Influences of Electron Donor, Bicarbonate, and Sulfate on Bioreduction Processes and Manganese/Copper Redistributions among Minerals in a Water-Saturated Sediment

Bioreduction processes have profound influences on mobility and bioavailability of metals in soils and sediments. In this study, a series of microcosm studies were conducted to investigate bioreduction progresses (ferric iron and sulfate reduction) and their influences on manganese and copper element redistributions with the change of microbial community under various geochemical conditions. Results indicated that ethanol stimulated higher rates of bioreduction processes than acetate did. High-concentration bicarbonate and sulfate addition inhibited iron reduction but not sulfate reduction. Sequential extraction revealed that the exchangeable and carbonate bonding-iron were increased in ethanol amendment, whereas those of copper were decreased. The elevated bicarbonate concentration and sulfate addition both influenced the mobility and redistribution of metals. 16S rRNA analysis indicated that ethanol amendment stimulated the growths of microbial iron and sulfate reducer. A high concentration of bicarbonate suppressed the growth of iron reducer Geobacteraceae, but showed limited effect on sulfate reducers. This study concluded that geochemical conditions such as electron donor, bicarbonate and sulfate concentration influenced the microbial community and led to changes in bioreduction processes and metal distributions in the anerobic sediments.