware, Massachusetts, Maine, New Hampshire, New Jersey, New York,

Pennsylvania, Rhode Island, Virginia, and West Virginia.

Shale Gas Well Drilling and Stimulation

Well drilling technology has progressed markedly over the last 50 years. An important recent

advance in drilling is the ability to direct the drill bit horizontally beyond the region immediately

beneath the drill rig.28 It is this directional drilling, in combination with hydraulic fracturing, that

has made it feasible to develop the Marcellus Shale and other unconventional gas and oil

formations.

Directional drilling offers a significant advantage over vertical well drilling in developing gas

shales. In the case of thin or inclined shale formations, a long horizontal well increases the length

of the well bore in the gas-bearing formation and therefore increases the surface area for gas to

28

Early directional drilling involved placing a steel wedge down-hole (whipstock) that deflected the drill toward the

desired target, but lacked control and consumed time. Advances such as steerable down-hole drill motors that operated

on the hydraulic pressure of the circulating drilling mud offered improved directional control. Newer rotary steerable

systems introduced in the 1990s drill directionally with continuous rotation from the drilling rig at surface. Continuous

rotation eliminates the need to slide a steerable down-hole motor. Rotation also leads to higher rates of penetration and

fewer incidents of the drill-string sticking. Schlumberger, Better Turns for Rotary Steerable Drilling: Overview,

http://www.slb.com/content/services/resources/oilfieldreview/ori002/01.asp?.

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flow into the well. Directional drilling technology also enables drilling a number of wells from a

single well pad, thus cutting costs and reducing environmental disturbance. (See Figure 4.)

However, this drilling technique alone is often insufficient to significantly improve gas

production without some means of artificially stimulating flow. In tight formations like shale,

inducing fractures can increase flow by orders of magnitude. However, before stimulation can

take place, the well must be cased, cemented, and completed (the well casing perforated).

Figure 4. Traditional Wells vs. Multi-Well Pad

(multi-well pad (right) used in Marcellus Shale)

Source: Chesapeake Energy, http://www.askchesapeake.com/Eagle-Ford-Shale/Drilling/Pages/information.aspx.

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In the late 1940s, drilling companies began inducing hydraulic pressure in wells to fracture the

producing formation. This fracturing process stimulated further production by effectively

increasing the area from which a single well could produce gas. Combining hydraulic fracturing

with directional drilling has opened up production of tighter (less permeable) petroleum and

natural gas reservoirs, and in particular, unconventional gas shales like the Marcellus.

Well Construction and Casing

Wells, whether commercial gas and oil or municipal water-supply, use a series of telescoping steel

well casings to prevent well-bore collapse and water infiltration while drilling. The casing also

conducts the produced reservoir fluids (gas or oil) to the surface. A properly designed and

cemented casing also prevents reservoir fluids from infiltrating the overlying aquifers.

During the first phase of drilling, termed “spudding-in,” shallow casing is installed underneath

the drilling platform to reinforce the ground surface. Drilling continues to the bottom of the water

table (or the potable aquifer), at which point the drill string is removed to lower a second casing

string, which is cemented-in and plugged at the bottom. Drillers use special oil-well cement that

expands when it sets to fill the void between the steel casing and the rock wellbore.

When properly constructed, surface casing and the casing extending to the bottom of the water

table should prevent water from flooding the well while also protecting the groundwater from

contamination by drilling fluids and reservoir fluids. (The initial drilling stages may use

compressed air in place of drilling fluids to avoid contaminating the potable aquifer.) Drilling and

casing then continue to the “pay zone”—the formation that produces gas or oil. The number and

length of the casings will depend on the depth and the properties of the geologic strata. (See

Figure 5.)

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Figure 5. Typical Well Casing and Horizontal Well Schematic

Source: American Petroleum Institute, http://www.api.org/policy/exploration/hydraulicfracturing/upload/

HYDRAULIC_FRACT_ILLUSTRATION_121609.pdf.

Note: Graphic is not necessarily a shale well and is not to scale.

After completing the well to the target depth and cementing-in the final casing, the drilling

operator may hire an oil-well service company to run a “cement evaluation log.” An electric

probe, lowered into the well, measures the cement thickness to detect anomalies that may

correlate with voids in the cement. A cement evaluation log provides the critical confirmation that

the cement will function as designed—preventing well fluids from bypassing outside the casing

and infiltrating overlying formations. Absent any cement voids, the well is ready for completion.

A perforating tool that uses explosive shape charges punctures the casing sidewall at the pay

zone. The well may then start producing under its natural reservoir pressure or, as in the case of

gas shales, may need stimulation (i.e., hydraulic fracturing). Good well construction is key to

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protecting ground water during gas production, and complaints that well stimulation treatments

(discussed below) affect drinking-water wells may have links to poor well construction practices.

Hydraulic Fracturing

Despite the Marcellus Shale formation’s abundant content of natural gas, the gas does not flow

freely from the shale because of its low permeability. Economic production depends on some

means of artificially stimulating the shale to liberate gas. Hydraulic fracture stimulation

treatments have been adapted to unconventional shale formations, such as the Barnett Shale (TX)

and Haynesville Shale (AR, LA, and TX), and more recently the Marcellus Shale.

Hydraulic fracturing involves injecting large volumes of water containing sand or other proppant

into production wells.29 Specialized chemicals are also included in the fracture fluid as surfactants

or for other purposes, and the fluid is injected under enough pressure to fracture low-permeability

geologic formations containing oil and/or natural gas.30 The sand or other proppant holds the new

fractures open to allow the oil or gas to flow freely out of the formation and into a production

well.

Typical “frac” treatments or frac jobs (as they are commonly known) are massive operations. The

oilfield service company contracted for the work may take a week to stage the job and a convoy

of trucks to deliver the equipment and large volumes of water and materials required.

One company involved in developing gas shale offered the following description of a frac job:31

Shale gas wells are not hard to drill, but they are difficult to complete. In almost every case,

the rock [pay zone] around the wellbore must be hydraulically fractured before the well can

produce significant amounts of gas. Fracturing involves isolating sections of the well in the

producing zone, then pumping fluids and proppant (grains of sand or other material used to

hold the cracks open) down the wellbore through perforations in the casing and out into the

shale.

The pumped fluid, under pressures up to 8,000 psi, is enough to crack shale as much as 3,000

ft in each direction from the wellbore. In the deeper high-pressure shales, operators pump

slickwater (a low-viscosity waterbased fluid) and proppant. Nitrogen-foamed fracturing

fluids are commonly pumped on shallower shales and shales with low reservoir pressures.

Ideally, hydraulic fractures propagate outward from the section of the well casing where it has

been perforated (completed prior to the frac job). In vertical wells, the fracture height

approximates the length of the perforated casing section, which is confined to the thickness of the

formation to maximize production. In horizontally drilled wells, the height and depth of the

fracture depend on the thickness of shale formation (in the case of the Marcellus) and the physical

29

According to the Schlumberger Oilfield Glossary, propping agents, or proppants, are “particles mixed with fracturing

fluid to hold fractures open after a hydraulic fracturing treatment. In addition to naturally occurring sand grains, manmade or specially engineered proppants, such as resin-coated sand or high-strength ceramic materials like sintered

bauxite, may also be used.” The glossary is available at http://www.glossary.oilfield.slb.com/default.cfm.

30

This process is distinct from enhanced oil and gas recovery and other secondary and tertiary hydrocarbon recovery

techniques, which involve separate wells. Injections for hydraulic fracturing are done through the production wells.

31

Schlumberger, Inc., Shale Gas: When Your Gas Reservoir is Unconventional, So is Our Solution. See

http://www.slb.com/media/services/solutions/reservoir/shale_gas.pdf.

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properties of the overlying rock formations to confine the fracture. Frac treatments attempted at

too shallow a depth may result in horizontally oriented fractures (which is undesirable), and some

state regulations identify minimum fracture depths. As noted, the depth of the Marcellus where

production is occurring generally places it far below any potential groundwater aquifers, and the

possibility of creating a fracture that reaches the near surface is remote. However, geology is

never 100% predictable or certain. (See discussion under “Potential Risks to Groundwater,”

below.)

Fracturing Fluids

Fracturing fluid functions in two ways: opening the fracture and transporting the “propping”

agent (or proppant) the length of the fracture.32 As the term propping implies, the agent functions

to prop or hold the fracture open to create conductive paths for the natural gas to reach the

wellbore so it can be produced. Silica sands and ceramic beads are the most commonly used

proppants.

Water-based fluids consist of 99% water, with the remainder made up of additives.33 Acid-based

fluids also use hydrochloric acid to dissolve the mineral matrix of carbonate formations

(limestone and dolomite) and thus improve porosity; the reaction produces calcium chloride salt

and carbon dioxide gas. Gelling agents, based on water-soluble polymers such as vegetablederived guar gum, adjust frac fluid viscosity. The most widely used additives for breaking down

fluid viscosity after fracturing are oxidizers such as ammonium (NH+4), potassium, and sodium

salt of peroxydisulfate (S2O8-2); enzyme breakers may be based on hemicellulase (actually a

mixture of enzymes which can hydrolyze the indigestible components of plant fibers). Silica flour

serves as good fluid-loss additive. Biocides added to polymer-containing fluids prevent

degradation of the polymers by bacteria (as the polysaccharides (sugar polymer) used to thicken

water are an excellent food source for bacteria). Methanol (an alcohol) and sodium thiosulfate

(Na2S2O3—an antidote to cyanide poisoning) are commonly used stabilizers added to prevent

polysaccharide gels degrading above temperatures of 200°F. Notably, the service companies

adjust the proportion of these and many other frac fluid additives to the unique conditions of each

well. In addition to the water-based frac fluids, oil-based fluids are used in hydrocarbon bearing

formations susceptible to water damage, but they are expensive and difficult to use. They have

been used primarily in coal-bed methane frac jobs. At the federal level, the Occupational Safety

and Health Administration (OSHA) requires that material safety data sheets (MSDS) accompany

each chemical used on the drill site, but the proportion of each chemical additive may be kept

proprietary.34 A number of states recently have adopted new or expanded disclosure rules for

chemicals used to stimulate wells.35

32

Michael J. Economides and Kenneth G. Nolte, ed., “Chapter 7 - Fracturing Fluid Chemistry and Proppants,” in

Reservoir Stimulation, 3rd ed. (John Wiley & Sons, LTD, 2000).

33

The fluid’s properties must exhibit the proper viscosity and low friction pressure when pumped, break down and

clean up rapidly when treatment is over, and provide good fluid-loss control (not dissipate). The fluid chemistry may be

water-based, oil-based, or acid-based, depending on the properties of the formation. Water-based fluids (sometimes

referred to as slickwater) are the most widely used (especially in shale formations) because of their low cost, high

performance, and ease of handling.

34

29 C.F.R. §§1910 Subpart Z, Toxic and hazardous substances.

35

For a discussion of disclosure developments among the states, see CRS Report R41760, Hydraulic Fracturing and

Safe Drinking Water Act Issues, by (name redacted) and (name redacted).

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Hydraulic Fracture Process

It is in the operating company’s interest to control the fractures and keep them within the

formation to maximize production. Fracture treatments are planned, monitored, and adjusted

operations that proceed in stages. Before beginning a treatment, the service company performs a

series of tests on the well to determine if it is competent to hold up to the hydraulic pressures

generated by the fracture pumps.

In the initial stage, a hydrochloric acid (HCl) solution pumped down the well cleans up residue

left from cementing the well casing. The portion of the well that lies within the shale is separated

into zones, and each zone is isolated from the rest of the well (with a cement barrier or

mechanical device) and fractured separately by the application of very high pressures to the shale

via the fracking fluid containing proppants and chemical additives. Each successive “frac” stage

pumps fluid (slickwater) and proppant down the well into each isolated zone to open and

propagate the fracture further into the formation. The treatment may last upwards of an hour or

more, with the final stage designed to flush the well. Marcellus wells are likely to receive

multiple treatments to produce multiple fractures within each zone along the horizontal wells.

A fracture treatment for a single zone may consume more than 500,000 gallons of water.36 Wells

subject to multiple treatments consume 3 million to 5 million gallons or more. For comparison, an

Olympic-size swimming pool holds over 660,000 gallons of water, and the average daily per

capita consumption of fresh water (roughly 1,430 gallons per day) works out to 522,000 gallons

over one year.37

The high injection pressure not only opens and propagates the fracture but also drives fluid into

the shale’s pore spaces. A high volume of fluid remains in the fracture and impedes gas flow to

the well if not pumped out. The subsequent “flowback” treatment attempts to recover as much of

the remaining fluid as possible without removing the proppants. The “flowback” water pumped

out of the well along with brine from the shale formation may be high in dissolved salts and frac

chemicals, however, making it unsuitable for continued use, and thus requiring disposal through

deep well injection or treatment before reuse or disposal to surface water. After the well begins

producing gas, it may produce more flowback water. Flowback disposal presents environmental

issues, as discussed in the “Surface Water Quality Protection” section below.

Potential Risks to Groundwater

The geologic environment that led to the deposition of the Marcellus Shale, and the overlying

layers of siltstone, shale, sandstone, and limestone has kept gas from the Marcellus Shale

confined at depth, and prevented it from naturally migrating upward into fresh water aquifers.

The process of developing a shale gas well—drilling through an overlying aquifer, stimulating the

well via hydraulic fracturing, completing the well, and producing the gas—is an issue of concern

for increasing the risk of groundwater contamination. Typically, well drilling and completion

practices, as described above, require that the well be sealed by casing throughout the aquifer

interval. A properly cased well would allow the gas to be produced up the well to the surface,

while preventing drilling fluids, hydraulic fracturing fluids, or natural gas from leaking into the

36

37

Modern Shale Gas Development in the United States: A Primer, pp. 58-59.

USGS, Summary of Water Use in the United States, 2000, http://ga.water.usgs.gov/edu/wateruse2000.html.

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permeable aquifer and contaminating groundwater. Similarly, groundwater in the aquifer would

be prevented from leaking down the well where it could interfere with the gas production process.

The challenge of sealing off the groundwater and isolating it from possible contamination is not

unique to development of the Marcellus Shale; thousands of oil and gas wells in New York,

Pennsylvania, West Virginia, and eastern Ohio also require similar well drilling and proper casing

procedures to protect groundwater resources. The inset to Figure 4 shows how a well could be

designed to protect against leakage into a drinking water aquifer by a succession of casing types

down the well from the surface through the aquifer. To protect against contamination, the well

must be properly designed and properly constructed. Problems could arise even for a properly

designed well—for example, if the casing is not properly cemented, and gaps or pockets in the

cement provide a pathway for fluids to migrate outside the casing. Improperly cemented wells

might also allow gas or brine to leak into the well from gas-bearing shale formations thousands of

feet above the Marcellus. The gas and brine could migrate up the well outside of the casing into

an overlying drinking water aquifer. As with the development of other gas-bearing formations,

sound well construction and operating practices are essential to reducing the risk of groundwater

contamination in the Marcellus Shale region.

Another concern is the possibility of introducing contaminants into aquifers from the hydraulic

fracturing process itself, described above. Hydraulic fracturing is intended to induce new

fractures into the Marcellus Shale and/or lengthen existing fractures. Concerns have been raised

that this process would create or extend fractures linking the Marcellus Shale to an overlying

aquifer and provide a pathway for gas or fracturing fluids to migrate. The chances of this

occurring are likely remote, because the vertical distance separating the Marcellus Shale from

most aquifers is usually much greater than the length of the fractures induced during hydraulic

fracturing. Also, thousands of feet of rock layers typically overlie the Marcellus Shale and serve

as barrier to flow. It should be noted, however, that if the shallow portions of the Marcellus Shale

are developed, then the thickness of the overlying rocks would be less and the distance from the

Marcellus to drinking water aquifers would be shorter, posing more of a risk to groundwater.38

Engineers designing and carrying out the hydraulic fracturing procedure have an incentive to

keep the fractures contained within the gas producing shale. Extending the fractures into a

surrounding formation might allow saline fluids or brines to enter the induced fracture and flow

into the gas producing portion of the shale, which could significantly hamper gas production.

Even if hydraulically induced fractures extend into overlying formations, the possibility for fluids

to leak upward into an aquifer is remote, unless those fractures are also connected to some other

pathway, such as leaky wells and casings.

In the Marcellus Shale region, a single well may need multiple hydraulic fracture treatments,

which could require injecting 3 million to 5 million gallons or more. After the formation is

hydraulically fractured, a portion of these fluids is typically recovered and pumped back out of

the well to the surface. In the Marcellus region, typically less than 35% of injected fluids are

recovered at the surface.39 Historically, produced waters from oil and gas wells have been

disposed of by injecting them into deep wells or treating them before disposal into surface

38

State geological surveys and oil and gas agencies estimate that the Marcellus Shale lies between 7,650 feet and 2,125

feet beneath treatable ground water. DOE, Modern Shale Gas Development: A Primer, p. 17.

39

In other shale gas producing regions, according to industry estimates, the volume of flowback water can range from

less than 30% to more than 70% of the original fracture fluid volume. DOE, Modern Shale Gas Development in the

United States: A Primer, p. 66.

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waters.40 Underground injection is not always a practical or economic option in the Marcellus

Shale region. (See “Underground Injection of Shale Gas Wastewater.”)

If these recovered fluids are improperly disposed of at the surface and allowed to infiltrate from

the ground surface downward, they could present a risk for contaminating shallow groundwater.

Improper surface disposal could pose a particular risk for shallow aquifer systems in northern

Pennsylvania and southern New York that are composed of very permeable unconsolidated sand

and gravel deposits. Many of these surficial sand and gravel aquifers form valley-fill deposits, in

low-lying areas or stream valleys, and are recharged by precipitation that runs off surrounding,

less permeable uplands.41 As such, they would be particularly susceptible to leaky surface

impoundments or careless surface disposal because of the relatively short distance and travel time

from the land surface to the top of the water table. New York, for example, has deemed these

unconsolidated sand and gravel aquifers “primary” or “principal” aquifers, which are highly

productive and presently are used as a significant source of water, or are a potentially abundant

water supply.42

Leaks resulting from improper disposal of fluids at the surface could be exacerbated by poorly

constructed drinking water wells in the vicinity. Generally, drinking water wells are shallower

than natural gas wells, may not be cased for the entire depth, and may not be subject to the same

level of oversight and scrutiny as natural gas wells. A water well that is not cased from the

surface, or is not constructed and cased properly, might allow contaminated water to flow from

the ground surface and enter the water well, possibly compromising the quality of drinking water

in the well and even contaminating the aquifer itself. In such instances, and particularly where

natural gas drilling and stimulation activities are nearby, leaky surface impoundments or careless

surface disposal of drilling fluids at the natural gas operation could increase the risk of

contaminating the nearby water well.

A further confounding factor in regions where drinking water wells and natural gas wells are in

close proximity is the possibility of water well contamination from surface waters unrelated to

drilling activities. For example, a leaky septic system, or improper disposal of domestic refuse

such as car batteries or used oil, can leak from the surface into the water well. If this is the case, a

dispute could ensue as to who may be responsible for contaminating the water well. Resolving the

dispute could involve a hydrogeological investigation, possibly combined with chemical analysis

or isotopic analysis, to prove or disprove any linkage between natural gas development activities

and water well contamination, often at considerable expense and with an uncertain outcome,

given the complexity of groundwater flow at most sites.

40

The Schlumberger glossary notes that “produced fluid is a generic term used in a number of contexts but most

commonly to describe any fluid produced from a wellbore that is not a treatment fluid. The characteristics and phase

composition of a produced fluid vary and use of the term often implies an inexact or unknown composition.”

“Flowback” refers to “the process of allowing fluids to flow from the well following a treatment, either in preparation

for a subsequent phase of treatment or in preparation for cleanup and returning the well to production.”

41

Henry Trapp Jr. and M. A. Horn, “U.S. Geological Survey Ground Water Atlas of the United States,” HA 730-L

(1997).

42

See New York State, Department of Environmental Conservation, “Primary & Principal Aquifers,”

http://www.dec.ny.gov/lands/36119.html.

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Federal and State Laws and Regulations Affecting

Marcellus Shale Gas Development

Development of natural gas resources in the Marcellus Shale is subject to regulation under several

state and federal environmental laws. In particular, the large volumes of water needed to drill and

hydraulically fracture the shale, and the disposal of this water and other wastewater associated

with gas extraction, may pose significant water quality and quantity challenges that trigger

regulatory attention. USGS noted in a 2009 publication that “concerns about the availability of

water supplies needed for gas production, and questions about wastewater disposal have been

raised by water-resource agencies and citizens through the Marcellus Shale gas development

region.”43 Essentially all permitting, inspection, and enforcement activities related to gas

development are conducted by state agencies. In the cases where federal laws may apply, these

regulatory requirements also are typically administered by the states. The following sections

review key provisions of two relevant federal laws—the Safe Drinking Water Act (SDWA) and

the Clean Water Act (CWA)—and related state requirements.

Surface Water Quality Protection

As previously described, hydraulic fracturing involves injecting water, proppants, and chemicals

into the shale layer at extremely high pressures, which creates fractures that allow natural gas to

flow from the shale. It is a water-intensive practice. Typical Marcellus Shale projects may use 3

million to 5 million gallons of water, although pumped fluid volumes of 7 million to 8 million

gallons are not unusual; 0.5 million pounds of sand or other proppant; and smaller amounts of

chemicals for each well. Furthermore, production sites may have multiple wells. Regarding the

Marcellus Shale region, USGS observed “many regional and local water management agencies

are concerned about where such large volumes of water will be obtained, and what the possible

consequences might be for local water supplies.”44

Some of the injected fluids remain trapped underground, but a portion of the injected water—in

the Marcellus Shale region, roughly 9% to 35%—returns to the surface as “flowback” after the

frac treatment. It typically contains proppant (sand) and chemical residues as well as metals and

trace amounts of naturally occurring radioactive elements that may be present in the water

produced from the geologic formations.45 USGS notes that because the quantity of fluid used is so

large, the additives in a 3 million-gallon frac job would yield about 15,000 gallons of chemicals

in the waste.46 Frac fluid flowback returns to the surface in the first few weeks, although

flowback can continue for several months after gas production has begun but slows over time.

43

Daniel J. Soeder and William M. Kappel, Water Resources and Natural Gas Production from the Marcellus Shale,

U.S. Department of the Interior, Fact Sheet 2009-3032, May 2009, http://pubs.usgs.gov/fs/2009/3032/pdf/FS20093032.pdf. Hereafter, USGS Fact Sheet.

44

USGS Fact Sheet, p. 4.

45

These particles, termed naturally occurring radioactive materials (NORMS), can be brought to the surface on drilling

equipment and in fluids. Subsurface formations may contain low levels of such materials as uranium and thorium and

their daughter products, radium 226 and radium 228. On gamma-ray logs, shales can be differentiated from other rocks

such as clean sandstones and limestones because shales have higher concentrations of potassium-40-bearing minerals.

See Commonwealth of Pennsylvania, Department of Conservation and Natural Resources, Pennsylvania Geology, vol.

38, no. 1 (Spring 2008), p. 5. http://www.dcnr.state.pa.us/topogeo/pub/pageolmag/pdfs/v38n1.pdf.

46

USGS Fact Sheet, p. 4.

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Normally, flowback fluid is stored on-site until it can be disposed of or reused. That is, the well

service company may temporarily retain the flowback in tanks or open-air, lined retention ponds

before reusing it, if possible. Flowback waters from natural gas well drilling activities can

generally be recycled until they reach certain very high concentrations of total dissolved solids

(TDS), at which point the wastewater must be disposed. In the Marcellus Shale region,

wastewater management is particularly of interest in the states where natural gas drilling and

production that uses hydraulic fracturing already occurs—Pennsylvania, West Virginia, and

eastern Ohio—or is expected to begin soon—New York.

Many natural gas operations in the Marcellus Shale region have begun employing on-site

treatment processes to facilitate reuse of the flowback fluids, especially in light of technical and

regulatory constraints to offsite options, discussed below. Several companies have introduced

mobile and fixed treatment units using processes such as evaporation, distillation, oxidation, and

membrane filtration for recycling and reuse. On-site treatment technologies may be capable of

returning 70%-80% of the initial water to potable water standards, thus making the water

immediately available for reuse. The remaining 20%-30% is very brackish and considered brine

water. A portion may be further recoverable as process water, but not to achieve potable water

standards. The economics of any such options are critical, and site factors such as available power

and final water quality are often the determinant in treatment selection. Ultimately, flowback

water and production brine that are not reused require proper disposal, either through

underground injection or treatment and surface discharge.

As described below (“Underground Injection of Shale Gas Wastewater”), produced water from

natural gas extraction may be disposed of through underground injection. Although this disposal

method is commonly used in other shale plays, in some areas across the Marcellus Shale region

(such as northeastern Pennsylvania), the local geology can limit the disposal of wastewater

through underground injection wells. Where underground injection is not feasible, the well

service company may discharge the flowback and other produced water to surface waters if the

discharge does not violate a stream or lake’s water quality standards. Standards established by

states under Section 303 of the Clean Water Act (CWA) protect designated beneficial uses of

surface waters, such as recreation or public water supply.47 But direct discharge of untreated

flowback and formation brine water is rarely possible in the Marcellus Shale region, because of

the chemical additives, naturally occurring contaminants, and salinity found in the wastewater.

Because contaminants present in the flowback broadly prevent discharge to surface water without

further treatment, it is likely that the service company will transfer the wastewater off-site to an

industrial treatment facility or a municipal sewage treatment plant for processing the wastewater.

In this case, the operator of the publicly owned treatment works (POTW) or private centralized

waste treatment (CWT) facility would assume responsibility for treating the waste before

discharging it into nearby receiving water in compliance with effluent limits contained in the

facility’s discharge permit.48

The chemical frac additives returned in flowback and the produced brine could cause operational

problems for POTWs. First, chemical contaminants in industrial process wastewaters can kill the

biota essential to a POTW’s operation. Second, if TDS or other contaminants pass through the

47

33 U.S.C. §1313.

Under CWA Section 301, it is illegal to discharge pollutants into the nation’s waters except in compliance with

substantive and procedural provisions of the law, which include obtaining a discharge permit. 33 U.S.C. §1311.

48

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POTW without adequate treatment, the discharge could violate water quality standards. TDS is an

indicator of salinity, which can be toxic to aquatic organisms. If wastewater is discharged from a

POTW or CWT without adequately removing contaminants, the discharges also may contribute to

impaired drinking water quality for downstream users. In that regard, there is particular concern

for bromides and other salts that comprise TDS, as these chemicals can combine with chlorine in

drinking water treatment processes to potentially form carcinogenic disinfection byproducts

(DBPs).

The potential scale of natural gas drilling and extraction in the Marcellus Shale region has

enormous wastewater management implications, as described by Pennsylvania regulators.49

The Marcellus Shale play has resulted in thousands, and will result in tens of thousands, of

new sources of natural gas drilling wastewaters. Although the industry has shown some

recent success with reduction in volumes of wastewater needing treatment through the

recycling and reuse of flowback and production waters, it is clear that the future wastewater

return flows and treatment needs will be substantial.... This play, estimated to contain as

much as 500 trillion cubic feet of recoverable natural gas, could result in the development of

up to 50,000 new, producing gas wells over the next 20 years.... These wells are anticipated

to produce very highly concentrated TDS wastes (over 300,000 mg/L) continuously over the

course of 20 to 30 years. For example, if these wells produce an average of ten barrels per

week of produced water over their useful lives, a single average well could produce about 27

tons of salt per year (at 300,000 mg/L). Multiply this amount by tens of thousands of

Marcellus gas wells, and the potential pollutional effects from these loadings are tremendous.

Finally, not enough is known at this point about whether Marcellus wells may need to be “refracked” one or more times in the future, thus providing additional uncertainty regarding

treatment and disposal needs for the wastewater.

Conventional POTW technology is largely ineffective at treating flowback and brine from gas

extraction operations in the Marcellus Shale region. POTWs may remove heavy metals, but the

processes employed generally do not actually treat for the very high-TDS concentrations, sulfates,

chlorides, or radionuclides in natural gas drilling wastewater. In particular, the very high

concentrations of TDS will necessitate treatment by evaporation/distillation technology, which is

not typically standard at municipal sewage treatment plants.

Under the Clean Water Act (CWA), regulatory authorities must ensure that permits issued to a

POTW or CWT adequately account for and limit discharges of contaminants that could harm

aquatic life in streams and rivers. If wastewater is transported to a CWT for treatment, subsequent

discharges are subject to EPA-established limitations and standards that are reflected in the

facility’s permit.50 If wastewater is transported to a POTW, the facility’s permit must include

conditions requiring characterization of effluent introduced to the plant, to ensure that

incompatible wastes are not allowed. Throughout the Marcellus Shale region, states are

authorized to implement these provisions of the CWA and to oversee facilities’ compliance with

CWA permits.51

49

Pennsylvania Department of Environmental Quality, “Wastewater Treatment Requirements, 25 PA Code Ch. 95,”

August 21, 2010, http://www.pabulletin.com/secure/data/vol40/40-34/1572.html. Footnotes omitted.

50

These EPA limitations and standards are published in the Code of Federal Regulations at 40 C.F.R. Part 437.

51

For information on applicable CWA requirements, see U.S. Environmental Protection Agency, “Natural Gas Drilling

in the Marcellus Shale, NPDES Program Frequently Asked Questions,” March 16, 2011, http://www.epa.gov/npdes/

pubs/hydrofracturing_faq.pdf.

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EPA also has a continuing oversight role regarding state CWA programs. In Pennsylvania, the

federal agency has accelerated efforts, working with state regulators, to require POTWs and

CWTs that receive fracking wastewater to conduct sampling for radionuclides and to issue CWA

information requests to POTWs and CWTs for compliance determinations and evaluation of the

adequacy of CWA discharge permits. Also, Pennsylvania regulators are working with treatment

facilities and community water systems to monitor for radionuclides, TDS, bromide, chloride, and

other substances of concern.52

In the fall of 2008, water samples from the mid-Monongahela River valley of Pennsylvania

showed high levels of TDS. Although the TDS was determined to pose little threat to health or

safety, it can have a profound environmental impact, particularly by killing microorganisms and

insect larvae essential to healthy ecosystems, such as trout streams. It can also degrade soil if used

for irrigation. Preliminary analysis suggested that the principal source likely was large truck

deliveries of wastewater from gas well drilling sites in the Marcellus Shale to POTWs

discharging, directly or indirectly, into the Monongahela River. At that time, state officials

ordered nine sewage treatment plants to reduce their volumes of gas well drilling water, which

contains high concentrations of TDS. Subsequent analysis concluded that discharge from

abandoned mines was more responsible for the high TDS than drilling wastewater discharges

from municipal wastewater treatment plants.53 However, as indicated by the above quotation,

state officials remain concerned about the projected need for treatment of wastewater (both initial

flowback water from hydraulic fracturing and longer-term production brines) from gas well

development—estimated to be as much as 20 million gallons per day in 2011—and the capacity

of the state’s surface waters to assimilate associated wastewaters.

In 2010, the Pennsylvania Department of Environmental Protection issued new standards for

facilities that accept oil and gas wastewater for treatment. The standards apply to new or

increased discharges from treatment facilities, and set strict discharge limits for TDS, chlorides,

barium, and strontium. The new standards are intended to protect aquatic life by promoting reuse

of water. The goal is to prohibit new and expanding sources of high-TDS wastewater discharge

from the natural gas industry.54 However, 27 Pennsylvania POTWs, which had historically

accepted drilling wastewater, are not bound by the 2010 standards unless they increase the

amount of drilling wastewater that they accept. During 2010 and early 2011, 11 of these

municipal plants voluntarily stopped taking shale gas extraction waste. Both Pennsylvania and

federal regulators took steps in 2011 to end the practice of natural gas companies sending

fracking wastewater to POTWs because of concerns that the facilities are inadequately equipped

to handle waste from fracking operations. In April, state environmental regulators asked drilling

operators to stop sending Marcellus Shale wastewater to the 16 remaining POTWs, citing

evidence linking the wastewater to elevated levels of bromides in western Pennsylvania rivers.55

Subsequently, EPA sent information request letters to six natural gas drillers directing them to

disclose how and where they dispose of or recycle wastewater generated by their Marcellus Shale

natural gas exploration, extraction, and production activities. In response, all six companies

52

For information on these EPA and Pennsylvania activities, see http://www.epa.gov/region03/marcellus_shale/.

“Minimal Impact on Total Dissolved Solids Found in Monongahela River Last Fall,” Natural Gas, Tapping

Pennsylvania’s Potential, May 20, 2009, http://marcelluscoalition.org/category/newsroom.

54

Pennsylvania Department of Environmental Quality, “Wastewater Treatment Requirements, 25 PA Code Ch. 95,”

August 21, 2010, http://www.pabulletin.com/secure/data/vol40/40-34/1572.html.

55

Commonwealth of Pennsylvania, Department of Environmental Protection, “DEP Calls on Natural Gas Drillers to

Stop Giving Treatment Facilities Wastewater,” press release, April 19, 2011.

53

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indicated their intention to employ reuse, disposal through underground injection, and/or

treatment rather than conventional treatment by any of Pennsylvania’s POTWs. The companies

indicated intention to recycle 90% or more of produced water (including flowback) in

Pennsylvania, where injection wells are limited.56 Marcellus Shale operators have stopped

sending wastewater to the state’s POTWs.57

West Virginia, too, recognizes that wastewater disposal is “perhaps the greatest challenge

regarding these operations.”58 State officials say that underground injection (see discussion

below) may be the best option for wastewater disposal, but the state has only two permitted

commercial injection wells available. The state has one industrial wastewater treatment facility in

Wheeling, and state officials are cautious about the capability of the municipal POTWs to handle

the flow and quality of waste that they might receive.59 In 2009 the West Virginia Department of

Environmental Protection proposed changes to the state’s oil and gas drilling rules (which

required approval of the state legislature) and to an industry guidance document to assist

operators in planning for the water issues associated with drilling and operating these wells.

However, local groups criticized the proposed rules and draft non-binding guidance for failing to

address disposal of wastewater, disclosure of chemicals used in hydraulic fracturing, and where

the additional quantities of water required for drilling will come from.60 Subsequently, the state’s

legislature considered a number of bills to implement the proposed rules, and also to make other

changes such as increasing permit fees. In December 2011, the state legislature passed, and the

governor signed, the Horizontal Well Act, which requires drillers to provide water management

plans and to disclose all chemicals used in hydraulic fracturing fluids, among numerous other

provisions intended to protect water supplies.

For several years, New York State regulators have been evaluating the potential environmental

impacts of high-volume hydraulic fracturing in the state. During this time, New York has imposed

a moratorium on processing permits to drill Marcellus Shale wells under the existing Generic

Environmental Impact Statement (SGEIS). (Traditional oil and gas wells still may be permitted

using the SGEIS). In September 2011, the state’s Department of Environmental Conservation

released a Revised Draft Supplemental Generic Environmental Impact Statement (RDSGEIS)

with recommendations that, when finalized, are intended to allow natural gas development

consistent with environmental protection requirements while banning drilling in specified

sensitive areas, including the New York City and Ithaca watersheds.61 Regarding wastewater

56

The six companies—Atlas Resources, Cabot Gas & Oil Corp., Chesapeake Energy; Range Resources-Appalachia,

SWEIP, and Talisman Energy USA—hold more than half of all permits issued for natural gas drilling in Pennsylvania.

EPA’s May 12, 2011, letters to the companies and their responses regarding wastewater management are available at

http://www.epa.gov/region03/marcellus_shale/.

57

Traditional oil and gas well operators may continue to take their produced water to authorized facilities.

58

State of West Virginia, Department of Environmental Protection, Office of Oil and Gas, “Industry Guidance, Gas

Well Drilling/Completion, Large Water Volume Fracture Treatments (Draft),” March 13, 2009, p. 3,

http://www.wvsoro.org/curent_events/marcellus/Marcellus_Guidance_Draft.pdf.

59

Ibid. at 3-4. Reportedly, one company with wells in the Marcellus Shale in West Virginia has its hydraulic fracturing

wastewater trucked to an out-of-state commercial facility that treats the water and then injects it into depleted oil and

gas reservoirs. (P. Kasey, “New Drilling Efforts Raise Questions,” The State Journal, August 14, 2008.)

60

West Virginia Surface Owners’ Rights Organization, “Proposed Changes to Oil & Gas Rules, Marcellus Guidance

Document,” http://www.wvsoro.org/curent_events/.

61

New York State Department of Environmental Conservation, Revised Draft Supplemental Generic Environmental

Impact Statement on the Oil, Gas and Solution Mining Regulatory Program: Well Permit Issuance for Horizontal

Drilling and High-Volume Hydraulic Fracturing to Develop the Marcellus Shale and Other Low-Permeability Gas

Reservoirs, Albany, NY, September 30, 2011, http://www.dec.ny.gov/energy/75370.html.

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management, the revised draft SGEIS would allow POTWs to accept flowback water if the

municipal plant has a state-approved pretreatment program for accepting industrial waste and the

plant’s discharge permit assures that surface water quality standards for TDS and other

contaminants are not violated. Underground injection, discussed below, also may be authorized.

To help POTWs manage produced water, in October 2011, EPA initiated a rulemaking to develop

technology-based standards that shale gas wastewaters must meet before going to a POTW. EPA

expects to issue a proposed rule for shale gas wastewater standards in 2014.62

Other Surface Water Quality Issues

Another potential source of water pollution from oil and gas drilling sites is runoff that occurs

after a rainstorm. Storm water runoff can transport sediment to nearby surface water bodies.

Provisions of the CWA generally regulate storm water discharges from industrial and municipal

facilities by requiring implementation of pollution prevention plans and, in some cases,

remediation or treatment of runoff.63 Industries that manufacture, process, or store raw materials

and that collect or convey storm water associated with those activities are subject to the act’s

requirements. Furthermore, fracking fluid chemicals and wastewater can leak or spill from

injection wells, flow lines, trucks, tanks, or holding pits, and thus may contaminate soil, air, and

water resources.

The federal Clean Water Act (CWA) specifically exempts the oil and gas industry from these

storm water management regulatory provisions. CWA Section 402(l)(2) exempts mining

operations or oil and gas exploration, production, processing, or treatment operations or

transmission facilities from federal storm water regulations, and Section 502(24) extends the

exemption to construction activities, as well.64 Thus, federal law contains no requirements to

minimize uncontaminated sediment pollution from the construction or operation of oil and gas

operations. However, the federal exemption does not hinder states from requiring erosion and

sedimentation controls at well sites, under authority of non-federal law. Pennsylvania, for

example, requires well drill operators to obtain a permit for implementation of erosion and

sedimentation controls, including storm water management, if the site disturbance area is more

than 5 acres in size. If the site is less than 5 acres, a plan for erosion and sediment control is

required. Storm water requirements are part of this permit.65 New York has similar requirements

for erosion and sedimentation controls at well sites, regardless of site area. West Virginia requires

erosion and sediment control plans for proposed well sites that would disturb 3 or more acres of

land.66 The Delaware River Basin Commission, which has jurisdiction over water quality in a

portion of the area underlain by the Marcellus Shale (see section on “State Water Quality Laws”)

has similar requirements, regardless of site area.

62

EPA is developing standards for wastewater discharges produced by natural gas extraction from shale formations and

coal beds. The regulations will be established under EPA’s effluent guidelines program, which sets national regulations

to control the discharge of pollutants from industry to surface waters and to POTWs. Effluent guidelines are specific to

an industry and are established under the authority of CWA §304(m). For more information, see http://water.epa.gov/

lawsregs/lawsguidance/cwa/304m/.

63

Clean Water Act §402(p); 33 U.S.C. §1342(p).

64

33 U.S.C. §1342(l)(2); 33 U.S.C. §1362(24).

65

The Pennsylvania permit is called an Earth Disturbance Permit (ESCGP-1).

66

W. Va. C.S.R. §35-8-3, Department of Environmental Protection Oil and Gas, Rules Governing Horizontal Well

Development, http://www.dep.wv.gov/oil-and-gas/Documents/35-8%20%20%20Horizontal%20Well%20Rule.pdf.

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Groundwater and Drinking Water Protection

A controversial water quality issue associated with development of the Marcellus Shale regards

the potential for hydraulic fracturing operations to contaminate groundwater and drinking water

wells (as discussed under “Potential Risks to Groundwater”). Responding to widespread public

concern, the 111th Congress urged EPA to study the impact that fracturing may have on potable

aquifers and drinking water supplies.67 However, EPA is not authorized to regulate the

underground injection of fluids for hydraulic fracturing purposes, except where diesel fuel is

used.68 The agency expects to publish initial research results in 2012, and a final report in 2014.

As part of the research, EPA has identified three Marcellus Shale case studies in Pennsylvania:

two retrospective case studies to investigate drinking water contamination incidents, and one

prospective study where shale gas development is planned.69

A question that has arisen is whether state oil and gas laws and regulations are adequate to protect

groundwater and drinking water wells, given the increasingly extensive development of

unconventional gas and oil resources that rely on hydraulic fracturing in combination with deep

vertical and horizontal drilling. The deep horizontal wells used in unconventional oil and gas

development can be subjected to greater pressures than conventional wells and may be at greater

risk of failure if not properly constructed and operated.

In 2009, the Ground Water Protection Council (GWPC)70 reviewed state oil and gas regulations

designed to protect water resources for the major producing states.71 The GWPC concluded that,

in general, state oil and gas regulations are adequately designed to protect water resources. State

regulations generally include permitting, well drilling and construction, well closure and

abandonment, and waste fluid management. Until recently, few states explicitly mentioned

hydraulic fracturing in their oil and gas regulations; however, drilling, construction (e.g., casing

and cementing), pressure testing, completion, blowout prevention, reporting, and other

requirements are intended to protect fresh water aquifers (and hydrocarbon resources) during oil

and gas production.

67

P.L. 111-88, H.Rept. 111-316.

The Energy Policy Act (EPAct) of 2005 (P.L. 109-58, §322) amended the SDWA to exempt from the definition of

underground injection the injection of fluids or propping agents (other than diesel fuel) for hydraulic fracturing

purposes. For a history of this provision, and the EPA underground injection control program and its role in regulating

hydraulic fracturing, see CRS Report R41760, Hydraulic Fracturing and Safe Drinking Water Act Issues, by (name

redacted) and (name redacted).

69

EPA has selected seven sites for case studies to develop information about the potential impacts of hydraulic

fracturing on drinking water resources under different circumstances. Two sites are prospective case studies where EPA

will monitor aspects of the hydraulic fracturing process at future development sites (i.e., the Haynesville Shale in

DeSoto Parish (LA), and the Marcellus Shale in Washington County (PA). Five retrospective studies will investigate

reported drinking water contamination attributed to hydraulic fracturing operations at gas production sites (i.e., the

Bakken Shale in Kildeer, Dunn County (ND); the Barnett Shale in Wise County (TX); the Marcellus Shale in Bradford

and Susquehanna Counties (PA); the Marcellus Shale in Washington County (PA); and the Raton Basin (CO)). For

information on the EPA hydraulic fracturing study, see the agency’s hydraulic fracturing website, http://water.epa.gov/

type/groundwater/uic/class2/hydraulicfracturing/. The final study plan is available at http://www.epa.gov/hfstudy/

HF_Study__Plan_110211_FINAL_508.pdf.

70

The Ground Water Protection Council is a professional association of state groundwater and underground injection

control agencies responsible for groundwater protection.

71

GWPC, DOE, Office of Fossil Energy, National Energy Technology Laboratory, State Oil and Natural Gas

Regulations Designed to Protect Water Resources, May 2009.

68

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Although major oil and gas producing states have extensive programs to manage oil and gas

development activities, the GWPC noted that related state groundwater protection rules and

practices can be uneven. Among other actions, the Council recommended the development of best

management practices (BMPs) for hydraulic fracturing, which state agencies could use either to

develop state-specific BMPs or develop new state regulations. GWPC advised states to review

rules to determine whether “they meet an appropriate level of specificity (e.g. use of standard

cements, plugging materials, pit liners, siting criteria, and tank construction standards, etc.)” to

protect water resources.72

In a groundwater contamination case in Pennsylvania, Department of Environmental Protection

officials attributed the migration of methane gas into 18 residential water wells in Dimock, PA, to

“defective casing and cementing” of shale gas wells.73 The state since has updated oil and gas

rules. The regulators explained the need for the revised regulations.74

Many of the regulations governing well construction and water supply replacement were

promulgated in July 1989 and remained largely unchanged until this final-form rulemaking.

Since that time, recent advances in drilling technology have attracted interest in producing

natural gas from the Marcellus Shale, a rock formation that underlies approximately 2/3 of

this Commonwealth. New well drilling and completion practices now employed to extract

natural gas from the Marcellus Shale and other similar shale formations in this

Commonwealth, as well as several recent incidents of contaminated drinking water caused

by traditional and Marcellus Shale wells resulted in the Department’s decision to reevaluate

the existing well construction requirements.

It was determined that the existing regulations were not specific enough in detailing the

Department’s expectations of a properly cased and cemented well, especially in light of the

new techniques used by Marcellus Shale operators. The Department also determined that the

existing regulations did not address the need for an immediate response by operators to a gas

migration complaint and did not require routine inspection of existing wells by the operator.

The final-form rulemaking contains revised design, construction, operational, monitoring,

plugging, water supply replacement and hydraulic fracturing reporting requirements. The

final-form rulemaking also provides material specifications and performance testing to

ensure the proper casing, cementing and operation of a well. Additionally, the final-form

rulemaking contains new provisions that require routine inspection of wells and outline the

actions an operator and the Department will take in the event of a gas migration incident.

Other states in the region also have amended or are revising regulations to address challenges

related to unconventional oil and gas development, including hydraulic fracturing. In 2010, Ohio

legislators made major revisions to the state oil and gas law, adding requirements for companies

to submit hydraulic fracturing records, and to report the type and volume of materials used,

pumping pressures, and return volumes.75 The law also expanded well construction, casing, and

72

Ibid, pp. 39-40.

See Pennsylvania Department of Environmental Protection website, http://www.dep.state.pa.us/dep/DEPUTATE/

MINRES/OILGAS/Final%20COA%20121510.pdf. For further information on this complex matter, see

http://www.cabotog.com/pdfs/Letter_Sec_Hanger.pdf. For a review of non-routine incidents in Pennsylvania involving

development of the Marcellus Shale, see http://www.dec.ny.gov/docs/materials_minerals_pdf/rdsgeisch100911.pdf.

74

In February 2011, the Pennsylvania Environmental Quality Board published notice of final oil and gas well

regulations to prevent gas migration incidents, 25 PA. Code Ch. 78, http://www.pabulletin.com/secure/data/vol41/41-6/

239.html.

75

For information on Ohio’s environmental regulations on drilling for natural gas in the Marcellus and Utica shales,

(continued...)

73

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cementing requirements to protect underground sources of drinking water.76 And, as discussed,

New York State has undergone a comprehensive review of the issues associated with shale-gas

development, and is developing a new regulatory regime for horizontal drilling and high-volume

hydraulic fracturing.

In December 2011, West Virginia enacted the Horizontal Well Act, which makes numerous

changes to existing law.77 The act imposes new conditions on horizontal well permits to protect

groundwater, surface water, and water resource supplies. (See section below, “State Regulation of

Water Resources.”) The act requires well operators to provide state regulators with well-casing

plans, details on the rock formation, and drilling-depth plans. Additionally, the law increases

permit fees to support more state inspectors. Among other provisions, the law specifies minimum

distances horizontal wells must be from water wells, public water supplies, streams, wetlands, etc.

As noted, managing the large volumes of wastewater produced during natural gas production

(including flowback from hydraulic fracturing and brine produced from the rock formation) has

emerged as a major water quality issue related to Marcellus Shale development. In some areas

across the Marcellus Shale region (such as northeastern Pennsylvania), the local geology can limit

the disposal of wastewater through underground injection wells. However, underground injection

remains the most common—and traditionally preferred—produced water disposal practice in the

oil and gas production industry, and is increasing in this region as gas development expands.

The increased use of underground injection for wastewater disposal, combined with proposals to

authorize EPA to regulate hydraulic fracturing as underground injection, has drawn new attention

to the federal underground injection control program. This program’s statutory and regulatory

framework is reviewed briefly below.78

Federal Underground Injection Control Program

The disposal of flowback and other water produced from gas wells through deep well injection is

regulated through EPA’s Underground Injection Control (UIC) program authorized by the federal

Safe Drinking Water Act (SDWA).79 This act established the national program for protecting

“underground sources of drinking water” by limiting, through regulation, underground injection

that could contaminate usable aquifers. Although the SDWA excludes from regulation the

(...continued)

see http://www.epa.ohio.gov/shale.aspx.

76

SB 165, Ohio Department of Natural Resources, Division of Mineral Resources Management, Oil and Gas, June 30,

2010. For information on the law and rules, see http://www.ohiodnr.com/oil/SB165updates/tabid/22848/Default.aspx.

Additionally, Ohio and Pennsylvania recently had their oil and gas regulatory programs reviewed under State Review

of Oil and Natural Gas Environmental Regulations (STRONGER), to evaluate the adequacy of their hydraulic

fracturing requirements. STRONGER is a state program review process, conducted by a multi-stakeholder, national

nonprofit group. State hydraulic fracturing reviews are available at http://www.strongerinc.org/.

77

H.B. 401, 80th Leg., 4th Spec. Sess. (W. Va. 2011).

78

For a discussion of EPA’s UIC program and its role in oil and gas production and hydraulic fracturing activities, see

CRS Report R41760, Hydraulic Fracturing and Safe Drinking Water Act Issues, by (name redacted) and (name redacted).

79

The Safe Drinking Water Act of 1974 (P.L. 93-523) authorized the UIC program at EPA. UIC provisions, as

amended, are contained in SDWA Part C, §§1421 - 1426; 42 U.S.C. §§300h - 300h-5.

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underground injection of fluids used in hydraulic fracturing (unless diesel fuel is used), the

injection of wastewater produced during oil and gas development is subject to this law.80

Section 1421 of SWDA directs the EPA administrator to issue regulations for state UIC programs,

and mandates that the EPA rules “contain minimum requirements for programs to prevent

underground injection that endangers drinking water sources.”81 To implement the UIC program,

EPA has established six classes of underground injection wells based on categories of materials

that are injected into the ground for each class. The wells within a class are required to meet a set

of performance criteria for protecting underground sources of drinking water (USDW), and the

rules broadly prohibit the injection of waste fluids into USDWs. The UIC regulations for each

class include the following broad elements: site characterization, area of review, well

construction, well operation, site monitoring, well plugging and post-injection site care, public

participation, and financial responsibility.82 Class II injection wells are used to dispose of brines

(salt water) and other fluids associated with oil and gas production or storage, to store natural gas,

or to inject fluids for enhanced oil and gas recovery.83

The SDWA authorizes EPA to delegate primary enforcement authority (primacy) for UIC

programs to the states, provided that the state program meets EPA regulations developed under

Section 1421 and prohibits underground injection that is not authorized by a state permit or rule.84

If a state’s UIC program plan is not approved, or the state has chosen not to assume program

primacy, then EPA must implement the UIC program in that state. However, in lieu of meeting the

specific requirements of EPA’s regulations for the injection of brine or other fluids brought to the

surface in connection with oil or gas production (Class II injection wells), Section 1425 allows

states to demonstrate that their Class II UIC programs are effective in preventing endangerment

of underground sources of drinking water.85 This gives states flexibility to implement their own

program requirements, rather than meet the specific EPA regulations.

Where a state has primacy, EPA is still required to take enforcement actions for regulatory

violations if the state fails to do so.86 Additionally, the SDWA grants the EPA administrator

80

EPAct 2005 (P.L. 109-58, §322) amended the SDWA to exempt from the definition of underground injection the

injection of fluids or propping agents (other than diesel fuel) for hydraulic fracturing purposes (42 U.S.C. §300h(d)).

EPA retains the authority to regulate the use of diesel fuel for the purpose of hydraulic fracturing, and the agency is

developing guidance to help states implement this provision. EPA’s website notes that “any service company that

performs hydraulic fracturing using diesel fuel must receive prior authorization from the UIC program,” and that

“injection wells receiving diesel fuel as a hydraulic fracturing additive will be considered Class II wells by the UIC

program.” See http://water.epa.gov/type/groundwater/uic/class2/hydraulicfracturing/wells_hydroreg.cfm#safehyfr.

81

42 U.S.C. §300h(b).

82

Regulatory requirements for state UIC programs are established in 40 C.F.R. §§144-147.

83

EPA historically has differentiated Class II wells from production wells. The agency’s UIC website states that

“production wells bring oil and gas to the surface; the UIC Program did not regulate production wells.” EPA, Class II

Wells—Oil and Gas Related Injection Wells (Class II), “What are the types of Class II wells?,” http://water.epa.gov/

type/groundwater/uic/class2/index.cfm.

84

42 U.S.C. §300h-1. The minimum requirements for a state UIC program can be found at 40 C.F.R. Part 145. To

receive primacy, a state must demonstrate to EPA that its UIC program is at least as stringent as the federal standards;

the state requirements may be more stringent than the federal requirements. For Class II wells, states must demonstrate

that their programs are effective in preventing endangerment of underground sources of drinking water (USDWs).

85

42 U.S.C. §300h-4 (SDWA §1425). To receive approval under §1425 optional demonstration provisions, a state

program must include permitting, inspection, monitoring, and record-keeping and reporting requirements.

86

42 U.S.C. §300h-2 (SDWA §1423).

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emergency powers to issue orders and commence civil actions to protect public water systems or

underground sources of drinking water.87

In the Marcellus region, Maryland, Ohio, and West Virginia have assumed primacy and have lead

implementation and enforcement authority for their UIC programs. As with most oil and gas

producing states, Ohio and West Virginia have received primacy for Class II wells under Section

1425, which enables these states to administer their own equivalent program, rather than adopt

EPA regulations. Maryland has adopted EPA regulations, but has no Class II injection wells for

the disposal of wastewater from oil and gas production.88 In New York, Pennsylvania, and

Virginia, EPA directly implements the entire UIC program. Permits are required both by EPA and

the state environmental agency in New York and Pennsylvania, if the disposal method for shale

gas wastewater is by deep well injection.

Underground Injection of Shale Gas Wastewater

Most of the fluid injected into Class II wells is brine brought to the surface in producing oil and

gas. This brine, a naturally occurring formation fluid, is often very saline and may contain toxic

metals and naturally occurring radioactive substances. To prevent contamination of land, surface

water, and groundwater, Class II wells provide a means for disposing of brines by re-injecting

them back into their source formation or into similar formations at significant depths. As states

have adopted rules to limit or prohibit the disposal of saline water to surface water and land, and

treatment remains challenging and costly, injection remains the preferred way to dispose of this

waste fluid, where the local geology permits.

The amount of water produced by shale gas wells, separate from the flowback of water injected

for hydraulic fracturing purposes, is likely to vary across the Marcellus Shale region. Given the

limited experience with development of the shale, it is uncertain how much produced water might

be generated. Generally speaking, shale gas formations are relatively impermeable and typically

produce much less water than traditional oil and gas fields or coalfields. However, because large

amounts of water must be used to fracture the shale, the disposal of this water and produced brine

presents a challenge. Moreover, the impermeability of the shale indicates that reinjection of

wastewater from fracturing into the shale formation may not be feasible in many locations, unless

other suitable formations are locally available.

Wastewater injection into the permeable Cambrian sandstones that lay beneath the Marcellus

Shale appears feasible. The Cambrian Mt. Simon Sandstone, considered an ideal geologic unit in

Ohio for disposal and long-term storage of liquid wastes, is relatively deep, and underlain and

overlain by impervious confining layers that prevent migration of injected fluids.89 In contrast, the

geology in Northeastern Pennsylvania is not favorable for injection.

87

42 U.S.C. §300i (SDWA §1431) authorizes the administrator to take action when information is received that (1) a

contaminant is present in or is likely to enter a public drinking water supply system or underground source of drinking

water “which may present an imminent and substantial endangerment to the health of persons,” and (2) the appropriate

state or local officials have not taken adequate action to protect such persons.

88

EPA, 2010 UIC Well Inventory, Office of Water, 2010, http://water.epa.gov/type/groundwater/uic/.

89

Ohio Department of Natural Resources, Division of Geological Survey, The Geology of Ohio—The Cambrian,

GeoFacts No. 20, May 1998.

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Capacity for deep well injection of wastewater varies across the Marcellus region. In Ohio, oil

and gas permits generally prohibit the discharge of brine directly into state waters, and roughly

98% of all brine is disposed of by deep well injection.90 The Ohio Department of Natural

Resources has permitted 184 Class II brine disposal wells, and permit requests for additional

wells are pending. Since Marcellus Shale gas development began in West Virginia, the number of

permitted commercial Class II disposal wells there has increased from two to 13. New York has

six active Class II disposal wells; however, before New York stopped processing permits for

horizontal drilling and high-volume hydraulic fracturing in 2008, operators from one company

had submitted more than 60 permit applications for such wells.91 In Pennsylvania, six Class II

disposal wells are operating, and EPA (which implements the UIC program for the state) has

approved two more wells, but these permits are under appeal. However, since the state has limited

surface water discharges, interest in deep well injection within the commonwealth is increasing.

Emerging Issue: Deep Well Injection and Seismic Events

In recent months, several small earthquakes have occurred in eastern Ohio in the vicinity of injection wells used to

dispose of brine and other wastewater produced from oil and gas wells. No causal link has been established between

the wastewater injection and these seismic events, but state officials have had operators shut-in the nearby wells

while the events are investigated. Past incidents of induced seismicity have been identified: in 1967, the injection of

wastes at the Rocky Mountain Arsenal was halted once fluid injection was linked to a series of earthquakes. In 1990,

the U.S. Geological Survey (USGS) reported that,

of the well-documented cases of earthquakes related to fluid injection, most are associated with

water-flooding operations for the purpose of secondary recovery of hydrocarbons… [The]

operations often entail large arrays of wells injecting fluids at high pressures into small confined

reservoirs that have low permeabilities. In contrast, waste-disposal wells typically inject at lower

pressures into large porous aquifers that have high permeabilities. This explains, in large part, why, of

the many hazardous and nonhazardous waste-disposal wells in the United States, only two have ever

been conclusively shown to be associated with triggering significant adjacent seismicity. (The wells are

near Denver, CO, and Ashtabula, OH.)92

Currently, EPA and USGS are evaluating several case studies of possible induced seismicity. The forthcoming report

will include lessons learned and make recommendations to assist states in regulating injection well operations.

State Water Quality Laws

In addition to federal laws, state laws addressing the quality of surface water and groundwater

also apply to Marcellus Shale development. For example, in New York, various aspects of

unconventional gas development would require a permit under the state’s State Pollutant

Discharge Elimination System (SPDES).93 SPDES is an “approved,” rather than delegated,

version of the federal National Pollutant Discharge Elimination System (NPDES) permit program

under the Clean Water Act, which means that the state program differs from the federal rules in

various ways, but that EPA has determined that the state program is at least as protective as

federal rules. One significant difference in the state program is that, while the federal NPDES

90

Ohio Department of Natural Resources, Division of Oil and gas Resources Management, Underground Injection

Control (UIC), http://www.ohiodnr.com/mineral/injection/tabid/10374/Default.aspx.

91

J. Daniel Arthur, et al, Evaluating the Environmental Implications of Hydraulic Fracturing in Shale Gas Reservoirs,

2008, available at http://www.all-llc.com.

92

Craig Nicholson and Robert L. Wesson, USGS Bulletin 1951, U.S. Geological Survey, Earthquake Hazard

Associated with Deep Well Injection - A Report to the U.S. Environmental Protection Agency, 1990.

93

N.Y. Envtl. Cons. Law §17-0505.

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covers only discharges to surface water, SPDES covers discharges to groundwater also. The

SPDES permit requirement could apply to hydraulic fracturing, unless four conditions are met.

Most importantly, the state must determine that injection will not degrade groundwater.94 A

wastewater treatment plant would likely dispose of fluids produced from the well, in which case

the plant’s SPDES permit would apply. SPDES permits would also cover treatment facilities built

specially for disposing of flowback water, if there would be discharges into a water body.

Applicable state water quality standards would control the permit’s discharge limits, in part.95

The New York State Environmental Quality Review Act (SEQRA) is also relevant.96 As with its

federal counterpart, the National Environmental Policy Act, a requirement that an environmental

impact statement be prepared in certain circumstances lies at the heart of the statute.97 New York

has been evaluating the potential environmental impacts associated with directional drilling and

hydraulic fracturing activities for more than 15 years. As noted above, in September 2011, the

state’s New York Department of Environmental Conservation (DEC) released for public comment

the Revised Draft Supplemental Generic Environmental Impact Statement (RDSGEIS) under

SEQRA on high-volume hydraulic fracturing natural gas development in the Marcellus Shale

region of the state with recommendations to comprehensively revise the state’s procedures for

regulating operations using High Volume Hydraulic Fracturing (HVHF). Until New York

completes a final SGEIS consistent with SEQRA, regulators will not process permit applications

for gas wells involving horizontal drilling and high-volume hydraulic fracturing.98 The DEC

received more than 32,000 comments on the revised draft and is now reviewing them.

The RDSGEIS would not apply to specified areas, including within the New York City and

Syracuse watersheds, on primary aquifers, on certain state lands, in floodplains, within 2,000 feet

of public drinking water supplies, and within 500 feet of private water wells (unless agreed to by

the landowner). Nor would the RDSGEIS apply to HVHF operations in shallow portions of shale

formations, specifically in locations where the top of the target fracture zone would be shallower

than 2,000 feet below the surface, or less than 1,000 feet below the base of a known fresh water

supply. In these locations, site-specific environmental assessments and SEQRA determinations of

significance would be required for HVHF permit applications. (Figure 6 indicates specific

geographic areas where drilling permits would not be granted under the RDSGEIS and, in effect,

prohibited.) The DEC also has proposed regulations that revise existing oil and gas regulations,

establish new regulations for HVHF, and update the SPDES regulations.

94

N.Y. Code of Rules and Regulations (Conservation) §750-1.5(a)(6).

N.Y. Envtl. Cons. Law §17-0501.

96

N.Y. Envtl. Cons. Law §§8-0101–8-0117.

97

Id. at §8-0109.

98

David A. Paterson, Governor, New York, “Executive Order No. 41: Requiring Further Environmental Review,”

December 10, 2010, http://www.dec.ny.gov/energy/46288.html#41. The September 2011 Revised Draft SGEIS is

available at http://www.dec.ny.gov/energy/75370.html.

95

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Figure 6. New York State Areas Where Shale Development Is to Be Prohibited

(NYC and Syracuse watersheds, primary aquifers, and state lands)

Source: New York Department of Environmental Conservation, http://www.dec.ny.gov/energy/75370.html.

Note: The Draft Revised Supplemental Generic EIS also establishes setbacks from public water supplies and

private wells and contains other high-volume hydraulic fracturing drilling restrictions.

Maryland, too, currently is not processing permit applications for drilling and hydraulic fracturing

in the state’s portion of the Marcellus Shale (although several permits are pending). Officials plan

to study “best practice” standards for drilling and fracking before permitting a small number of

exploratory wells to evaluate the environmental viability of gas production.99

In Pennsylvania, oil and gas exploration and development are regulated under a number of state

laws, including the Clean Streams Law, the Solid Waste Management Act, and the Water

Resources Planning Act. For example, pursuant to the Clean Streams Law,100 Pennsylvania

regulates waste discharges from municipal and industrial sources and regulates the impact of

mining on water quality, supply, and quantity. It also is the basis for state permit requirements to

99

Robert M. Summers, Acting Secretary of the Maryland Department of the Environment, Testimony before the U.S.

Congress, Senate Committee on Environment and Public Works, Subcommittee on Water and Wildlife, “Hydraulic

Fracturing in the Marcellus Shale and Water Quality,” April 12, 2011.

100

35 P.S. §691.1 et seq.

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manage stormwater runoff from oil and gas operations through erosion and sediment control

plans. (See “Other Surface Water Quality Issues.”)

As another example, West Virginia’s NPDES permit program would apply to wastewater

treatment plants to which flowback from Marcellus Shale production sites was taken and to

treatment facilities built specially for the frac water that discharges into a water body.101

Applicable state water-quality standards would control the permit’s discharge limits, in part.102

However, this program applies to surface water only, not groundwater, and the state’s

Groundwater Protection Act exempts “groundwater within geologic formations which are site

specific to ... the production ... of ... natural gas....”103 The state’s underground injection control

program regulates the injection of flowback and produced water for disposal.104

In addition to state water-quality laws, the interstate Delaware River Basin Commission (36% of

whose jurisdictional land area in Pennsylvania and New York overlies the Marcellus Shale

formation) would also impose water quality requirements.105 The Commission’s water quality

(and other) requirements are legally separate from those of the affected states—that is, obtaining

state approval does not excuse an applicant from seeking Commission approval—although in

some cases the two requirements may be substantively identical. Another interstate-compactcreated commission within the Marcellus Shale region, the Susquehanna River Basin

Commission, regulates only water quantity, not water quality.106 These commissions are discussed

further below.

Water Supply Management

Thousands of wells are being drilled in the Marcellus Shale region, and large volumes of water

are needed to develop each well. Roughly 1 million gallons typically may be needed for every

1,000 feet fractured in the horizontal portion of a well, for perhaps 3 million to 8 million gallons

per well, and wells may need to be hydraulically fractured several times during their productive

lifespan.

Availability of adequate supplies of fresh water required for drilling and hydraulic fracturing can

be a constraint for gas producers who must arrange to procure water in advance of their drilling

and development activity. Extensive development of the Marcellus Shale could place short-term,

but potentially significant, demands on local water resources. This is especially true if water

needed for gas development is taken from smaller headwater streams or limited groundwater

101

W. Va. Code Ann. §22-11-4(a)(16). See regulations at W. Va. Code of State Rules, Tit. 47, ser. 10.

W. Va. Code of State Rules tit. 47, ser. 2.

103

W. Va. Code Ann. §22-12-5(i).

104

W. Va. Code Ann. §22-11-8(b)(7). See regulations at W. Va. Code of State Rules tit. 47, ser. 13.

105

The compact creating the Delaware River Basin Commission was ratified by Congress: P.L. 87-328, 75 Stat. 688.

Section 3.8 of the Compact states: “No project having a substantial effect on the water resources of the basin shall

hereafter be undertaken by any person, corporation, or government authority unless it shall have been first submitted to

and approved by the commission....” Section 2.3.5 B of the Delaware River Basin Comm’n Administrative Manual

(Rules of Practice and Procedure) lists 18 types of projects that must be submitted to the Commission, including

withdrawal of groundwater and discharge of pollutants into surface or ground waters of the basin. Codified at 18 C.F.R.

§401.35(b).

106

The compact creating the Susquehanna River Basin Commission was ratified by Congress: P.L. 91-575, 84 Stat.

1509 (1970).

102

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supplies. In these cases, large water withdrawals have the potential to impair water quality

through diminished stream flows that could affect aquatic life, fishing and recreational activities,

or private wells and water supplies. Concerns have arisen specifically regarding the ability to

maintain baseline stream flows to avoid cumulative and seasonal impacts. Management of water

use for Marcellus Shale operations is largely a matter of geography—in some areas, it is the

responsibility of interstate commissions, and in other areas, it is the responsibility of state

agencies.

State Regulation of Water Resources

The laws and regulations governing the availability of fresh water lie with each state, and water

rights and water supply regulations generally differ among the states. Depending on individual

state resources and historic development, states may use one of two water rights doctrines,

riparian or prior appropriation, or a hybrid of the two. Under the riparian doctrine, a person who

owns land that borders a watercourse has the right to make reasonable use of the water on that

land.107 Traditionally, the only limit to users under the riparian system is the requirement of

reasonableness in comparison to other users.108 Under the prior appropriation doctrine, a person

who diverts water from a watercourse (regardless of his location relative thereto) and makes

reasonable and beneficial use of the water may acquire a right to use of the water.109

States east of the Mississippi River generally follow a riparian doctrine of water rights, while

western states typically follow the prior appropriation doctrine.110 The system of water rights

allocation in a particular state with shale gas resources may affect the development process,

particularly in times when shortages in water supply affect the area of shale gas development. In

areas where the Marcellus Shale is located, which are generally riparian states, water rights may

not be as much of a concern as in other areas of the country with shale gas development, such as

the Barnett Shale in Texas. That is, even in times of shortage, shale gas development may be able

to continue in the Marcellus Shale region because riparian users reduce water usage

proportionally and may still receive enough for supply requirements of the development process.

However, whether the amount of water required for hydraulic fracturing processes would be

considered “reasonable” remains unclear. As shale gas development continues to draw on water

resources in riparian states, this question may become a significant factor in the public debate

over hydraulic fracturing.

Because of the general recognition of the riparian doctrine in the region, the states in the area of

shale development apply surface and groundwater regulations similarly. Some states have specific

regulatory programs in place, however, and gas producers using fresh water for drilling and

107

See generally A. Dan Tarlock, “Law of Water Rights and Resources, ch. 3,” Common Law of Riparian Rights.

Id. at §3:12.

109

See generally id. at ch. 5, “Prior Appropriation Doctrine.” The prior appropriation system limits users to the

quantified amount of water the user secured under a state permitting process with a priority based on the date the state

conferred the water right. Because of this priority system, the phrase “first in time, first in right” has sometimes

substituted for appropriative rights. Some states have implemented a dual system of water rights, assigning rights under

both doctrines.

110

The distinction between these doctrines arises primarily from the historic availability of water geographically. In the

generally wetter, eastern riparian states, water users share the water resources because water availability historically did

not pose a problem to settlement and development. In the drier, western states that experience regular water shortages,

the prior appropriation system provides a definitive hierarchy that allows users to acquire well-defined rights to water

as a limited resource that requires planning to avoid scarcity.

108

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development must comply with state and local administration of water rights (as well as any

relevant interstate water compacts). Examples of water supply regulations in the Marcellus Shale

states are discussed below, but a comprehensive analysis of state water regulation schemes is

beyond the scope of this report.

Some states have implemented permit programs that require certain water users who wish to

withdraw large amounts of water resources to register with the appropriate state agency. For

example, New York requires users of water for public water supply, irrigation, and specific

projects designated by law (unrelated to shale development) to acquire a permit.111 However,

under that program, water users pursuing shale development appear to remain unregulated. Other

states have adopted permit programs that require water users who withdraw in excess of a set

threshold (e.g., 10,000 gallons per day) to obtain approval from the state.112

Other states have undertaken various planning and reporting programs to monitor water use in the

state, but do not generally require a permit.113 For example, by statute, West Virginia requires

certain users of water resources whose withdrawals exceed 750,000 gallons in any month to

register with the Department of Environmental Protection.114 Water users must provide

information about the sources of withdrawals, anticipated volumes, and the time of year of

withdrawals.115 The goal is to ensure that water withdrawal from ground or surface waters does

not exceed sustainable volumes.116 State officials have introduced measures that would impose a

lower threshold for registration on the use of water in gas development projects.117 In 2011, West

Virginia enacted the Natural Gas Horizontal Wells Control Act, which mandates that certain

horizontal well applications used for fracturing include a water management plan.118 The water

management plan is required for applications for a well work permit if the fracturing of the well

requires more than 210,000 gallons of water during any 30-day period.119 The plan must identify

information about the use of water, including the type of water source, and the anticipated volume

and time of withdrawal.120

States may implement a variety of these programs concurrently. For example, Pennsylvania

implements both a permit program and a planning and reporting program, in addition to specific

requirements imposed on drillers to include water use management plans with applications for

drilling permits. Under the permit program, public water supply agencies must receive approval

from the state’s Department of Environmental Protection.121 Other users do not appear to be

covered by a permit program outside of the Susquehanna and Delaware River Basins. Under the

111

N.Y. Envtl. Conserv. Law §15-1501.

See 9 Va. Admin. Code §25-210-60.B; 401 Ky. Admin. Regs. 4:010.

113

See 27 Pa.C.S. §3101 et seq.

114

W. Va. Code Ann. §22-26-3.

115

State of West Virginia, Department of Environmental Protection, Office of Oil and Gas, “Industry Guidance, Gas

Well Drilling/Completion, Large Water Volume Fracture Treatments,” January 8, 2010, http://www.dep.wv.gov/oiland-gas/GI/Documents/Marcellus%20Guidance%201-8-10%20Final.pdf.

116

Id.

117

See also W. Va. S.B. 424 (introduced February 4, 2011), http://www.legis.state.wv.us/bill_status/bills_text.cfm?

billdoc=sb424%20intr.htm&yr=2011&sesstype=RS&i=424.

118

H.B. 401, 80th Leg., 4th Spec. Sess. (W. Va. 2011).

119

Id. at §22-6A-7(e).

120

Id.

121

32 Pa. Stat. Ann. §636.

112

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reporting program, users must report withdrawals that on average exceed 10,000 gallons per day

in a 30-day period.122 Users are required to report information including source of water supply,

location, and the amount of withdrawals.123 Additionally, Marcellus Shale drillers must develop

and submit a water use management plan, which, once approved, becomes a condition of a shale

well permit.124

Interstate Compacts in the Marcellus Shale Region

The Marcellus Shale region includes parts of Kentucky, Maryland, New York, Ohio,

Pennsylvania, Virginia, and West Virginia.125 Several of these states include watersheds that are

subject to specific regulations, usually resulting from the adoption of an interstate compact. Three

interstate compacts may have a direct impact on potential water resources for the development

process: the Delaware River Basin Compact, the Susquehanna River Basin Compact, and the

Great Lakes-St. Lawrence River Basin Water Resources Compact.

The Delaware River Basin Commission (DRBC) governs water resource issues in the Delaware

River Basin, which includes parts of Delaware, New Jersey, New York, and Pennsylvania.126 The

Susquehanna River Basin Commission (SRBC) governs water resource issues in the Susquehanna

River Basin, which includes parts of Maryland, New York, and Pennsylvania.127 (See Figure 7.)

Both the DRBC and the SRBC regulate water use through requirements imposed on any entity—

public or private—whose use would affect the respective basins.

The Great Lakes-St. Lawrence River Basin Water Resources Compact governs management of

the Great Lakes and St. Lawrence River Basin, which includes parts of Illinois, Indiana,

Michigan, Minnesota, New York, Ohio, Pennsylvania, and Wisconsin.128 This basin overlies a

small portion of the Marcellus Shale, but includes other shale formations, including the Utica

Shale. The Great Lakes-St. Lawrence compact imposes requirements on the states (as parties to

the compact) to adopt standards of regulation for water use within the basin. Rules governing

these compacts have increasingly included requirements to regulate the water use of hydraulic

fracturing projects.

122

See 27 Pa. Cons. Stat. Ann. §3118.

Id.

124

The Pennsylvania Department of Environmental Protection has issued detailed instructions on how to complete a

water management plan, which is available at http://www.dep.state.pa.us/dep/deputate/minres/oilgas/new_forms/

marcellus/marcellus.htm.

125

See USGS, Assessment of Undiscovered Oil and Gas Resources of the Devonian Marcellus Shale of the

Appalachian Basin Province, August 2011, http://pubs.usgs.gov/fs/2011/3092/pdf/fs2011-3092.pdf.

126

P.L. 87-328, 75 Stat. 688 (1961).

127

P.L. 91-575, 84 Stat. 1509 (1970).

128

P.L. 110-342, 122 Stat. 3739 (2008).

123

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Figure 7. Major River Basins and Sub-Basins Overlying the Marcellus Shale

Source: J.D. Arthur, M. Uretsky, and P. Wilson (ALL Consulting). “Water Resources and Use for Hydraulic

Fracturing in the Marcellus Shale Region.” Prepared in conjunction with the New York State Energy Research

and Development Authority, Susquehanna River Basin Commission, and the Delaware River Basin Commission

and others under U.S. Department of Energy Research Project DE-FE0000797.

Note: The Great Lakes-Saint Lawrence River Basin overlaps with the north edges of the Marcellus region.

The DRBC imposes limits on projects that have “a substantial effect on the water resources of the

basin” and requires that any person or entity seeking to undertake such a project obtain prior

approval.129 The DRBC is directed to approve projects if it finds the project “would not

substantially impair or conflict with the comprehensive plan” for managing the basin.130 Certain

projects are exempt from the requirement for prior approval, including water withdrawals and

129

Delaware River Basin Compact, art. 3, §3.8, available at http://www.state.nj.us/drbc/regs/compa.pdf. See also art.

10, §10.3.

130

Id. at §3.8.

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diversions that do not exceed an average of 100,000 gallons per day.131 Specific regulatory

requirements apply to applications for withdrawals in excess of 1 million gallons on average per

day, including monitoring requirements, contingency plans for emergency conservation, and

reporting requirements.132 The DRBC has issued draft regulations to protect the basin’s resources

relating to the development of natural gas projects.133 Under the proposed regulations, DRBC

approval is required before water sources in the basin may be used for the purpose of natural gas

development projects.134

A similar regulatory scheme was established in the Susquehanna River basin. The SRBC also

imposes approval requirements for certain projects affecting the water resources of the basin.135

Among the projects generally requiring prior approval from the SRBC are new and increased

consumptive use projects using an average of 20,000 gallons per day or more; new and increased

withdrawals of an average of 100,000 gallons per day or more; and diversions into or out of the

basin of an average of 20,000 gallons per day or more.136 In addition to these general

requirements, the SRBC has adopted regulations specific to the Marcellus Shale, which require

approval for “any natural gas well development project in the basin targeting the Marcellus or

Utica shale formations, or any other formation …, for exploration or production of natural gas

involving a withdrawal, diversion or consumptive use, regardless of the quantity.”137

Lying along the northwestern perimeter of the Marcellus Shale region is the Great Lakes-St.

Lawrence River Basin. Approved by Congress in 2008, the Great Lakes-St. Lawrence River

Basin Water Resources Compact includes monitoring, registration, and reporting requirements to

protect the use of water resources within this basin.138 Within five years of the compact taking

effect, any withdrawal of an average of 100,000 gallons per day or more and any diversion must

be registered with the proper administering authority.139 Each party must be notified of and given

the opportunity to comment on any proposal for a consumptive use of 5 million gallons per day or

more.140 Under the compact, diversions of water resources out of the basin are generally

prohibited with few exceptions.141 Each state is required to adopt a regulatory program for

withdrawals and consumptive uses within five years of the effective date of the compact, which

sets a threshold level of regulation at an average of 100,000 gallons per day or more.142

131

18 C.F.R. §401.35.

18 C.F.R. §401.36.

133

Revised Draft Natural Gas Development Regulations (November 8, 2011), http://www.state.nj.us/drbc/

notice_naturalgas-draftregs.htm.

134

Natural Gas Development Regulations §§7.3(b) and 7.4 (November 8, 2011), http://www.state.nj.us/drbc/

naturalgas-REVISEDdraftregs110811.pdf.

135

Susquehanna River Basin Compact, art. 3, §3.10, http://www.srbc.net/about/srbc_compact.pdf.

136

18 C.F.R. §806.4(a)(1), (2), and (3).

137

18 C.F.R. §806.4(a)(8). An amendment has been proposed that would broaden the applicability of this provision. If

adopted as a final rule, “any unconventional natural gas development project in the basin involving a withdrawal,

diversion or consumptive use, regardless of the quantity,” would require SRBC approval. Susquehanna River Basin

Commission, “Review and Approval of Projects,” 76 Federal Register 41154-57 (July 13, 2011).

138

Great Lakes-St. Lawrence River Basin Water Resources Compact, available at http://www.cglg.org/projects/water/

docs/12-13-05/Great_Lakes-St_Lawrence_River_Basin_ Water_Resources_Compact.pdf.

139

Great Lakes–St. Lawrence River Basin Water Resources Compact, art. 4, §4.1, paragraph 3.

140

Great Lakes–St. Lawrence River Basin Water Resources Compact, art. 4, §4.6, paragraph 1.

141

Great Lakes–St. Lawrence River Basin Water Resources Compact, art. 4, §§4.8–4.9.

142

Great Lakes –St. Lawrence River Basin Water Resources Compact, art. 4, §4.10.

132

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Congressional Interest

The Marcellus Shale formation represents one of the largest unconventional or conventional

natural gas resources in the United States. Current and planned projects to develop Marcellus

Shale gas are apparent across the six-state region that overlies the resource. For example, gas

producers have reportedly planned over 2,000 gas wells just in West Virginia, and the state’s Oil

and Gas Commission estimates that, based on current information, there could be a well on every

40 acres in the state. Throughout the region, this activity is placing increasing demands on

regulatory agencies—especially state agencies—for necessary licensing, permitting, inspections,

and enforcement, and also for revising regulations. Because of questions related to water supply

and wastewater disposal, some state agencies and DRBC have been cautious about granting

permits until these issues are resolved. New York, in particular, is taking a cautious approach and

has accepted, but not processed, permits pending completion of a state Supplemental Generic

Environmental Impact Statement. At the same time, there is counter-pressure from companies,

drillers, and landowners to move forward with developing the gas resource. The success of

planned development activities could depend, in part, on the capacity of regulatory agencies to

provide the administrative and oversight resources to support such plans.

The development of the Marcellus Shale and other unconventional natural gas resources, and the

use of hydraulic fracturing in particular, has generated considerable debate in Congress and has

been the topic of hearings and legislation. Industry and many state agencies are arguing against

broad federal regulation of hydraulic fracturing under the SDWA, and noting a long history of the

successful use of this practice in developing oil and gas resources. A typical horizontal well is

estimated to cost between $3 million and $5 million,143 and industry representatives argue that

more federal regulation is unnecessary and would likely slow domestic gas development and

increase energy prices. At the same time, the amount of natural gas produced from

unconventional formations that rely on hydraulic fracturing continues to grow. Moreover, drilling

and reservoir stimulation methods have changed significantly over time as they have been applied

to more challenging formations, increasing markedly the amount of water and fracturing fluids

involved in production operations. It is the rapidly increasing and geographically expanding use

of hydraulic fracturing and directional drilling, along with a number of citizen complaints of

water contamination and other environmental problems attributed to this practice—and to shale

gas development more broadly—that has led to calls for greater state and/or federal

environmental oversight of this activity.

Pending Federal Legislation

In March 2011, the Fracturing Responsibility and Awareness of Chemicals Act of 2011 (FRAC

Act) was introduced in the House (H.R. 1084) and Senate (S. 587). The bills are substantively

similar and would amend the Safe Drinking Water Act to revise the definition of underground

injection to include hydraulic fracturing, and to create a new disclosure requirement for the

chemicals used in hydraulic fracturing. Under both bills, the definition of “underground injection”

that was amended in 2005 to exclude most hydraulic fracturing would be amended again to

143

Larry Wickstrom, et al., The Marcellus and Utica Shale Plays in Ohio, Ohio Department of Natural Resources,

Division of Geological Survey, March 11, 2011, http://www.dnr.state.oh.us/portals/10/energy/

Marcellus_Utica_presentation_OOGAL.pdf.

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include “the underground injection of fluids or propping agents pursuant to hydraulic fracturing

operations related to oil or gas production activities.”144

The FRAC Act also would require anyone conducting hydraulic fracturing to disclose to the state

(or EPA if EPA has primary enforcement responsibility), before starting hydraulic fracturing

operations, a list of chemicals intended for use in any underground injection during the

operations.145 The information must include identification of the chemical constituents of

mixtures, Chemical Abstracts Service numbers for each chemical and constituent, material safety

data sheets when available, and the anticipated volume of each chemical. Additionally, within 30

days after the end of any hydraulic fracturing operations, the operator must provide information

on the chemicals and amounts actually used.146

The bills would also require that the state or EPA make the disclosure of chemical constituents

public, including posting the information on a website. The bills specify that the disclosure

requirements do not authorize the state or EPA to require the public disclosure of proprietary

information. This language attempts to protect proprietary business information, that is, “secret”

formulas of the chemical constituents being used in hydraulic fracturing or practices that drilling

companies believe they should not be required to disclose to regulators or the public.

Increasingly, state oil and gas production laws and rules are requiring disclosure to regulators of

the chemical constituents being used in hydraulic fracturing, while extending similar protections

for proprietary business information.147

Furthermore, the FRAC Act would require operators to disclose proprietary chemical information

to treating medical professionals in cases of medical emergencies.148 Although most state oil and

gas rules do not require disclosure of proprietary chemical information to medical professionals,

such disclosure broadly parallels federal requirements under the Occupational Safety and Health

Act (OSHAct).149 Nonetheless, the OSHAct requirements were not designed for environmental

144

H.R. 1084, at §2(a). S. 587 is similar but does not include geothermal production activities.

The lack of information regarding chemicals used in hydraulic fracturing has made investigations of contamination

difficult, as well owners and state regulators typically have not known which chemicals to test for to determine whether

a fracturing fluid has migrated into a water source. In April 2011, the Ground Water Protection Council and the

Interstate Oil and Gas Compact Commission launched a hydraulic fracturing chemical registry website where

companies voluntarily post information on chemicals used in hydraulic fracturing on a well-by-well basis. The website

covers wells fractured since January 1, 2011. The website also includes state oil and gas regulations and other

information. See http://fracfocus.org/.

146

Id. at §2(b).

147

The Pennsylvania Department of Environmental Protection (DEP) requires drilling companies to disclose the names

of all chemicals to be stored and used at a drilling site as part of the permit application process. The information is kept

on file with DEP and is available to landowners, local governments, and emergency responders. Ohio and West

Virginia also have adopted hydraulic fracturing reporting and disclosure requirements. New York’s RDSGEIS also

contains disclosure requirements. In April 2011, the Ground Water Protection Council and the Interstate Oil and Gas

Conservation Commission launched a website that provides a public registry of chemicals used in hydraulic fracturing,

with companies voluntarily identifying chemicals used in fracturing individual wells. The site also includes state

regulations and other information. See http://fracfocus.org/.

148

H.R. 1084, §2(b).

149

The Occupational Safety and Health Administration has promulgated a set of regulations under the Occupational

Safety and Health Act (OSHAct; 29 USC §651 et seq.), referred to as the Hazard Communication Standard (29 C.F.R.

§1910.1200). Additionally, OSHAct regulations require operators to maintain Material Safety Data Sheets (MSDS) for

hazardous chemicals at the job site. The federal Emergency Planning and Community Right to Know Act (EPCRA)

requires that facility owners submit an MSDS for each hazardous chemical present that exceeds an EPA-determined

threshold level, or a list of such chemicals, to the local emergency planning committee (LEPC), the state emergency

(continued...)

145

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investigation purposes, and the provided information may not be suited for such purposes.

Consequently, calls for disclosure of hydraulic fracturing chemicals have increased as

homeowners and others express concern about the potential presence of unknown chemicals in

tainted well water near oil and gas operations.

Other bills in the 112th Congress also address hydraulic fracturing. H.R. 2133, the Fulfilling U.S.

Energy Leadership (FUEL) Act, recognizes the role of the states in regulating oil and natural gas

production and declares a sense of Congress that “the Safe Drinking Water Act (42 U.S.C. 300f et

seq.) was not intended to regulate natural gas and oil well construction and stimulation.” The bill

further notes that industry should be encouraged to voluntarily disclose chemicals used in the

hydraulic fracturing process and that the information should be made available to the public.

Reported bill H.R. 1425 (Section 514) would amend the Small Business Act150 to direct federal

agencies to give funding preference for research on reducing the environmental (including water

quality) impact of the use of hydraulic fracturing during natural gas exploration activities.

Conclusion

Natural gas locked in tight, impermeable shale has been uneconomical to produce until recently.

Advances in directional well drilling and reservoir stimulation have dramatically increased the

production from these unconventional shales. However, the development of the Marcellus and

other shales comes with some challenges and controversy.

The Marcellus Shale formation represents one of the largest unconventional or conventional

natural gas resources in the United States. The natural gas produced from the eastern portion of

the formation is pipeline quality, requiring no upgrading. Although the gas transmission pipeline

network needed to supply the residential, retail, and commercial customers in the northeast

United States is largely in place, gas producers would need to construct an extensive network of

gathering pipelines and supporting infrastructure to move the gas from the new well fields to the

transmission pipelines, as is the case for developing any new well field. The lack of such

infrastructure may limit or delay gas production in some areas of the region.

Shale gas development has stirred concerns regarding water consumption and potential

groundwater and water well contamination from hydraulic fracturing, and surface water

contamination from disposal of the fracturing fluids. The process of developing a shale gas well is

an issue of concern for increasing the risk of water contamination, and concerns about

contamination of fresh surface water or groundwater must be addressed during three phases of

gas well development: (1) drilling through an overlying aquifer, completing and casing the well,

(2) stimulating the well via hydraulic fracturing, and (3) flowback of fluids to the surface during

development of the well and production of the gas). If contamination of fresh water supplies from

shale gas development is suspected, each of these three phases must be carefully examined to

ensure that each is conducted without causing undue environmental impacts.

(...continued)

response commission, and the local fire department. For non-proprietary information, EPCRA generally requires a

LEPC to provide an MSDS to a member of the public on request.

150

15 U.S.C. §638.

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1. Drilling and well construction through an aquifer: A properly cased well allows

gas production up through the well to the surface, while preventing drilling

fluids, hydraulic fracturing fluids, or natural gas from leaking into the permeable

aquifer and contaminating groundwater. Construction of an oil and gas well of

any type generally requires penetration of near-surface fresh water aquifers, and

the application of rigorous drilling and well completion techniques is vital during

this phase of production. These activities are regulated by the states.

2. Hydraulic fracturing: Hydraulic fracturing does induce new fractures into the

Marcellus Shale, and may lengthen existing fractures. The chances of creating or

extending fractures linking the Marcellus Shale to an overlying aquifer appear

remote, however, because the vertical distance separating the Marcellus Shale

from most aquifers is typically much greater than the length of the fractures

generally induced during hydraulic fracturing. Hydraulically fractured gas

production wells are subject to state regulations, but legislation has been

introduced to authorize EPA to regulate broadly hydraulic fracturing under

SDWA, which likely would affect state requirements.

3. Flowback of fracking fluids and produced waters: The flowback water pumped

back to the surface after fracturing poses a significant environmental

management challenge in the Marcellus Shale region. The flowback and

produced water’s high content of salts, minerals, and other contaminants must be

disposed of or adequately treated before discharged to surface waters. State laws

and the federal Clean Water Act regulate the discharge of this flowback water and

other drilling wastewater to surface waters, while the Safe Drinking Water Act

regulates deep well injection of such wastewater.

Cumulatively, the concerns about the potential water quality and other environmental impacts of

unconventional gas exploration and development, including in the Marcellus Shale, have

prompted close examination at a number of levels.

•

Congress has directed EPA to “review the risks that hydraulic fracturing poses to

drinking water supplies, using the best available science, as well as independent

sources of information.”151 EPA expects to report on the interim research results

in 2012, and issue a follow-up report in 2014.

•

In March 2011, President Obama announced a broad “Blueprint for a Secure

Energy Future.” In it, the President asked the DOE Secretary to identify steps that

can be taken to improve the safety and environmental performance of shale gas

production, and to develop consensus recommendations on practices to ensure

the protection of public health and the environment, including water quality.152 In

151

P.L. 111-88, H.Rept. 111-316. The report accompanying the Department of the Interior, Environment, and Related

Agencies Appropriations Act, FY2010 (H.R. 2996, H.Rept. 111-180), includes the following provision:

Hydraulic Fracturing Study.—The conferees urge the Agency to carry out a study on the

relationship between hydraulic fracturing and drinking water, using a credible approach that relies

on the best available science, as well as independent sources of information. The conferees expect

the study to be conducted through a transparent, peer-reviewed process that will ensure the validity

and accuracy of the data. The Agency shall consult with other Federal agencies as well as

appropriate State and interstate regulatory agencies in carrying out the study, which should be

prepared in accordance with the Agency’s quality assurance principles.

152

See http://www.whitehouse.gov/sites/default/files/blueprint_secure_energy_future.pdf.

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November, the Secretary of Energy Advisory Board (SEAB) Shale Gas

Subcommittee issued a final report, with recommendations for state and federal

governments and industry. Water quality recommendations, aimed mainly at the

states, include (1) adopting best practices for well construction (casing,

cementing, and pressure management), (2) adopting requirements for background

water quality measurements, (3) manifesting all water transfers across various

locations, and (4) measuring and publicly reporting the composition of water

stocks and flow throughout the fracturing and cleanup process. The SEAB also

suggested that states review and modernize rules and enforcement practices.153

•

In April 2011, the New York State Attorney General stated he would sue the

federal government if an environmental review of natural gas drilling in the

Delaware River Basin was not conducted under the National Environmental

Policy Act (NEPA).154 Also in April, a coalition of environmental advocates,

including the Chesapeake Bay Foundation, petitioned the White House to

conduct an environmental impact analysis on the effects that natural gas drilling

and production may have within the Marcellus Shale region.155

•

In October 2011, EPA initiated a rulemaking to set technology-based pretreatment standards to regulate discharges of shale gas wastewaters to publicly

owned treatment works.

•

Across the region, state oil and gas regulators and environmental regulators have

been evaluating and revising regulations to strengthen water quality protections

during shale gas exploration and production.

Shale gas development using high-volume horizontal drilling and hydraulic fracturing has been

done for only about a decade and is increasing rapidly, catching states and communities at various

states of preparedness. The industry’s growth has created new regulatory, enforcement, and

oversight challenges for state officials, and often new concerns for landowners and communities

in the Marcellus Shale region. The growing number of gas wells and related infrastructure and

land-use changes has drawn attention to the adequacy of regulatory oversight governing this

industry.

Natural gas production has long been regulated by the states. State oil and gas and environmental

protection agencies widely support keeping responsibility for regulating oil and gas production

generally, and hydraulic fracturing specifically, with the states. The Interstate Oil and Gas

Compact Commission (IOGCC), representing the oil and gas producing states, adopted a

resolution urging Congress not to remove the fracturing exemption from provisions of the SDWA,

noting that the process is a temporary injection-and-recovery technique and does not fit the UIC

program which EPA generally developed to address the permanent disposal of wastes.

If Congress were to require EPA to regulate all hydraulic fracturing of oil and gas wells, a key

issue would involve EPA’s capacity to assume such a role. EPA likely would require substantial

153

U.S. Department of Energy, The Secretary of Energy Advisory Board, Shale Gas Production Subcommittee, Second

Ninety Day Report—November 18, 2011, http://www.shalegas.energy.gov/.

154

Eric T. Schneiderman, New York State Attorney General, Schneiderman to Feds: Commit to Study Safety Impacts of

“Fracking” in Delaware River Basin or I’ll Sue, Press Release, Office of the Attorney, April 18, 2011.

NEPA is codified at 92 U.S.C. §§4321-4347.

155

See http://www.cbf.org/document.Doc?id=640.

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new resources and technical staff to oversee major elements of oil and gas production and to

directly implement any new rules in non-primacy states. For example, unless Pennsylvania and

New York assumed primacy for the UIC program, EPA would have responsibility for permitting

and overseeing all hydraulically fractured wells in those states, while the wells remained subject

to state permitting requirements and regulations. This scenario has raised concerns from states

and industry regarding the potential benefits, costs, and redundancies that may result from such

an approach.

Nonetheless, given the concern about potential water contamination expressed by citizens and

communities, and uneven regulation across the states, some continue to urge greater federal

involvement. The American Water Works Association (AWWA, representing drinking water

professionals and public water suppliers), various towns, and environmental groups support the

FRAC Act.

EPA currently is developing new measures to protect water quality during shale gas

development.156 The agency is developing regulations under the Clean Water Act to regulate

flowback and produced water discharges to municipal wastewater treatment plants.157 Also, EPA

is writing guidance under the SDWA UIC program to assist states with permitting hydraulic

fracturing operations that use diesel fuel. The pending diesel guidance may provide insight into

how the agency might regulate hydraulic fracturing broadly, if directed to do so by Congress.

Currently, there is little agreement as to the potential risks that shale gas development poses to

water resources across the region. Given the level of debate, it appears that the understanding of

the risks could benefit from a better scientific foundation. Congress has urged EPA to study the

relationship between hydraulic fracturing and drinking water. The results of the EPA study, along

with work being done by the states, interstate commissions, industry, and others, should enable a

better assessment of the risks that unconventional shale development may pose to water

resources, and help inform any potential congressional action. In the meantime, states across the

Marcellus Shale region continue to review and revise regulatory programs in response to robust

growth in the shale gas industry.

156

On federal lands, the Bureau of Land Management (BLM), within the Department of the Interior, administers oil

and gas leasing and coordinates planning and permitting with other federal agencies, as appropriate. The BLM also is

reviewing and revising its oil and gas regulations to reflect changes in production technologies and processes.

157

Additionally, on July 28, 2011, EPA proposed new regulations to reduce air pollution from upstream oil and natural

gas production sources currently unregulated at the federal level. The proposed rules include (1) a new source

performance standard for volatile organic compounds; (2) a new source performance standard for sulfur dioxide; (3) an

air toxics standard for oil and natural gas production; and (4) an air toxics standard for natural gas transmission and

storage. An extension to the original consent decree requires EPA to take final action on these regulations by April 3,

2012. See U.S. Environmental Protection Agency, “Oil and Natural Gas Sector: New Source Performance Standards

and National Emission Standards for Hazardous Air Pollutants Reviews,” 76 Federal Register 52738, August 23, 2011,

http://www.gpo.gov/fdsys/pkg/FR-2011-08-23/pdf/2011-19899.pdf.

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