Thermodynamics of Water Solubility and Partitioning

Research Article| January 01, 2006 Thermodynamics of Water Solubility and Partitioning Hans Keppler; Hans Keppler Bayerisches Geoinstitut Universität Bayreuth 95440 Bayreuth, Germany, e-mail: Hans.Keppler@uni-bayreuth.de Search for other works by this author on: GSW Google Scholar Nathalie Bolfan-Casanova Nathalie Bolfan-Casanova Laboratoire Magmas et Volcans - CNRS UMR 6524 63038 Clermont-Ferrand cedex, France, e-mail: N.Bolfan@opgc.univ-bpclermont.fr Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2006) 62 (1): 193–230. https://doi.org/10.2138/rmg.2006.62.9 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 Hans Keppler, Nathalie Bolfan-Casanova; Thermodynamics of Water Solubility and Partitioning. Reviews in Mineralogy and Geochemistry 2006;; 62 (1): 193–230. doi: https://doi.org/10.2138/rmg.2006.62.9 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 When it was realized that nominally anhydrous minerals could be a major storage site of water in the mantle (Smyth 1987; Bell and Rossman 1992), it also became rather obvious that many mantle samples probably have lost most of their water during ascent (e.g., Ingrin and Skogby 2000). While analyses of natural samples therefore in many circumstances only provide a lower limit of the actual water content in the mantle, measurements of water solubility give an upper limit of the amount of water that might be stored in a mineral. Experimental measurements of water solubility have... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.