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Thermal expansion of Mg(OH)2 brucite under high pressure and pressure dependence of entropy
Authors:H.?Fukui  author-information"  >  author-information__contact u-icon-before"  >  mailto:fukuih@ess.sci.osaka-u.ac.jp"   title="  fukuih@ess.sci.osaka-u.ac.jp"   itemprop="  email"   data-track="  click"   data-track-action="  Email author"   data-track-label="  "  >Email author,O.?Ohtaka,T.?Suzuki,K.?Funakoshi
Affiliation:(1) Department of Earth and Space Science, Osaka University, Toyonaka, Osaka, 560–0043, Japan;(2) Faculty of Environmental Engineering, The University of Kitakyushu, Hibikino, Fukuoka, 808–0135, Japan;(3) Japan Synchrotron Radiation Research Institute, SPring-8, Hyogo, 678–5198, Japan
Abstract:An 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.
Keywords:Brucite  Equation of state  Thermal expansion  Entropy  X-ray diffraction
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