DISSOLVED GAS GEOCHEMISTRY OF SHALLOW GROUNDWATER SYSTEMS IN PENNSYLVANIA AND NEW YORK, ASSOCIATED WITH NATURAL GAS EXTRACTION
Methane was detected in approximately 85% of homeowner water wells regardless of gas industry operations. However, the dissolved methane concentrations were 17.4 times higher on average in active extraction areas (19.2 mg/L; n=26) than in non-active gas extraction areas (1.1 mg/L; n=34). The higher chain hydrocarbons (ethane, propane, and butane) were detected more often in active areas (21, 8, and 3, respectively) compared to non-active areas (3, 0, and 0, respectively), indicating a more thermogenic methane character. The carbon isotope values of methane (δ13C-CH4), in active extraction areas were on average less negative (-37±7 ‰) than non-active extraction areas (-54±11‰). We conclude from these and other results that there are important differences in methane concentration, natural gas composition, and δ13C-CH4 values in shallow groundwater wells between active and non-active natural gas extraction areas. Furthermore, the dissolved gas geochemistry in active extraction areas is consistent with a more thermally mature source of organic matter, whereas the dissolved gas in shallow ground water from non-active extraction areas tends to be more mixed biogenic/thermogenic in character. Results from additional sampling in 2011 will also be presented.