Substantial amounts of iron are present in many subsurface environments. This element has a significant effect on both the biogeochemical cycling of carbon and the fate and transport of trace environmental contaminants, because it is readily transformed among several reactive species. The interactions of subsurface iron with various naturally occurring bacteria have a major influence on its environmental impacts, but these interactions are not well understood. Scientists at Argonne National Laboratory and three partner universities have identified a key role for sulfur in how bacteria affect the speciation of subsurface iron. They determined that bacteria unable to reduce ferric iron directly under alkaline conditions can do so indirectly. The bacteria do this by reducing elemental sulfur to sulfide ion, which then reduces the ferric iron in the goethite to ferrous iron. In addition, this ferrous iron can reduce other metal species such as uranyl ion, thus affecting their solubility. The researchers determined that this process is common in alkaline environments such aquifers, especially those in arid regions. This new understanding of this environmental role of iron will enable progress in a wide range of areas, from modeling of potential carbon capture systems to understanding speciation of contaminants such as uranium and arsenic.
References: Flynn, T. M., E. J. O’Loughlin, B. Mishra, T. J. DiChristina, and K. M. Kemner. 2014. “Sulfur-Mediated Electron Shuttling During Bacterial Iron Reduction,”, Science 344, 1039-42. DOI: 10.1126/science.1252066. (Reference link)
Friedrich, M. W., and K. W. Finster. 2014. “How Sulfur Beats Iron,” Science 344, 974-75. DOI: 10.1126/science.1255442. (Reference link)
Contact: Roland F. Hirsch, SC-23.2, email@example.com, 301-903-9009.
SC-33.1 Earth and Environmental Sciences Division, BER
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