The band gap and electrical resistivity of FeS2-pyrite at high pressures

被引:23
作者
Cervantes, P
Slanic, Z
Bridges, F
Knittle, E
Williams, Q [1 ]
机构
[1] Univ Calif Santa Cruz, Dept Earth Sci, Santa Cruz, CA 95064 USA
[2] Univ Calif Santa Cruz, Dept Phys, Santa Cruz, CA 95064 USA
基金
美国国家科学基金会;
关键词
electrical conductivity;
D O I
10.1016/S0022-3697(02)00179-8
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The indirect energy gap and electrical resistivity of FeS2-pyrite have been measured at high pressures and 300 K using optical absorption spectroscopy and electrical conductivity measurements. Absorption spectra extend to similar to28 GPa, while resistivity is determined to similar to34 GPa. The band gap of FeS2 is indirect throughout this pressure range and decreases linearly with pressure at a rate of -1.13(9) x 10(-2) eV/GPa. If this linear trend continues, FeS2 is expected to metallize at a pressure of 80(+/-8) GPa. The logarithm of resistivity also linearly decreases with pressure to 14 GPa with a slope of -0.101(+/-0.001)/GPa. However, between 14 and 34 GPa, the logarithm of resistivity is nearly constant, with a slope of -0.011(+/-0.003)/GPa. The measured resistivity of pyrite may be generated predominantly by extrinsic effects. (C) 2002 Published by Elsevier Science Ltd.
引用
收藏
页码:1927 / 1933
页数:7
相关论文
共 42 条
[11]   PHOTOELECTROCHEMICAL RESPONSE AND OPTICAL-ABSORPTION OF PYRITE (FES2) NATURAL SINGLE-CRYSTALS [J].
FERRER, IJ ;
SANCHEZ, C .
SOLID STATE COMMUNICATIONS, 1992, 81 (05) :371-374
[12]   ABOUT THE BAND-GAP NATURE OF FES2 AS DETERMINED FROM OPTICAL AND PHOTOELECTROCHEMICAL MEASUREMENTS [J].
FERRER, IJ ;
NEVSKAIA, DM ;
DELASHERAS, C ;
SANCHEZ, C .
SOLID STATE COMMUNICATIONS, 1990, 74 (09) :913-916
[13]  
FINKLEA SL, 1976, ACTA CRYSTALLOGR A, V32, P529, DOI 10.1107/S0567739476001198
[14]   ELECTRONIC-STRUCTURE OF SOME 3D TRANSITION-METAL PYRITES [J].
FOLKERTS, W ;
SAWATZKY, GA ;
HAAS, C ;
DEGROOT, RA ;
HILLEBRECHT, FU .
JOURNAL OF PHYSICS C-SOLID STATE PHYSICS, 1987, 20 (26) :4135-4144
[15]   X-RAY DETERMINATION OF ELECTRON-DISTRIBUTION IN CRYSTALS OF [CO(NH3)6][CR(CN)6] AT 80-K [J].
IWATA, M .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1977, 33 (JAN15) :59-69
[16]   IS THE INNER CORE OF THE EARTH PURE IRON [J].
JEPHCOAT, A ;
OLSON, P .
NATURE, 1987, 325 (6102) :332-335
[17]   ELECTRICAL AND OPTICAL-PROPERTIES OF NATURAL IRON PYRITE (FES2) [J].
KARGUPPIKAR, AM ;
VEDESHWAR, AG .
PHYSICA STATUS SOLIDI A-APPLIED RESEARCH, 1988, 109 (02) :549-558
[18]  
Kittel C., 2018, Introduction to solid state physics, V8th
[19]   THE HIGH-PRESSURE PHASE-DIAGRAM OF FE0.94O - A POSSIBLE CONSTITUENT OF THE EARTHS CORE [J].
KNITTLE, E ;
JEANLOZ, R .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1991, 96 (B10) :16169-16180
[20]  
KOU WW, 1978, PHYS REV B, V18, P7062, DOI 10.1103/PhysRevB.18.7062