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Proceedings of the National Academy of Sciences of the United States of America logoLink to Proceedings of the National Academy of Sciences of the United States of America
. 2016 Nov 14;113(48):13636–13641. doi: 10.1073/pnas.1605913113

Identification and characterization of high methane-emitting abandoned oil and gas wells

Mary Kang a,1, Shanna Christian b, Michael A Celia c, Denise L Mauzerall c,d, Markus Bill e, Alana R Miller c, Yuheng Chen b, Mark E Conrad e, Thomas H Darrah f, Robert B Jackson a,g
PMCID: PMC5137730  PMID: 27849603

Significance

Millions of abandoned oil and gas wells exist across the United States and around the world. Our study analyzes historical and new field datasets to quantify the number of abandoned wells in Pennsylvania, individual and cumulative methane emissions, and the attributes that help explain these emissions. We show that (i) methane emissions from abandoned wells persist over multiple years and likely decades, (ii) high emitters appear to be unplugged gas wells and plugged/vented gas wells, as required in coal areas, and (iii) the number of abandoned wells may be as high as 750,000 in Pennsylvania alone. Knowing the attributes of high emitters will lead to cost-effective mitigation strategies that target high methane-emitting wells.

Keywords: abandoned wells, oil and gas development, methane emissions, high emitters, climate change

Abstract

Recent measurements of methane emissions from abandoned oil/gas wells show that these wells can be a substantial source of methane to the atmosphere, particularly from a small proportion of high-emitting wells. However, identifying high emitters remains a challenge. We couple 163 well measurements of methane flow rates; ethane, propane, and n-butane concentrations; isotopes of methane; and noble gas concentrations from 88 wells in Pennsylvania with synthesized data from historical documents, field investigations, and state databases. Using our databases, we (i) improve estimates of the number of abandoned wells in Pennsylvania; (ii) characterize key attributes that accompany high emitters, including depth, type, plugging status, and coal area designation; and (iii) estimate attribute-specific and overall methane emissions from abandoned wells. High emitters are best predicted as unplugged gas wells and plugged/vented gas wells in coal areas and appear to be unrelated to the presence of underground natural gas storage areas or unconventional oil/gas production. Repeat measurements over 2 years show that flow rates of high emitters are sustained through time. Our attribute-based methane emission data and our comprehensive estimate of 470,000–750,000 abandoned wells in Pennsylvania result in estimated state-wide emissions of 0.04–0.07 Mt (1012 g) CH4 per year. This estimate represents 5–8% of annual anthropogenic methane emissions in Pennsylvania. Our methodology combining new field measurements with data mining of previously unavailable well attributes and numbers of wells can be used to improve methane emission estimates and prioritize cost-effective mitigation strategies for Pennsylvania and beyond.


Methane is a potent greenhouse gas (GHG) with a global warming potential 86 times greater than carbon dioxide over a 20-y time horizon (1). A reduction of methane emissions can lead to substantial climate benefits, especially in the short term (2). Recent measurements of methane emissions from abandoned oil and gas wells in Pennsylvania indicate that these wells may be a significant source of methane to the atmosphere (3). Across the United States, the number of abandoned oil/gas wells is estimated to be 3 million or more (4, 5), and this number will continue to increase in the future. As of February of 2016, abandoned oil/gas wells remain outside of GHG emissions inventories, despite evidence that emissions may be substantial nationally. As interest in mitigation of GHG emissions increases, quantifying persistent and large emissions and mitigating them will be increasingly important.

Methane emissions from abandoned wells, as with other fugitive sources in the oil and gas sector, appear to be governed by relatively few high emitters (3, 68). It is important for current and future abandoned wells to identify the characteristics that lead to high emissions. This information can provide a rationale for prioritized mitigation.

The century-and-a-half-long history of oil and gas development in Pennsylvania and other US states, such as Texas and California, has resulted in millions of abandoned wells, and in many cases, poorly documented or missing well records (3, 911). As a result, there is a lack of data to characterize abandoned oil and gas wells and the possible relationship between methane emissions and well attributes. Well attributes that may be correlated with methane emissions include depth, plugging status, well type, age, wellbore deviation, geographic location, oil/gas production, and abandonment method (9, 10, 1214). Previous studies have been limited to wells and attributes with readily available data (12, 14). However, compilation and analysis of historical documents, modern digital databases, and field investigations can be used to infer well attributes of the many wells without data. In this work, we focus on Pennsylvania, which has the longest history of oil and gas development, to determine and explore the role of well attributes, mainly depth, plugging status, well type (e.g., gas or oil), and coal area designation as well as proximity to subsurface-based energy activities, on methane leakage.

Previously estimated numbers of abandoned wells in Pennsylvania range from 300,000 to 500,000 (3, 15) and are based on either incomplete databases or qualitative expert opinion. The Pennsylvania Department of Environmental Protection (DEP) manages oil and gas well data and has records of only 31,676 abandoned oil and gas wells for the state as of October of 2015. Only 5% of the wells in Pennsylvania measured in an earlier study (3) were on the DEP’s list. Furthermore, because of changes in governing bodies and regulations over time, the quality of available records is likely to be poorer for older wells (15). To estimate the actual number of wells, historical documents and other data sources from oil and gas development need to supplement state records.

Pennsylvania, Ohio, West Virginia, and Kentucky, states through which the Appalachian Basin extends, are among the top 10 US states in terms of the number of inactive and total oil and gas wells (10). Questions remain about potential links between abandoned wells and other active subsurface-based energy activities commonly found in theses states, such as, underground natural gas storage and unconventional oil/gas production (9, 16). For example, could nearby unconventional gas production or underground gas storage reservoirs lead to larger methane leaks from abandoned wells? Previously available measurements and data are insufficient to explore these potential effects. Therefore, we conducted additional field measurement campaigns to fill the data gaps. In the process, we expanded the geographic coverage, previously limited to northwestern Pennsylvania (3), to cover much of the western portion of the state (Fig. 1).

Fig. 1.

Fig. 1.

The 88 measured abandoned oil and gas wells in Pennsylvania overlaid with conventional oil and gas pools (34), underground natural gas storage fields (34), and workable coal seams within the study area (38).

Geochemical information including methane and noble gas isotopes is useful for understanding methane sources (1618). To evaluate wellbore integrity and design effective mitigation strategies, it is important to identify the source of methane, including whether it is microbial or thermogenic, and if possible, the source formation and migration pathway. It is also important to know as many well attributes as possible and cross-check those attributes with geochemical data when possible. Here, we provide an expanded set of geochemical information including carbon and hydrogen isotopes of methane and concentrations of ethane, propane, n-butane, and noble gases.

To identify and characterize high methane-emitting abandoned oil/gas wells, we provide in this paper (i) a database of previously unavailable attributes of measured abandoned wells; (ii) 122 additional field measurements over multiple seasons of methane flow rates and geochemical data, including previously unavailable hydrogen isotopes of methane and noble gas data; (iii) improved estimates of well numbers based on all available data sources; and (iv) an attribute-based methane emissions estimate for abandoned oil and gas wells in Pennsylvania. These data and the associated analysis framework will improve estimates of methane emissions from abandoned oil and gas wells and help develop mitigation strategies across Pennsylvania and beyond.

Results

Methane Flow Rates and Well Attributes.

Methane flow rates span from below detection (BD) to 105 mg h−1 well−1 for positive methane flow rates (sources of methane to the atmosphere) and from BD to −101 mg h−1 well−1 for negative methane flow rates (sinks of methane from the atmosphere) (Fig. 2). Most methane flow rates from abandoned wells (90%) are positive, and all negative numbers are small in magnitude.

Fig. 2.

Fig. 2.

Methane flow rates of 88 abandoned wells in Pennsylvania and the coefficient of variation of methane flow rates measured from 2 to 10 times over 2 years (July of 2013 to June of 2015) at 27 wells. If more than one measurement has been made at the given well, the methane flow rates represent an average of all measurements taken. Plugging status is determined based on field observations, and the well type (gas vs. oil or combined oil and gas) is determined using our database-based estimates of well attributes. Methane flow rates below detection (BD) limits (P values > 0.2) are shown in the gray portion of the plot between the plots of positive and negative flow rates.

Methane flow rates are measured from different categories of abandoned wells in Pennsylvania. For the measured wells without well records, plugging status is determined based on field observations, and the well type (gas vs. oil or combined oil and gas) is determined based on our estimates of well attributes from our assembled database (SI Appendix). Across the dataset, abandoned gas wells, specifically unplugged and plugged/vented wells (Pennsylvania Code, Chapter 78), have the highest observed rates of methane emissions (Fig. 2). Abandoned oil wells have consistently lower emissions compared with abandoned gas wells (Fig. 2). The highest measured methane flow rate is 3.5 ×105 mg h−1 well−1 at an unplugged gas well in McKean County, and the second highest is 2.9 ×105 mg h−1 well−1 at a plugged but vented gas well in Clearfield County. Venting of plugged wells is required in coal areas, which in Pennsylvania, include regions where mineable coal seams exist (SI Appendix).

Methane flow rates are most strongly related to well type (W; gas vs. oil or combined oil and gas), plugging status (P), and coal area designation (C) (Table 1 and SI Appendix, Table S3). No strong trends are observed between methane flow rates and well depth (d), distance to the nearest unconventional well (rU), or distance to the nearest underground natural gas storage field (rS). A multilinear fit of d, W, P, C, rU, and rS to lnm˙, where m˙ (mg hour−1 well−1) is the methane flow rate, gives an R2 value of 0.44 and a P value of 4.4×108. The P values for the intercept, C, P, and W are below 0.05 and range from 2×106 (for C) to 0.04 (for the intercept). The P values for d, rS, and rU are high at 0.3, 0.8, and 0.4, respectively. The statistically significant well attributes (P values < 0.05) based on the multilinear regression analysis (Table 1 and SI Appendix, Table S3) are used in methane emissions estimation. The methane emission factors for nine well categories defined by combinations of W, P, and C range from 1.2 ×102 to 6.0 ×104 mg h−1 well−1 (Table 2).

Table 1.

Variable coefficients of the multilinear model with R2 value of 0.44 and P value of 4.4 × 10−8

Variable in model Variable coefficient
Intercept 2.84*
D 0.00039
C = coal area −5.50***
P = unplugged 3.99***
P = plugged/vented 8.33***
W = oil −2.88*
rS 0.016
rU −0.087

These results are for model L6b in SI Appendix, Table S3. The results of additional models are shown and discussed in SI Appendix. P values are noted (*P < 0.05; ***P < 0.001).

Table 2.

Emission factors based on coal indicator, plugging status, and well type

Well type and coal area designation Emission factor (mg⋅h−1⋅well−1) No. of measured wells SE
Unplugged Plugged Unplugged Plugged Unplugged Plugged
All
 None 2.2 ×104 11.5 ×104 53 35 9.2 ×103 1.0 ×104
 Coal 1.2 ×103 4.3 ×104 17 12 9.9 ×102 2.9 ×104
 Noncoal 3.1 ×104 4.5 ×102 36 23 1.3 ×104 2.8 ×102
Oil and combined oil and gas
 None 1.9 ×102 3.3 ×102 34 13 9.7 ×101 2.6 ×102
 Coal 1.1 1.2 ×102 13 1 9.1 ×101 n/a
 Noncoal 3.1 ×102 3.6 ×102 21 12 1.5 ×102 2.8 ×102
Gas
 None 6.0 ×104* 2.4 ×104 19 22 2.4 ×104 1.6 ×104
 Coal 5.2 ×103 4.7 ×104* 4 11 3.9 ×103 3.2 ×104
 Noncoal 7.5 ×104* 5.4 ×102 15 11 2.9 ×104 5.1 ×102

The emission factors are averages of mean methane flow rate measurements per well (mg⋅hour−1⋅well−1). The corresponding numbers of wells and SEs are shown in the next columns. Coal areas are defined here as wells that overlap with one or more workable coal seams. n/a, not applicable.

*

The three highest emission factors are shown.

The measured plugged wells in coal areas are vented as required by regulations.

Methane Flow Rates over Time.

Repeat measurements of the same abandoned wells conducted 2–10 times (July of 2013 to June of 2015) (SI Appendix, Table S2) show that high emitters (104 mg h−1 well−1) have relatively low coefficients of variation, with values ranging from 0.04 to 0.3 (Fig. 2). This result implies that high emitters are emitting methane at consistent levels over multiple years. The coefficient of variation decreases with increasing methane flow rates, implying that lower emitters are more likely to be influenced by variable factors, such as seasonal impacts and measurement error. We also find that the coefficient of variation is unrelated to the number of repeat measurements (SI Appendix, Fig. S2).

Geochemistry.

The origin of methane from high-emitting wells is predominantly thermogenic, with δ13C-CH4 values ranging from −33 to −45‰ (Fig. 3). [Thermogenic methane typically has δ13C-CH4 values greater than −40 to −50‰, whereas microbial methane typically has δ13C-CH4 values below −50‰ (17, 19, 20); intermediate δ13C-CH4 values, around −50‰, can represent mixed thermogenic and microbial sources.] The ratio of C2−4/C1 confirms the thermogenic source of high emitters, because the ratio ranges from 0.01 to 0.2. [Microbial sources of methane typically have ratios less than 0.0005 (19, 21).] A larger range in both δ13C-CH4 and C2−4/C1 values is observed for oil compared with gas wells, with oil wells more likely to emit methane in the microbial range. We do not observe a strong difference in methane isotopes or hydrocarbon ratios between plugged and unplugged wells, although we find that plugged/vented wells have narrower ranges in δ13C-CH4 and C2−4/C1 values. Wells in coal areas tend to have lower C2−4/C1 ratios, regardless of their plugging status or well type, with ratios ranging from 0.001 to 0.04. For wells (in any area) where both δ13C-CH4 and δ2H-CH4 are analyzed, most are found to be within the thermogenic range for gases associated with oil reservoirs (17).

Fig. 3.

Fig. 3.

Carbon and hydrogen isotopes of methane (δ13C-CH4 and δ2H-CH4), hydrocarbon concentration ratios (C2−4/C1), noble gas data, and methane flow rate data shown colored by well type, circled by plugging status, and marked with green diamond outlines if in a coal area. For repeat measurements, the average of the data for the well is shown. The regions representing thermogenic methane associated and not associated with oil are from ref. 17.

High methane-emitting gas wells are found to have the following noble gas ratios: 3He/4He < 0.10RA (where R/RA is the ratio of 3He to 4He in a sample compared with the ratio of those isotopes in air, and RA nomenclature denotes the 3He/4He ratios of samples with respect to air), 4He/22Ne > 100, and CH4/36Ar > 1,000 (Fig. 3 and SI Appendix, Fig. S4). 4He occurs in very low abundances in the atmosphere and is not produced in association with biogenic methane (22). By comparison, 22Ne and 36Ar are ubiquitous, well-mixed, and uniform in the atmosphere. As a result, the noble gases and specifically, elevated levels of 4He or ratios of thermogenic gases (4He or CH4) to atmospheric gases are able to identify high thermogenic methane-emitting gas wells, which cannot always be achieved with hydrocarbon-based geochemical information alone (23).

Number of Abandoned Wells.

Using comprehensive databases (15, 24) and analysis of historical documents (2528) (SI Appendix), we estimate the number of abandoned wells in Pennsylvania to be between 470,000 and 750,000 (SI Appendix, Table S4). The key difference between our well numbers and previous lower estimates is that we include additional wells drilled for enhanced recovery (ER) purposes (SI Appendix). Similar to oil and gas wells used for production, injection wells drilled for water flooding, a widely used enhanced oil recovery technique (26, 29), can also act as pathways for methane and other fluid migration. The data show that the inclusion of ER wells leads to an increase in estimated well numbers by multiplicative factors of 1.7–3.5. We base our estimate of ER wells using these factors for years before 1950, for which the number of ER wells is unknown. There also are discrepancies among the numerous data sources available in historical documents and modern digital datasets (Fig. 4). We compare the data sources to estimate the potential degree of error, which is included as multiplicative factors of 1.3–1.5 in the upper bound estimate (SI Appendix, Table S4).

Fig. 4.

Fig. 4.

Number of drilled and/or completed oil and gas wells in Pennsylvania from various historical documents and databases (SI Appendix). The thick black lines represent the 1929–2013 data used to estimate the total number of wells (SI Appendix, Table S4, second column). For 1859–1928, we use a total well number provided in ref. 25, and the curves shown here are not used to estimate well numbers.

Methane Emission Estimates.

The emission factors (Table 2) are combined with the number of wells in each well category in the Pennsylvania DEP database (24) (Fig. 5). The methane emissions contributed by gas wells and wells in coal areas are significantly larger than their share in well numbers. Considering each attribute independently, wells in coal areas represent 21% of the DEP database but 72% of the estimated methane emissions; similarly, gas wells represent 32% of the DEP database but 77% of the methane emissions (Fig. 5). Plugged wells, including those that are vented, represent an estimated 74% of the methane emissions, slightly higher than the number for plugged wells (70%) in the DEP database. The DEP database does not distinguish between plugged wells and plugged/vented wells; both are simply categorized as plugged. In our estimate, plugged/vented wells are those that are both plugged and in coal areas, following regulatory requirements in Pennsylvania. Therefore, the methane emissions for all plugged wells (Fig. 5) represent both a large contribution from high methane-emitting plugged/vented gas wells (in coal areas) and a smaller contribution from low methane-emitting plugged wells that are not vented.

Fig. 5.

Fig. 5.

Number of wells in the PA DEP database (Left) and the corresponding relative methane emissions distribution (Right) based on plugging status, coal area designation, and well type. Each of three attributes is considered independently.

Our attribute-based methane emissions estimates for Pennsylvania using improved well numbers range from 0.04 to 0.07 Mt CH4 per year, which correspond to 5–8% of estimated annual anthropogenic methane emissions for 2011 in Pennsylvania (SI Appendix).

Discussion

Methane Emissions.

Well attributes determined for the measured wells in this paper likely remain unavailable for many wells across the United States. Therefore, well attribute estimation studies similar to this analysis may be valuable for many states. For example, West Virginia has at least 57,597 wells that were drilled before 1929 (34% of Pennsylvania wells over the same time period) (25), and records for many wells in the state are likely to be missing. Determining well attributes and numbers is as important as collecting additional measurements for estimating methane emissions. The attributes of high methane-emitting abandoned oil and gas wells identified here as plugging status (P), well type (W), and coal area designation (C) may also be indicative of high emitters elsewhere. In the United States, there are 31 oil-producing states, 33 natural gas-producing states, and 25 coal-producing states (30), with many states simultaneously producing oil, natural gas, and coal. Other well attributes, such as age, wellbore deviation, and operator (12), may also be predictors of methane flow rates. However, we do not explore these attributes here because of a lack of data. Efforts to collect and compile additional well attributes are needed to explore the role of attributes not considered in this study.

The total number of abandoned oil and gas wells remains uncertain in Pennsylvania and across the United States. Documented numbers of wells are more likely to represent lower bounds, because they may not include certain types of wells (e.g., injection wells for ER) and may be missing records. For example, the estimate of 3 million abandoned wells across the United States (4) does not include injection wells drilled for ER or undocumented wells. In addition, our upper limit in the number of abandoned wells in Pennsylvania of 750,000 may also be an underestimate because of uncertainties associated with differences in terminology among databases and the accuracy of modern digital databases, even in recent records (SI Appendix).

The uncertainties associated with well numbers may be addressed through the application of well-finding technologies (31), field verifications, and database updates. These activities can also help estimate well attributes. In addition, more field measurements of methane emissions are needed from abandoned wells with different attributes and in other geographical locations (i.e., states and countries) to reduce uncertainties in emission factors (32) (Table 2).

Mitigation.

Targeting high emitters will lower mitigation costs per unit of methane emissions avoided. The identification of abandoned conventional gas wells and plugged/vented gas wells as the highest emitters allows government agencies to prioritize gas fields and coal areas in their mitigation efforts. Furthermore, explicit categorization of plugged/vented wells, which are found to be high emitters, in state databases may be useful. In addition to database analysis, noble gases, specifically low 3He/4He and high 4He/22Ne ratios, provide an independent approach to identify attributes of high methane-emitting abandoned wells.

Because abandoned wells emit methane continuously, over multiple years and presumably many decades, mitigating their emissions will have a larger apparent benefit when longer time periods are considered. Our multiyear measurements show that the high emitters are likely to emit methane at consistently high levels. Such wells may have been emitting at these levels for many decades and will likely continue for decades into the future. A comparison of the benefits of methane emissions reductions from abandoned wells with reductions from intermittent, short-term sources, such as unconventional oil/gas well development, should be performed using emissions integrated over many years.

Well plugging, which is currently viewed as the main mitigation solution (5, 10), does not guarantee a reduction in methane emissions. Plugging was required originally to protect oil and gas reservoirs, reduce risks of explosions, and more recently, protect groundwater. Plugged wells that are vented, as required by regulations in coal areas in Pennsylvania, are very likely to be high emitters. There are many oil- and gas-producing states with geographically extensive coal layers (e.g., Colorado, Illinois, Indiana, Kentucky, Ohio, Oklahoma, Pennsylvania, West Virginia, and Wyoming). These states have special decommissioning or plugging requirements for coal areas (10). States that require venting in coal areas may want to consider alternatives that ensure safety while reducing methane emissions.

Conclusions

High methane-emitting abandoned wells are found to be unplugged gas wells in noncoal areas and plugged but vented gas wells in coal areas, and they seem to be unrelated to the presence of underground natural gas storage areas or unconventional oil/gas production. The identification of these high emitters provides an opportunity to target mitigation efforts and reduce mitigation costs.

Our attribute-based estimate of 5–8% of estimated annual anthropogenic methane emissions in Pennsylvania is higher than previous estimates, which were based on a single emission factor for all wells and a smaller well count (3, 8, 15). The methane flow rates characterized by well attributes may provide insight into potential emissions outside of Pennsylvania in the 33 oil- and gas-producing US states and other oil- and gas-producing countries. Using the analysis framework presented here, scientists and policymakers can better estimate methane emissions and develop cost-effective mitigation strategies for the millions of abandoned oil and gas wells across the United States and abroad.

Materials and Methods

Well Attributes and Numbers.

To determine attributes of the measured wells and estimate the number of abandoned oil and gas wells, we combine information from different types of data sources: historical documents, published literature, field investigations, and state databases. Historical documents include Pennsylvania agency reports (2628) and books (25, 33). State databases, including geospatial data, were obtained from the Pennsylvania Department of Conservation and Natural Resources (DCNR) (34) and the Pennsylvania DEP (24), agencies that emerged in 1995 from the Pennsylvania Department of Environmental Resources (DER). We combine and analyze the information to estimate attributes of measured wells based mainly on their location with respect to nearby or overlying oil/gas wells, pools, and fields with attributes in the DCNR database. The attributes determined are depth (d), coal area designation (C), plugging status (P), well type (W), distance to nearest natural gas storage field (rS), and distance to nearest unconventional oil and gas well (rU). To estimate the number of abandoned wells, we sum the number of wells drilled annually compiled from multiple sources (15, 24, 25, 27, 28, 33, 35) and subtract the number of active wells from the total (24). We include wells drilled for ER purposes and estimate missing well numbers by scaling available well and production data. We also compare data sources to quantify uncertainties in well numbers. Details on the attribute estimation methodology and the well number estimation are provided in SI Appendix, SI Materials and Methods.

Field and Laboratory Methods.

The measurements of methane flow rates and light hydrocarbon (ethane, propane, and n-butane) concentrations (January, March, and June of 2015 samples) followed methods presented in ref. 3. The measurements were performed across seven counties in Pennsylvania (SI Appendix, Table S2). The measurements of methane isotopes were performed at Princeton University (3, 36) and Lawrence Berkeley National Laboratory (LBNL). At LBNL, we also analyzed hydrogen isotopes of methane if concentrations were sufficiently high (1,200 ppmv). For October of 2014 and January, March, and June of 2015, we analyzed the samples for the following noble gases, He, Ne, and Ar, at Ohio State University following methods presented in ref. 22. Additional information on the field sampling and the analysis procedures is provided in SI Appendix, SI Materials and Methods.

Multilinear Regression.

We perform a multilinear regression using the following linear model expressed in Wilkinson notation (37):

lnm˙1+d+C+P+W+rS+rU. [1]

Note that the categorical variables, C, P, and W, are denoted using uppercase letters. Multilinear regression is also performed on other linear models, which are summarized in SI Appendix, SI Materials and Methods.

Methane Emission Estimates.

Based on the multilinear regression results, we use C, P, and W as the key attributes for methane emission estimation:

Eabandonedwells=wpcEFw,p,cnw,p,c, [2]

where E is the total methane emissions, EF is the emission factor, n is the number of wells, and subscripts w, p, and c represent the appropriate values of W, P, and C, respectively. We consider two well types (w = oil or combined oil & gas and gas), two plugging statuses (P = plugged and unplugged), and two coal area designations (c = coal and noncoal area). We use the Pennsylvania DEP’s wells database (24) and the above attributes to determine the proportion of wells in each category. Additional details, including discussions on uncertainties, are given in SI Appendix, SI Materials and Methods.

Supplementary Material

Supplementary File
pnas.1605913113.sapp.pdf (501.6KB, pdf)

Acknowledgments

We thank the Stanford Natural Gas Initiative, Princeton University, the Andlinger Center for Energy and the Environment, Stanford University, and the Precourt Institute for Energy. We also thank Venango Senior Environmental Corps (John and Ev Kolojejchick, Charlie, and Steve), Clearfield Senior Environmental Corps (Lyle Milland and Rick and Marianne Atkinson), Save Our Streams PA, Joann Parrick, Joe and Cheryl Thomas, Bill Peiffer, Camille Sage Lagron, and Bo Guo for help in the field. For valuable field, laboratory, and planning assistance, we thank David Pal, Ryan Edwards, Ashwin Venkatramen, Matthew Reid, Ejeong Baik, Christianese Kaiser, Eugene Cho, Daniel Ma, Kenneth Campbell, Colin J. Whyte, Myles Moore, and Ben Grove. For assistance in the laboratory and/or helpful comments, we thank Peter Jaffe, Tullis Onstott, Maggie Lau, Tsering W. Shawa, Joseph Vocaturo, Harmony Lu, Eric Lebel, Kristin Boye, and Scott Fendorf. Finally, we thank the PA DEP (Stewart Beattie, Scott Perry, Seth Pelepko, and John Quigley) for providing assistance with obtaining data and helpful insights on the data. We acknowledge National Oceanic and Atmospheric Administration Grant NA140AR4310131, the Princeton Environmental Institute, and Vulcan Inc. for supporting this research.

Footnotes

The authors declare no conflict of interest.

This article is a PNAS Direct Submission.

This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1605913113/-/DCSupplemental.

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