4.7 Article

Hydrogeochemistry and coal-associated bacterial populations from a methanogenic coal bed

Journal

INTERNATIONAL JOURNAL OF COAL GEOLOGY
Volume 162, Issue -, Pages 14-26

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.coal.2016.05.001

Keywords

Powder River Basin; Coalbed methane; Microbial enhanced CBM (MECoM) technology; Test site; Biosurfactant; Hydrology; Hydrogeochemistry

Funding

  1. U.S. Geological Survey Energy Resources Program
  2. Department of Energy [DE-FE0026155]
  3. DOE ZERT Program [DE-FC26-04NT42262]
  4. U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research, Genomics: GTL Foundational Science [DE-AC02-05CH11231]
  5. NSF [EAR-1322805]
  6. Division Of Earth Sciences
  7. Directorate For Geosciences [1322805] Funding Source: National Science Foundation
  8. Division Of Earth Sciences
  9. Directorate For Geosciences [1322795] Funding Source: National Science Foundation

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Biogenic coalbed methane (CBM), a microbially-generated source of natural gas trapped within coal beds, is an important energy resource in many countries. Specific bacterial populations and enzymes involved in coal degradation, the potential rate-limiting step of CBM formation, are relatively unknown. The U.S. Geological Survey (USGS) has established a field site, (Birney test site), in an undeveloped area of the Powder River Basin (PRB), with four wells completed in the Flowers-Goodale coal bed, one in the overlying sandstone formation, and four in overlying and underlying coal beds (Knoblach, Nance, and Tenet). The nine wells were positioned to characterize the hydraulic conductivity of the Flowers-Goodale coal bed and were selectively cored to investigate the hydrogeochemistry and microbiology associated with CBM production at the Birney test site. Aquifer-test results indicated the Flowers-Goodale coal bed, in a zone from about 112 to 120 m below land surface at the test site, had very low hydraulic conductivity (0.005 m/d) compared to other PRB coal beds examined. Consistent with microbial methanogenesis, groundwater in the coal bed and overlying sandstone contain dissolved methane (46 mg/L average) with low delta C-13 values (-67%. average), high alkalinity values (22 meq/kg average), relatively positive delta C-13-DIC values (4 parts per thousand average), and no detectable higher chain hydrocarbons, NO3-, or SOi(4)(2-). Bioassay methane production was greatest at the upper interface of the Flowers-Goodale coal bed near the overlying sandstone. Pyrotag analysis identified Aeribacillus as a dominant in situ bacterial community member in the coal near the sandstone and statistical analysis indicated Actinobacteria predominated coal core samples compared to claystone or sandstone cores. These bacteria, which previously have been correlated with hydrocarbon-containing environments such as oil reservoirs, have demonstrated the ability to produce biosurfactants to break down hydrocarbons. Identifying microorganisms involved in coal degradation and the hydrogeochemical conditions that promote their activity is crucial to understanding and improving in situ CBM production, Published by Elsevier B.V.

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