Effect of Water on the Equation of State of Nominally Anhydrous Minerals

Research Article| January 01, 2006 Effect of Water on the Equation of State of Nominally Anhydrous Minerals Steven D. Jacobsen Steven D. Jacobsen Department of Geological Sciences Northwestern University Evanston, Illinois, 60208, U.S.A., e-mail: steven@earth.northwestern.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Steven D. Jacobsen Department of Geological Sciences Northwestern University Evanston, Illinois, 60208, U.S.A., e-mail: steven@earth.northwestern.edu Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2006) 62 (1): 321–342. https://doi.org/10.2138/rmg.2006.62.14 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 Steven D. Jacobsen; Effect of Water on the Equation of State of Nominally Anhydrous Minerals. Reviews in Mineralogy and Geochemistry 2006;; 62 (1): 321–342. doi: https://doi.org/10.2138/rmg.2006.62.14 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 It is possible that the majority of Earth's H2O budget is present as hydroxyl (OH) structurally incorporated into the major nominally anhydrous minerals (NAMs) of the mantle (e.g., Martin and Donnay 1972). Ringwood (1966) thought as much as five times the surface H2O-mass could be present in the mantle, amounting to ~0.2 wt% H2O if distributed throughout the entire mantle (Harris and Middlemost 1969). We know now the (Mg,Fe)2SiO4 polymorphs of the upper mantle and transition zone can incorporate up to several weight percent of water in their... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.