Intrinsic stoichiometry and oxygen-induced p-type conductivity of pyrite FeS2

被引:65
作者
Sun, Ruoshi [1 ]
Chan, M. K. Y. [1 ,2 ]
Kang, Shin Young [1 ]
Ceder, G. [1 ]
机构
[1] MIT, Dept Mat Sci & Engn, Cambridge, MA 02139 USA
[2] Argonne Natl Lab, Ctr Nanoscale Mat, Argonne, IL 60439 USA
基金
美国国家科学基金会;
关键词
INITIO MOLECULAR-DYNAMICS; TOTAL-ENERGY CALCULATIONS; FILMS; SULFURIZATION; IMPURITIES; DEFECTS; GROWTH;
D O I
10.1103/PhysRevB.84.035212
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The stoichiometry and ubiquitous observation of p-type conductivity of synthetic pyrite FeS2 thin films are investigated via first-principles computations of native (vacancies, interstitials, antisites) and extrinsic (O-S, O-i) point defects. Native defects have high formation energies and are predicted to occur in low concentrations within the Fe- and S-rich limits, showing that pyrite should be intrinsically stoichiometric. Under sufficiently oxidizing conditions, O-S becomes the most dominant defect type and induces p-type conductivity. At the experimental oxygen impurity concentration, the hole concentration is predicted to be O(10(19)) cm(-3), in agreement with Hall measurements reported in the literature. Therefore, we attribute the unintentional p-type conductivity of pyrite to oxygen impurities and propose that improvements in device performance may be achieved under more reducing conditions.
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页数:7
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