THERMAL EXPANSION OF MG(OH)2 BRUCITE UNDER HIGH PRESSURE AND PRESSURE DEPENDENCE OF ENTROPY

dc.contributor.authorFukui H.
dc.contributor.authorOhtaka O.
dc.contributor.authorSuzuki T.
dc.contributor.authorFunakoshi K.
dc.date.accessioned2022-02-13T04:46:09Z
dc.date.available2022-02-13T04:46:09Z
dc.date.issued2003
dc.description.abstractAn equation of state for Mg(OH)2 brucite under high-pressure and high-temperature conditions has been obtained by measuring temperature dependence of volume up to 600 K at ambient pressure and pressure dependence of volume up to 16 GPa at 300, 473, 673, and 873 K with in situ X-ray diffraction. Pressure dependence of entropy of brucite has been calculated with thermal expansion coefficient and volume which are derived from the present EoS. This dependence indicates that generation of secondary OH dipoles affects entropy. The OH dipoles probably appear around 2 GPa and the number seems not to change over 8 GPa at 300 K.
dc.identifierhttps://elibrary.ru/item.asp?id=5108138
dc.identifier.citationPhysics and Chemistry of Minerals, 2003, 30, 9, 511-516
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/35277
dc.subjectBRUCITE
dc.subjectEQUATION OF STATE
dc.subjectTHERMAL EXPANSION
dc.subjectENTROPY
dc.subjectX-RAY DIFFRACTION
dc.titleTHERMAL EXPANSION OF MG(OH)2 BRUCITE UNDER HIGH PRESSURE AND PRESSURE DEPENDENCE OF ENTROPY
dc.typeСтатья

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