Field Evidence for Geophysical Detection of Subsurface Zones of Enhanced Microbial Activity
Geochemical data from closely spaced vertical intervals in a hydrocarbon-impacted aquifer were used to assess the relationship between bulk conductivity and zones of enhanced microbial activity. The bulk conductivity was measured using in situ vertical resistivity probes. Microbial activity was verified using terminal electron acceptors (nitrate, sulfate, iron, and manganese), dissolved inorganic carbon (DIC), and major ion chemistry. Peaks in bulk conductivity in the aquifer overlapped with zones where nitrates and sulfates were depleted, total petroleum hydrocarbon, iron, manganese, dissolved ions, and DIC were elevated, suggesting a link between higher electrical conductivity and zones of enhanced microbial activity stimulated by the presence of hydrocarbon. Thus the subsurface expression of microbial activity is apparently recorded in the bulk conductivity measurements. Our results argue for combining geophysics with biogeochemistry studies to delineate subsurface zones of enhanced microbial activity.
E. A. Atekwana et al., "Field Evidence for Geophysical Detection of Subsurface Zones of Enhanced Microbial Activity," Geophysical Research Letters, American Geophysical Union (AGU), Jan 2004.
The definitive version is available at http://dx.doi.org/10.1029/2004GL021576
Geosciences and Geological and Petroleum Engineering
Keywords and Phrases
Downhole Methods; Groundwater Quality; Magnetic and Electrical Methods; Magnetic and Electrical Properties
Article - Journal
© 2004 American Geophysical Union (AGU), All rights reserved.