Evaluation of Methane Sources in Groundwater in Northeastern Pennsylvania

Testing of 1701 water wells in northeastern Pennsylvania shows that methane is ubiquitous in groundwater, with higher concentrations observed in valleys vs. upland areas and in association with calcium‐sodium‐bicarbonate, sodium‐bicarbonate, and sodium‐chloride rich waters—indicating that, on a regi...

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Bibliographic Details
Published inGround water Vol. 51; no. 3; pp. 333 - 349
Main Authors Molofsky, Lisa J., Connor, John A., Wylie, Albert S., Wagner, Tom, Farhat, Shahla K.
Format Journal Article
LanguageEnglish
Published Malden, US Blackwell Publishing Ltd 01.05.2013
Ground Water Publishing Company
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Summary:Testing of 1701 water wells in northeastern Pennsylvania shows that methane is ubiquitous in groundwater, with higher concentrations observed in valleys vs. upland areas and in association with calcium‐sodium‐bicarbonate, sodium‐bicarbonate, and sodium‐chloride rich waters—indicating that, on a regional scale, methane concentrations are best correlated to topographic and hydrogeologic features, rather than shale‐gas extraction. In addition, our assessment of isotopic and molecular analyses of hydrocarbon gases in the Dimock Township suggest that gases present in local water wells are most consistent with Middle and Upper Devonian gases sampled in the annular spaces of local gas wells, as opposed to Marcellus Production gas. Combined, these findings suggest that the methane concentrations in Susquehanna County water wells can be explained without the migration of Marcellus shale gas through fractures, an observation that has important implications for understanding the nature of risks associated with shale‐gas extraction.
Bibliography:istex:DE8C5FBE89A8329FB3762255D19515C3B30DA555
ArticleID:GWAT12056
Appendix S1. Supporting Information for L.J. Molofsky et al. (2013).Table S8. Groundwater Quality Data for 1701 Water Well Samples from Susquehanna County, Pennsylvania
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GSI Environmental Inc.
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0017-467X
1745-6584
DOI:10.1111/gwat.12056