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dc.contributor.author Keppler H.
dc.contributor.author Bolfan-Casanova N.
dc.date.accessioned 2025-03-15T04:58:55Z
dc.date.available 2025-03-15T04:58:55Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=27902973
dc.identifier.citation Reviews in Mineralogy and Geochemistry, 2006, 62, 62. С. 1, 193-230
dc.identifier.issn 1529-6466
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48548
dc.description.abstract 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 therefore naturally evolved in the last decades as a major tool for understanding the water storage capacity of the mantle.
dc.title THERMODYNAMICS OF WATER SOLUBILITY AND PARTITIONING
dc.type Статья
dc.identifier.doi 10.2138/rmg.2006.62.9


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