|Torkzaban, Saeed - UC, RIVERSIDE|
|Tazehkand, Shiva - UTRECHT UNIV, NETHERLANDS|
|Walker, Sharon - UC, RIVERSIDE|
Submitted to: Water Resources Research
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: January 11, 2008
Publication Date: April 5, 2008
Repository URL: http://www.ars.usda.gov/SP2UserFiles/Place/53102000/pdf_pubs/P2201.pdf
Citation: Torkzaban, S., Tazehkand, S.S., Walker, S.L., Bradford, S.A. 2008. Transport and Fate of Bacteria in Porous Media: Coupled Effects of Chemical Conditions and Pore Space Geometry. Water Resources Research. Vol 44:1-12 Interpretive Summary: Studies were undertaken to better understand the factors that control the transport and fate of bacteria in soil. Experimental results indicate that bacteria retention in soils depend on both the chemistry of the system, and the configuration of the soil grains. Detailed simulations of water flow around several soil grains revealed that “immobile” regions occur in small pore spaces that are formed when soil grains contact each other. The number of bacteria that will be transported to these immobile regions is theoretically dependent on the chemistry of the system. Once the bacteria become trapped in these immobile regions, changes in the chemistry will not release them.
Technical Abstract: Experimental and theoretical studies were undertaken to explore the coupling effects of chemical conditions and pore space geometry on bacteria transport in porous media. The retention of Escherichia coli D21g was investigated in a series of batch and column experiments with solutions of different ionic strength (IS) and ultra pure quartz sand. DLVO calculations and results from batch experiments suggested that bacteria attachment to the sand surface was negligible when the IS was less than or equal to 50 mM. Breakthrough data from column experiments showed significant cell retention was strongly depending on the IS. This finding indicates that cell retention was dependent on the depth of the secondary energy minimum which increased with IS. When the IS of the influent solution was decreased to 1mM only a small fraction of the retained bacteria were released from the column. The remaining retained bacteria, however, were recovered from the sand that was excavated from the column and then placed in excess amounts of solution having the original IS. These observations suggest that the solution chemistry is not the only mechanism controlling bacteria retention in the porous media. Computational simulations of flow around several collector grains revealed another retention mechanism, which is dependent on both the solution chemistry and the pore space geometry. Simulations demonstrate that the pore space geometry created low velocity regions. The number of bacterial cells that may be transported to these relatively “immobile” regions will theoretically be dependent on the depth of the secondary energy minimum (the IS). Once the bacteria are trapped in these immobile regions, reduction of the secondary energy minimum does not necessarily release them due to hydrodynamic constraints.