Differentiating Between Biogenic And Thermogenic Sources Of Natural Gas In Coalbed Methane Reservoirs From The Illinois Basin Using Noble Gas And Hydrocarbon Geochemistry

While coalbed methane (CBM) is a significant source of natural gas production globally, uncertainties regarding the proportions of biogenic and thermogenic natural gas in CBM reservoirs still remain. We integrate major gases, hydrocarbon composition, hydrocarbon stable isotopes and noble gases in fluids from 20 producing CBM wells to more accurately constrain the genetic source of natural gases in the eastern Illinois Basin, USA. Previous studies have indicated primarily biogenic production of methane (>99.6%) with negligible contributions from thermogenic natural gases. However, by integrating noble gases, we identify quantifiable (up to 19.2%) contributions of exogenous thermogenic gas in produced gases from the Seelyville and Springfield coal seams. Thermogenic gases are distinguished by a positive relationship between methane, ethane and helium-4, lower C-1/C-2+, heavier delta C-13-CH4, more radiogenic noble gases (He-4, Ne-21(*), Ar-40(*)), and lower abundances of atmospherically derived gases (Ne-20, Ar-36). Biogenic gases displayed lighter delta C-13-CH4, higher C-1/C-2+, higher levels of atmospheric gases and lower abundances of radiogenic noble gases. Our data suggest that natural gases from a deeper, exogenous thermogenic source likely migrated to the Pennsylvanian-aged coals at an unknown time and later mixed with biogenic methane diluting the geochemical signature of the thermogenic methane within the Springfield and Seelyville coal seams.