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Hydraulic fracturing for natural gas: impact on health and environment Skip to content
Publicly Available Published by De Gruyter March 4, 2016

Hydraulic fracturing for natural gas: impact on health and environment

  • David O. Carpenter EMAIL logo

Abstract

Shale deposits exist in many parts of the world and contain relatively large amounts of natural gas and oil. Recent technological developments in the process of horizontal hydraulic fracturing (hydrofracturing or fracking) have suddenly made it economically feasible to extract natural gas from shale. While natural gas is a much cleaner burning fuel than coal, there are a number of significant threats to human health from the extraction process as currently practiced. There are immediate threats to health resulting from air pollution from volatile organic compounds, which contain carcinogens such as benzene and ethyl-benzene, and which have adverse neurologic and respiratory effects. Hydrogen sulfide, a component of natural gas, is a potent neuro- and respiratory toxin. In addition, levels of formaldehyde are elevated around fracking sites due to truck traffic and conversion of methane to formaldehyde by sunlight. There are major concerns about water contamination because the chemicals used can get into both ground and surface water. Much of the produced water (up to 40% of what is injected) comes back out of the gas well with significant radioactivity because radium in subsurface rock is relatively water soluble. There are significant long-term threats beyond cancer, including exacerbation of climate change due to the release of methane into the atmosphere, and increased earthquake activity due to disruption of subsurface tectonic plates. While fracking for natural gas has significant economic benefits, and while natural gas is theoretically a better fossil fuel as compared to coal and oil, current fracking practices pose significant adverse health effects to workers and near-by residents. The health of the public should not be compromized simply for the economic benefits to the industry.

Introduction

Shale deposits around the earth contain significant reservoirs of natural gas and oil. Until recently these deposits were not economically accessible, but recent advances in the development of the process of horizontal hydrofracturing, or “fracking”, of the shale formations have allowed recovery of natural gas in a cost-effective fashion. This method has also been referred to as “unconventional oil and gas extraction”. The application of these procedures has occurred especially in North America and Australia, but almost certainly will be applied throughout much of the world in the future. It has been suggested that the new largest developments will occur in China, India, Indonesia and Poland, all of whom have significant shale reserves (1, 2).

Figure 1 shows the global distribution of shale deposits. The natural gas is contained within the shale deposits, which are often located at significant depths of several kilometers, much below the level of the water table. A borehole is drilled vertically into the shale area and then is drilled laterally. The well casing of steel pipe is installed, and the upper portion lined with concrete. Water at high pressure containing a variety of chemicals (often proprietary) and a propping agent (usually sand) is injected into the shale to break it apart and allow release of the gas. The general classes of chemicals include biocides such as glutaraldehyde, surfactants, friction reducers, electrolytes, breakers such as sodium chloride, corrosion inhibitors, iron control agents, oxygen scavengers, and scale inhibitors. The propping agents hold open the fractures, which may be up to 2.5 cm in length and normally extend several to hundreds of meters from the well casing. The amount of water required is significant. For 17,265 horizontal fracking sites in the US between 2000 and 2010 the average water used was 11,392 m3/well, and the maximum was 42,372 m3/well (3).

Figure 1: Map of basins with assessed shale oil and gas formations, as of May 2013.From US Energy Information Administration and US Geological Survey (2).Source: United States basins from U.S. Energy Information Administration and United States Geological Survey; other basins from ARI based on data from various published studies.
Figure 1:

Map of basins with assessed shale oil and gas formations, as of May 2013.

From US Energy Information Administration and US Geological Survey (2).

Source: United States basins from U.S. Energy Information Administration and United States Geological Survey; other basins from ARI based on data from various published studies.

Health and environmental impacts

While the economic impacts of being able to access these natural gas deposits have already been considerable, there are also a number of concerns about human health impacts, both long and short term. The amount of water used per well is enormous, and many wells in the US are in places where adequate water supply is already a concern. Furthermore, up to 40% of the injected water comes back as produced water, containing chemicals, unusually high salt concentrations from primeval deposits, and naturally-occurring radioactive materials. The disposal of the produced water is a major problem, as conventional waste-water treatment plants are usually not capable of removing the chemicals or radioactive compounds. Ground and surface water contamination has been reported (4, 5) resulting from transportation spills, well casing leaks, leaks through the fractured rock, and wastewater disposal. Methane contamination of drinking water is a concern (6). In some places there was sufficient methane in household drinking water such that water from the kitchen sick could be lit by a flame. Depending upon the nature of the rock formations, the flow-back water may contain significant levels of radium. Radium, unlike uranium or thorium, is relatively water soluble, and the two principal isotopes have half-lives of 1600 and 5.75 years. In the Marcellus shale in Eastern United States the produced water had a median radium activity 2460 pCi/L, which is extremely high compared with the drinking water limit of 5 pCi/L and the limit for industrial effluent of 60 pCi/L (7). Because the produced water contains high salt concentrations there have been occasions where it was spread on roads for ice control in the winter without anyone monitoring levels of radioactivity. Since radium decays to radon gas, which has a half-life of 3.8 days, there is also some concern about levels of radon in natural gas. Radon radioactivity measured in natural gas samples obtained from 11 wells in Pennsylvania ranged from 1 to 79 pCi/L (8).

One solution for dealing with produced water has been to inject it deep into the earth. This, however, has resulted in a sharp increase in earthquakes (9). Fortunately to date none have been large, but the frequency with which they occur in areas with deep injection indicates potential danger.

In addition to concerns about surface and groundwater contamination with chemical and radioactive materials, there are major concerns about air pollution (10). Natural gas is primarily methane, but also contains other volatile organic compounds, aromatics, CO2, H2S and SO2 (11). There is often significant release of natural gas from well sites and compressor stations. My colleagues and I have reported on levels of volatile organic pollutants including benzene, hexane, formaldehyde, and H2S around fracking sites in six US states (12). When compared to cancer and non-cancer federal exposure standards, we found that 40% of the samples we collected exceeded safe levels. Figure 2 shows results from samples obtained in Wyoming in relation to the minimal risk levels (MRL) set by ATSDR for benzene, H2S, mixed xylenes and n-hexane. All these pollutants harm the respiratory and nervous systems and of particular concern is benzene, a known human carcinogen. Figures 3 and 4 show results for concentrations of formaldehyde and 1,3-butadiene in samples from Arkansas and Pennsylvania in relation to the USEPA IRIS 1/10,000 risk level, respectively. With the exception of formaldehyde, which was collected on a badge for an exposure period of at least 8 h, all other air samples were collected at points in time when there was an odor or some other reason to expect elevated concentrations of contaminants. These may be worst case scenarios, but clearly indicate potential hazards to human health. The elevations in levels of formaldehyde were striking. Formaldehyde is also a known human carcinogen. It is not certain that formaldehyde is a component of natural gas, but it is formed both from combustion (flaring of natural gas, exhaust from diesel trucks) and by action of sunlight on methane. Others have measured polyaromatic hydrocarbons (PAHs) in particulates and found high concentrations around well sites (13). PAHs are also known human carcinogens. Because cancer has a long latency the presence of so many known carcinogens in the air around fracking sites is of great concern.

Figure 2: Concentrations of volatile compounds exceeding health-based risk levels in samples collected in Wyoming.Note log scale on y-axis. Dashed lines represent ATSDR intermediate-term MRLs. Dotted lines represent ATSDR chronic MRLs (not displayed: toluene, ethylbenzene, and formaldehyde). From Macey et al. (12).
Figure 2:

Concentrations of volatile compounds exceeding health-based risk levels in samples collected in Wyoming.

Note log scale on y-axis. Dashed lines represent ATSDR intermediate-term MRLs. Dotted lines represent ATSDR chronic MRLs (not displayed: toluene, ethylbenzene, and formaldehyde). From Macey et al. (12).

Figure 3: Concentrations of volatile compounds exceeding health-based risk levels in samples collected in Arkansas.Dashed lines represent EPA IRIS 1/10,000 cancer risk for formaldehyde and 1,3 butadiene. From Macey et al. (12).
Figure 3:

Concentrations of volatile compounds exceeding health-based risk levels in samples collected in Arkansas.

Dashed lines represent EPA IRIS 1/10,000 cancer risk for formaldehyde and 1,3 butadiene. From Macey et al. (12).

Figure 4: Concentrations of volatile compounds exceeding health-based risk levels in samples collected in Pennsylvania.Dashed line represents EPA IRIS 1/10,000 cancer risk for formaldehyde. Dotted line represents EPA IRIS 1/100,000 cancer risk for benzene. From Macey et al. (12).
Figure 4:

Concentrations of volatile compounds exceeding health-based risk levels in samples collected in Pennsylvania.

Dashed line represents EPA IRIS 1/10,000 cancer risk for formaldehyde. Dotted line represents EPA IRIS 1/100,000 cancer risk for benzene. From Macey et al. (12).

Colborn et al. (14) examined 632 chemicals known to be used during natural gas extraction, and noted that many of these chemicals have known effects on skin, eyes, nervous, respiratory, gastrointestinal and cardiovascular systems. McKenzie et al. (15) observed elevations in rates of congenital heart disease and possibly neural tube defects in children born to mothers living within 10 miles of natural gas wells. There is strong evidence that air pollution increases risk of asthma (16) and cardiovascular disease (17). Inhalation of volatile organics is known to result in central nervous system alterations (18). The health of farm and pet animals is also a concern at sites near to the fracking wells (19). While there are few peer-reviewed reports of symptoms experienced by residents living near to fracking sites, advocacy groups have documented elevations in respiratory symptoms, behavior/mood and energy changes, and nosebleeds (20, 21).

A major long-term concern is determining the net benefit or harm from the process of fracking and burning natural gas as compared to that from extraction and use of alternative fossil fuels. Howarth (22) has presented data in support of the view that the greenhouse footprint of shale gas is even worse than that of coal, primarily because of methane releases, although the analysis of Hultman et al. (23) concluded that the greenhouse gas impacts of unconventional natural gas extraction and use was only 56% of that of coal. Methane is actually a more potent greenhouse gas than carbon dioxide, although it has a shorter half-life in the atmosphere (24). The industry should be able to find ways to reduce the unintended release of methane, but it will never go to zero. Climate change is a global concern, and these different conclusions indicate that further study is necessary. Obviously the ultimate goal should be to ween all of us away from use of fossil fuels.

In theory combustion of natural gas should be preferable to combustion of coal because it produces less CO2. But any advantage is offset by releases of methane to the atmosphere as well as local releases of methane along with other VOCs, H2S, particulate air pollution and formaldehyde. The short term health effects of fracking will be primarily on workers and near-by residents who are exposed to air and water contaminants, radioactivity and excessive noise and light pollution. These exposures will results in respiratory symptoms, neurologic impairment from the H2S and volatile organic compounds, and stress resulting from the smells, dusts, noise and light pollution. Esswein et al. (25) have also reported worker exposure to respirable crystalline silica that can result in restrictive lung disease. Furthermore, there are long-term dangers not only from cancer occurring in near-by residents and workers, but also from increased release of greenhouse gasses, excessive use of water and even generation of earthquakes. Fracking that is done in a responsible fashion may be of benefit, but present practices pose significant hazards to health and the environment.


Corresponding author: David O. Carpenter, MD, Institute for Health and the Environment, University at Albany, Rensselaer, NY 12144, USA, E-mail:

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Received: 2015-10-16
Accepted: 2015-12-14
Published Online: 2016-03-04
Published in Print: 2016-03-01

©2016 by De Gruyter

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