Atomistic simulation of the structure and elastic properties of pyrite (FeS2) as a function of pressure

Physics and Chemistry of Minerals - Tập 30 - Trang 615-619 - 2003
H.M. Sithole1,2, P.E. Ngoepe1, K. Wright3,4
1Materials Modelling Centre, School of Physical and Mineral Sciences, University of the North, Sovenga, South Africa
2De Beers Consolidated Mines, TSS Technologies, Johannesburg, South Africa
3Departments of Chemistry and Earth Sciences, University College London, London, UK
4Royal Institution, London, UK

Tóm tắt

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.