THE STRUCTURE OF HYDROUS SPECIES IN NOMINALLY ANHYDROUS MINERALS: INFORMATION FROM POLARIZED IR SPECTROSCOPY
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dc.contributor.author | Libowitzky E. | |
dc.contributor.author | Beran A. | |
dc.date.accessioned | 2024-08-03T06:10:58Z | |
dc.date.available | 2024-08-03T06:10:58Z | |
dc.date.issued | 2006 | |
dc.identifier | https://elibrary.ru/item.asp?id=38919042 | |
dc.identifier.citation | Reviews in Mineralogy and Geochemistry, 2006, 62, 62. С., 29-52 | |
dc.identifier.issn | 1529-6466 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/44623 | |
dc.description.abstract | Hydrogen is a major constituent in a wide variety of minerals in the Earth’s crust. Usually H is bonded to oxygen forming H 2 O molecules or OH − groups. In rare cases, H 3 O + , H 3 O 2− and H 5 O 2+ units are also formed. The occurrence of NH 4+ , 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 microporous minerals such as zeolites and clay minerals, which are of considerable economic and ecologic importance. | |
dc.title | THE STRUCTURE OF HYDROUS SPECIES IN NOMINALLY ANHYDROUS MINERALS: INFORMATION FROM POLARIZED IR SPECTROSCOPY | |
dc.type | Статья | |
dc.identifier.doi | 10.2138/rmg.2006.62.2 |
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