The Structure of Hydrous Species in Nominally Anhydrous Minerals: Information from Polarized IR Spectroscopy

Research Article| January 01, 2006 The Structure of Hydrous Species in Nominally Anhydrous Minerals: Information from Polarized IR Spectroscopy Eugen Libowitzky; Eugen Libowitzky Institut für Mineralogie und Kristallographie Universität Wien - Geozentrum Althanstraße 14, A-1090 Wien, Austria, eugen.libowitzky@univie.ac.at, anton.beran@univie.ac.at Search for other works by this author on: GSW Google Scholar Anton Beran Anton Beran Institut für Mineralogie und Kristallographie Universität Wien - Geozentrum Althanstraße 14, A-1090 Wien, Austria, eugen.libowitzky@univie.ac.at, anton.beran@univie.ac.at Search for other works by this author on: GSW Google Scholar Author and Article Information Eugen Libowitzky Institut für Mineralogie und Kristallographie Universität Wien - Geozentrum Althanstraße 14, A-1090 Wien, Austria, eugen.libowitzky@univie.ac.at, anton.beran@univie.ac.at Anton Beran Institut für Mineralogie und Kristallographie Universität Wien - Geozentrum Althanstraße 14, A-1090 Wien, Austria, eugen.libowitzky@univie.ac.at, anton.beran@univie.ac.at Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2006) 62 (1): 29–52. https://doi.org/10.2138/rmg.2006.62.2 Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Eugen Libowitzky, Anton Beran; The Structure of Hydrous Species in Nominally Anhydrous Minerals: Information from Polarized IR Spectroscopy. Reviews in Mineralogy and Geochemistry 2006;; 62 (1): 29–52. doi: https://doi.org/10.2138/rmg.2006.62.2 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 Hydrogen is a major constituent in a wide variety of minerals in the Earth’s crust. Usually H is bonded to oxygen forming H2O molecules or OH− groups. In rare cases, H3O+, H3O2− and H5O2+ units are also formed. The occurrence of NH4+, CHx, etc. in minerals will not be considered here. Hydrogen occurs stoichiometrically in hydrous compounds such as hydrates (e.g., gypsum), (oxy)hydroxides (e.g., goethite), and in many rock-forming silicates (e.g., micas), as well as in nonstoichiometric major amounts in... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.