Abstract

Research Article| January 01, 2006 Atomistic Models of OH Defects in Nominally Anhydrous Minerals Kate Wright Kate Wright Nanochemistry Research Institute, Curtin University of Technology, GPO Box 1987, Perth, Western Australia 6845, Australia, e-mail: kate@ivec.org Search for other works by this author on: GSW Google Scholar Author and Article Information Kate Wright Nanochemistry Research Institute, Curtin University of Technology, GPO Box 1987, Perth, Western Australia 6845, Australia, e-mail: kate@ivec.org Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2006) 62 (1): 67–83. https://doi.org/10.2138/rmg.2006.62.4 Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Kate Wright; Atomistic Models of OH Defects in Nominally Anhydrous Minerals. Reviews in Mineralogy and Geochemistry 2006;; 62 (1): 67–83. doi: https://doi.org/10.2138/rmg.2006.62.4 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search The Earth’s upper mantle may contain substantial amounts of water dissolved in nominally anhydrous minerals (NAMs) such as the Mg2SiO4 polymorphs, pyroxenes and garnets. This water, incorporated into the crystal lattice as hydrogen defects, can have a profound influence on the physical properties of the mantle, even when present at low concentrations. An understanding of these defects at the atomic level is therefore of fundamental importance for the development of models of the evolution and dynamics of the Earth’s mantle. The incorporation of hydrogen and its influence on the properties of NAMs has been an active area... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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