GC51F-1149
Source and Cycling of Trace Metals and Nutrients in a Microbial Coalbed Methane System

Friday, 18 December 2015
Poster Hall (Moscone South)
Marisa Melody Earll1, Elliott Paul Barnhart2, Dan Ritter1, David S Vinson3, William H Orem4, Avner Vengosh5 and Jennifer C McIntosh1, (1)University of Arizona, Tucson, AZ, United States, (2)Organization Not Listed, Washington, DC, United States, (3)University of North Carolina at Charlotte, Charlotte, NC, United States, (4)USGS Headquarters, Reston, VA, United States, (5)Duke University, Durham, NC, United States
Abstract:
The source and cycling of trace metals and nutrients in coalbed methane (CBM) systems are controlled by both geochemical processes, such as dissolution or precipitation, and biological mediation by microbial communities. CBM production by the microbes is influenced by trace metals and macronutrients such as nitrogen (N) and phosphate (P). Previous studies have shown the importance of these nutrients to both enhance and inhibit methane production; however, it’s not clear whether they are sourced from coal via in-situ biodegradation of organic matter or transported into the seams with groundwater recharge. To address this knowledge gap, trace metal and nutrient geochemistry and the organic content of solid coal and associated groundwater will be investigated across a hydrologic gradient in CBM wells in the Powder River Basin, MT. Sequential dissolution experiments (chemical extraction of organic and inorganic constituents) using 8 core samples of coal and sandstone will provide insight into the presence of trace metals and nutrients in coalbeds, the associated minerals present, and their mobilization. If significant concentrations of N, P, and trace metals are present in core samples, in-situ sourcing of nutrients by microbes is highly probable. The biogeochemical evolution of groundwater, as it relates to trace metal and nutrient cycling by microbial consortia, will be investigated by targeting core-associated coal seams from shallow wells in recharge areas to depths of at least 165 m and across a 28 m vertical profile that include overburden, coal, and underburden. If microbial-limiting trace metals and nutrients are transported into coal seams with groundwater recharge, we would expect to see higher concentrations of trace metals and nutrients in recharge areas compared to deeper coalbeds. The results of this study will provide novel understanding of where trace metals and nutrients are sourced and how they are cycled in CBM systems.