HR: 13:40h
AN: H12H-01 [PDF]
TI: Effect of Hydrocarbon Biodegradation on the Low-Frequency Electrical Properties of Unconsolidated
Sediments
AU: * Abdel Aal, G Z
EM: gagv4@umr.edu
AF: University of Missouri-Rolla, Geology and Geophysics Dept.
125 McNutt Hall, Rolla, MO 65401 United States
AU: Atekwana, E A
EM: atekwana@umr.edu
AF: University of Missouri-Rolla, Geology and Geophysics Dept.
125 McNutt Hall, Rolla, MO 65401 United States
AU: Slater, L D
EM: lslater@andromeda.rutgers.edu
AF: Rutgers University, Department of Earth and Environmental Sciences, Rutgers, NJ 07102 United States
AU: Atekwana, E A
EM: eliota@umr.edu
AF: University of Missouri-Rolla, Geology and Geophysics Dept.
125 McNutt Hall, Rolla, MO 65401 United States
AB:
A laboratory sand column experiment was conducted to investigate the effect of biodegradation of diesel on low-frequency
electrical measurements over a period of 36 weeks. Uniform fine to medium grained sands were used in the columns with the
following experimental treatments: nutrients; nutrients + diesel; nutrients + diesel + bacteria. The first two columns were
kept sterile by adding 200 mg/l mercury chloride, whereas the third column was kept active. Spectral electrical measurements
were conducted in the frequency range 0.1 to 1000 Hz biweekly for the first twenty weeks and monthly for the duration of the
experiment. Evidence of biodegradation in the active column was determined by monitoring the changes in concentration of
terminal electron acceptors (e.g., nitrate and sulfate) and total benzene, toluene, ethylbenzene and xylene (BTEX).
After 36 weeks, we observed in general that the active column exhibited major changes in electrical and geochemical
parameters compared to sterile columns. The active column showed about 100 and 120 percent increase in the magnitude of the
real and imaginary conductivities, respectively. No significant increases in the real and imaginary conductivity were
observed in the sterile columns. We note that, (a) the relative increase in the real conductivity exceeded the relative
increase in the fluid conductivity, and (b) the relative increase in the imaginary conductivity (polarization) exceeded the
relative increase in the real conductivity. The active column further showed 70 to 90 percent depletion in nitrate, sulfate
and BTEX concentrations. Moreover, magnesium and calcium concentrations increased within the active column to about 120
to160 percent (respectively) compared to the sterile column. The major biogeochemical changes associated with the active
column are an indication of active microbial degradation of diesel. Moreover, the increase in calcium and magnesium ion
concentrations in the active column, concurrent with a decrease in pH is indicative of mineral weathering accompanying the
degradation process.
Based on the geochemical analyses and the electrical parameters, we argue that microbial alteration of surface chemistry
(increase of surface charge density and ionic mobility) at the mineral-fluid interface, coupled with increases in the
electrical conductivity of the electrolyte, explain our observations in the active column. We conclude from this study that
low-frequency electrical measurements have the potential to monitor the biogeochemical and physical changes of hydrocarbon
contaminated soils undergoing biodegradation.
DE: 1615 Biogeochemical processes (4805)
DE: 3914 Electrical properties
DE: 4803 Bacteria
DE: 4815 Ecosystems, structure and dynamics
DE: 4854 Physicochemical properties
SC: Hydrology [H]
MN: 2003 Fall Meeting