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ReviewNanominerals, Mineral Nanoparticles, and Earth Systems
Minerals are more complex than previously thought because of the discovery that their chemical properties vary as a function of particle size when smaller, in at least one dimension, than a few nanometers, to perhaps as much as several tens of nanometers. These variations are most likely due, at least in part, to differences in surface and near-surface atomic structure, as well as crystal shape and surface topography as a function of size in this smallest of size regimes. It has now been established that these variations may make a difference in important geochemical and biogeochemical reactions and kinetics. This recognition is broadening and enriching our view of how minerals influence the hydrosphere, pedosphere, biosphere, and atmosphere.
1 Center for NanoBioEarth, Department of Geosciences, Virginia Polytechnic Institute and State University (Virginia Tech), Blacksburg, VA 24061–0420, USA.
2 School of Earth Sciences and School of Environment and Natural Resources, Ohio State University, Columbus, OH 43210, USA. 3 Department of Civil Engineering and Geological Sciences, University of Notre Dame, Notre Dame, IN 46556, USA. 4 Department of Chemistry, University of Minnesota, Minneapolis, MN 55455, USA. 5 Department of Geology and Geophysics, University of Wisconsin-Madison, Madison, WI 53706–1692, USA. 6 Center for Critical Zone Research, Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19717–1303, USA. 7 Department of Chemistry and Biochemistry, University of South Carolina, Columbia, SC 29208, USA. * To whom correspondence should be addressed. E-mail: hochella{at}vt.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)