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

被引:33
作者
Sithole, HM
Ngoepe, PE
Wright, K
机构
[1] UCL, Dept Chem, London WC1E 6BT, England
[2] Univ North, Sch Phys & Mineral Sci, Mat Modelling Ctr, ZA-0727 Sovenga, South Africa
[3] CSIR, Mfg & Mat Technol, ZA-0002 Pretoria, South Africa
[4] Royal Inst Great Britain, London W1S 4BS, England
关键词
pyrite; high pressure; computer simulation;
D O I
10.1007/s00269-003-0359-6
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
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.
引用
收藏
页码:615 / 619
页数:5
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