MOLECULAR DYNAMICS SIMULATIONS OF THE PHASE TRANSITION BETWEEN LOW-TEMPERATURE AND HIGH-TEMPERATURE CLINOENSTATITES

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dc.contributor.author Shimobayashi N.
dc.contributor.author Miyake A.
dc.contributor.author Kitamura M.
dc.contributor.author Miura E.
dc.date.accessioned 2021-03-15T05:26:55Z
dc.date.available 2021-03-15T05:26:55Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=812762
dc.identifier.citation Physics and Chemistry of Minerals, 2001, 28, 9, 591-599
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26708
dc.description.abstract Phase transition between low-temperature clinoenstatite (LT-CEn) and high-temperature clinoenstatite (HT-CEn) was studied by using molecular dynamics (MD) simulations, based on empirical potential parameters. Starting from LT-CEn, the MD calculations were carried out at atmospheric pressure and at elevated pressures (1-6 GPa). At elevated temperatures the transformation from the starting LT-CEn to HT-CEn occurred at any pressure. It was confirmed that the HT-CEn has the same space group C2/c as diopside but the M2 site is six-coordinated, unlike diopside. A significant difference in the MD-simulated cell volumes between LT-CEn and HT-CEn was also observed, showing a first-order transition. In addition, there were some temperature ranges where LT-CEN and HT-CEn would be coexistent and very small thermal hystereses between increasing and decreasing temperatures during the transition. These behaviors are consistent with the characteristic of a thermoelastic-martensitic transformation. The phase boundary between LT-CEn and HT-CEn was determined for the first time. Its positive dT/dP slope strongly shows that the high-pressure clinoenstatite is a significantly distinct phase from HT-CEn although the both phases have the same space group, C2/c.
dc.subject MOLECULAR DYNAMICS SIMULATION
dc.subject CLINOENSTATITE
dc.subject PHASE TRANSFORMATION
dc.subject POLYMORPH
dc.title MOLECULAR DYNAMICS SIMULATIONS OF THE PHASE TRANSITION BETWEEN LOW-TEMPERATURE AND HIGH-TEMPERATURE CLINOENSTATITES
dc.type Статья


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