PRESSURE-VOLUME-TEMPERATURE EQUATION OF STATE OF ANDRADITE AND GROSSULAR, BY HIGH-PRESSURE AND -TEMPERATURE POWDER DIFFRACTION

dc.contributor.authorPavese A.
dc.contributor.authorDiella V.
dc.contributor.authorPischedda V.
dc.contributor.authorMerli M.
dc.contributor.authorBocchio R.
dc.contributor.authorMezouar M.
dc.date.accessioned2021-03-30T10:40:29Z
dc.date.available2021-03-30T10:40:29Z
dc.date.issued2001
dc.description.abstractThe thermoelastic parameters of natural andradite and grossular have been investigated by high-pressure and -temperature synchrotron X-ray powder diffraction, at ESRF, on the ID30 beamline. The P–V–T data have been fitted by Birch-Murnaghan-like EOSs, using both the approximated and the general form. We have obtained for andradite K 0=158.0(±1.5) GPa, (dK/dT )0=−0.020(3) GPa K−1 and α0=31.6(2) 10−6 K−1, and for grossular K 0=168.2(±1.7) GPa, (dK/dT)0=−0.016(3) GPa K−1 and α0=27.8(2) 10−6 K−1. Comparisons between the present issues and thermoelastic properties of garnets earlier determined are carried out.
dc.identifierhttps://www.elibrary.ru/item.asp?id=872472
dc.identifier.citationPhysics and Chemistry of Minerals, 2001, 28, 4, 242-248
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/27187
dc.subjectANDRADITE
dc.subjectGROSSULAR
dc.subjectT EOS
dc.subjectX-RAY POWDER DIFFRACTION
dc.titlePRESSURE-VOLUME-TEMPERATURE EQUATION OF STATE OF ANDRADITE AND GROSSULAR, BY HIGH-PRESSURE AND -TEMPERATURE POWDER DIFFRACTION
dc.typeСтатья

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