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American Mineralogist; July 2004; v. 89; no. 7; p. 969-975
© 2004 Mineralogical Society of America
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Neutron and synchrotron X-ray diffraction study of the structures and dehydration behaviors of ramsdellite and "groutellite"

Jeffrey E. Post1,* and Peter J. Heaney2

1 Department of Mineral Sciences, Smithsonian Institution, Washington, D.C. 20560-0119, U.S.A.
2 Department of Geosciences, 309 Deike, Pennsylvania State University, University Park, Pennsylvania 16802, U.S.A.

Correspondence: * E-mail: post.jeffrey{at}nmnh.si.edu

The crystal structure of ramsdellite, MnO2, was refined using time-of-flight powder neutron diffraction data and the Rietveld method in order to assess the effects of reduction in cathodic battery materials. For the first time, we present a refined structure for "groutellite," a heretofore poorly characterized phase with ideal formula O1.5(OH)0.5. "Groutellite" is generated synthetically as an intermediate compound during the reduction of ramsdellite to groutite (MnOOH), and it also occurs as an intergrowth in certain natural specimens of ramsdellite. The Jahn-Teller distortions in "groutellite" are confined to the a–c plane, and they result in a 6.8% unit-cell volume increase relative to ramsdellite. The Mn—O bond lengths refined for "groutellite" are consistent with the replacement of half of the Mn4+ and O2– in ramsdellite by Mn3+ and (OH)–, respectively. In addition, the high-temperature behaviors of ramsdellite and "groutellite" were investigated by temperature-resolved synchrotron powder X-ray diffraction from 298 to 720 K. Rietveld refinements revealed a gradual thermal expansion of the groutellite structure to ~450 K. At higher temperatures, the unit-cell volume gradually decreased, primarily as a result of a decrease in c.




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