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

Show simple item record

dc.contributor.author Pavese A.
dc.contributor.author Diella V.
dc.contributor.author Pischedda V.
dc.contributor.author Merli M.
dc.contributor.author Bocchio R.
dc.contributor.author Mezouar M.
dc.date.accessioned 2021-03-30T10:40:29Z
dc.date.available 2021-03-30T10:40:29Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=872472
dc.identifier.citation Physics and Chemistry of Minerals, 2001, 28, 4, 242-248
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27187
dc.description.abstract The 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.subject ANDRADITE
dc.subject GROSSULAR
dc.subject T EOS
dc.subject X-RAY POWDER DIFFRACTION
dc.title PRESSURE-VOLUME-TEMPERATURE EQUATION OF STATE OF ANDRADITE AND GROSSULAR, BY HIGH-PRESSURE AND -TEMPERATURE POWDER DIFFRACTION
dc.type Статья


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record