Relaxation behavior in low-frequency complex conductivity of sands caused by bacterial growth and biofilm formation by Shewanella oneidensis under a high-salinity condition

Journal Article · 01 November 2021 · Geophysics

DOI: https://doi.org/10.1190/geo2020-0213.1 · OSTI ID:1823486

Joo, Hyun-Woo  ^[1]; Kwon, Tae-Hyuk  ^[1]; Lee, Seung-Rae ^[1]; Wu, Yuxin  ^[2]

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1. Korea Advanced Institute of Science and Technology (KAIST), Civil and Environmental Engineering, Daejeon 34141, Republic of Korea.(corresponding author), .
2. Earth and Environmental Sciences, Lawrence Berkeley National Laboratory (LBNL), Berkeley, California 94720, USA..

Complex electrical conductivity is increasingly used to monitor subsurface processes associated with microbial activities because microbial cells mostly have surface charges and thus electrical double layers. Although highly saline environments are frequently encountered in coastal and marine sediments, there are limited data available on the complex conductivity associated with microbial activities under a high-salinity condition. Therefore, we have developed the spectral responses of complex conductivity of sand associated with bacterial growth and biofilm formation under a highly saline condition of approximately 1% salinity and approximately 2 S/m pore water conductivity with an emphasis on relaxation behavior. A column test is performed, in which the model bacteria Shewanella oneidensis MR-1 are stimulated for cell growth and biofilm formation in a sand pack, whereas the complex conductivity is monitored from 0.01 Hz to 10 kHz. The test results indicate that the real conductivity increases in the early stage due to the microbial metabolites and the increased surface conduction with cell growth but soon begin to decrease because of the reduction of charge passages due to bioclogging. However, the imaginary conductivity significantly increases with time, and clear bell-shaped relaxation behaviors are observed with the peak frequency of 0.1–1 Hz, associated with the double-layer polarization of cells and electrically conductive pili and biofilms. The Cole-Cole relaxation model appears to capture such relaxation behaviors well, and the modeling results indicate gradual increases in normalized chargeability and decreases in relaxation time during bacterial growth and biofilm formation in the highly saline condition. Comparison with previous literature confirms that the high-salinity condition further increases the normalized chargeability, whereas it suppresses the phase shift and thus the imaginary conductivity. Our results suggest that the complex conductivity can effectively capture microbial biomass formation in sands under a highly saline condition.

• Sponsoring Organization: USDOE
• Grant/Contract Number: AC02-05CH11231
• OSTI ID: 1823486
• Journal Information: Geophysics, Journal Name: Geophysics Journal Issue: 6 Vol. 86; ISSN 0016-8033
• Publisher: Society of Exploration GeophysicistsCopyright Statement
• Country of Publication: United States
• Language: English