Article ID Journal Published Year Pages File Type
9529158 Chemical Geology 2005 13 Pages PDF
Abstract
The results of the experiments conducted in oversaturated conditions demonstrate that bacteria significantly enhance the rate and extent of Fe removal from solution relative to the bacteria-free controls. We use the results of the separate batch adsorption experiments to determine stability constants for Fe-bacteria surface complexes assuming zero precipitation at these low Fe, low pH conditions. The observed increase in Fe removed in the presence of bacteria in 'oversaturated' conditions can be accounted for by adsorption only, using a surface model based on the reaction:Fe3++R>L1−↔R>L1Fe2+ log K=6.1±0.4where R>L1− represents the deprotonated form of the bacterial surface functional group with a pKa value of 3.3. The stability of the Fe-bacteria sorption reaction is orders of magnitude stronger than that observed for the other metal-bacteria systems, emphasizing the importance of Fe(III) adsorption in bacteria-bearing systems. Some Fe removal by the bacteria was irreversible on the time scale of our experiments, indicating that, although adsorption has the potential to account for the observed Fe removal, the process is likely more complicated than simple metal adsorption onto bacterial cell wall functional groups.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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