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1 Stanford Synchrotron Radiation Lightsource
2575 Sand Hill Road, MS 69,
Menlo Park, CA 94025, USA
E-mail:
bargar{at}slac.stanford.edu
2 Environmental Microbiology Laboratory, Ecole
Polytechnique
Fédérale de Lausanne, 1015 Lausanne,
Switzerland
E-mail:
rizlan.bernier-latmani{at}epfl.ch
3 Department of Energy, Environmental and Chemical Engineering
Washington
University, 1 Brookings Drive
Campus Box 1180, St. Louis, MO 63130,
USA
E-mail:
giammar{at}wustl.edu
4 Division of Environmental and Biomolecular Systems
Oregon Health &
Science University, 20000 NW Walker Rd.
Beaverton, OR 97006, USA
E-mail:
tebo{at}ebs.ogi.edu
Biogenic uraninite is of interest to geoscientists for its importance to bioremediation strategies, remarkably small particle size, and biological origin. Recent studies have begun to illuminate the chemical/structural complexities of this important natural nanomaterial. Intriguingly, in spite of its incredibly diminutive size, the molecular-scale structure, energetics, and surface-area-normalized dissolution rates of hydrated biogenic uraninite appear to be similar to those of coarser-particle, abiotic, stoichiometric UO2. These findings have important implications for the role of size as a moderator of nanoparticle aqueous reactivity and for the bioremediation of subsurface U(VI) contamination.
KEYWORDS: uraninite, biogenic uraninite, microbial uranium reduction, bioremediation, dissolution, EXAFS
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