ATOMISTIC SIMULATION OF THE STRUCTURE AND ELASTIC PROPERTIES OF PYRITE (FES2) AS A FUNCTION OF PRESSURE

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dc.contributor.author Sithole H.M.
dc.contributor.author Ngoepe P.E.
dc.contributor.author Wright K.
dc.date.accessioned 2022-02-13T04:46:06Z
dc.date.available 2022-02-13T04:46:06Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=5103876
dc.identifier.citation Physics and Chemistry of Minerals, 2003, 30, 10, 615-619
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35259
dc.description.abstract Interatomic potential parameters have been derived at simulated temperatures of 0 K and 300 K to model pyrite FeS2. The predicted pyrite structures are within 1% of those determined experimentally, while the calculated bulk modulus is within 7%. The model is also able to simulate the properties of marcasite, even though no data for this phase were included in the fitting procedure. There is almost no difference in results obtained for pyrite using the two potential sets; however, when used to model FeS2 marcasite, the potential fitted at 0 K performs better. The potentials have also been used to study the high-pressure behaviour of pyrite up to 44 GPa. The calculated equation of state gives good agreement with experiment and shows that the Fe-S bonds shorten more rapidly that the S-S dimer bonds. The behaviour of marcasite at high pressure is found to be similar to that of pyrite.
dc.subject PYRITE
dc.subject HIGH PRESSURE
dc.subject COMPUTER SIMULATION
dc.title ATOMISTIC SIMULATION OF THE STRUCTURE AND ELASTIC PROPERTIES OF PYRITE (FES2) AS A FUNCTION OF PRESSURE
dc.type Статья


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