The influence of the Jahn-Teller effect at Fe 2+ on the structure of chromite at high pressure

Physics and Chemistry of Minerals

Volumn 39, Issue 2, 2012, Pages 131-141

  Kyono, Atsushi ^a,b   Gramsch, Stephen A ^b   Yamanaka, Takamitsu ^b   Ikuta, Daijo ^c   Ahart, Muhtar ^b   Mysen, Bjørn O ^b   Mao, Ho kwang ^b   Hemley, Russell J ^b  

^a UNIVERSITY OF TSUKUBA   (Japan)

^b GEOPHYSICAL LABORATORY   (United States)

^c CARNEGIE INSTITUTION OF WASHINGTON   (United States)

Author keywords

Chromite; Diamond anvil cell; High pressure; Jahn Teller effect; Phase transition; Spinel structure

Indexed keywords

ANGULAR DISTORTIONS; ANISOTROPIC DEFORMATION; BIRCH-MURNAGHAN EQUATION OF STATE; BOND DISTANCE; C-AXIS DIRECTION; DIAMOND ANVIL CELL; HIGH PRESSURE; JAHN TELLER EFFECT; OCTAHEDRAL SITES; PHASE-TRANSITION BOUNDARY; PRESSURE-INDUCED PHASE TRANSITION; SINGLE CRYSTAL X-RAY DIFFRACTION; SPACE GROUPS; SPINEL STRUCTURE; TETRAGONAL STRUCTURE; TETRAHEDRAL BONDS; TETRAHEDRAL GEOMETRY; TETRAHEDRAL SITES; UNIT CELLS; UNIT-CELL PARAMETERS; VOLUME CHANGE;

CELLS; CHROMITE; CHROMITE DEPOSITS; EQUATIONS OF STATE OF SOLIDS; GEOMETRY; HIGH PRESSURE ENGINEERING; IRON OXIDES; MOLECULAR ORBITALS; POSITIVE IONS; X RAY DIFFRACTION; X RAY DIFFRACTION ANALYSIS;

PHASE TRANSITIONS;

ANISOTROPY; CHROMITE; COMPRESSION; CRYSTAL STRUCTURE; DEFORMATION; DIAMOND ANVIL CELL; EQUATION OF STATE; HIGH PRESSURE; ISOTROPY; PHASE TRANSITION; TEMPERATE ENVIRONMENT; X-RAY DIFFRACTION;

EID: 84856232963     PISSN: 03421791     EISSN: 14322021     Source Type: Journal    
DOI: 10.1007/s00269-011-0468-6     Document Type: Article

References (44)

1. 4: a new hexagonal aluminous phase with implication for the lower mantle. Phys Earth Planet Inter 115: 67-77.
2. Angel RJ (2002) EOSFIT v5. 2. Crystallography laboratory. Virginia Tech, Blacksburg.
3. Angel RJ (2004) Absorption corrections for diamond-anvil cells implemented in the software package ABSORB 6. 0. J Appl Cryst 37: 486-492.
4. 4. J Magn Magn Mater 310: 807-809.
5. 4 ferrimagnetic spinels. Phys Rev Lett 103: 077205.
6. Burdett JK (1980) Molecular shapes. Wiley, New York.
7. Burdett JK (1981) Use of the Jahn-Teller theorem in inorganic chemistry. Inorg Chem 20: 1959-1962.
8. 4 spinels (M = Mg, Mn, Zn) by ab initio methods. Phys Chem Miner 26: 389-395.
9. Chen M, Shu JF, Mao HK, Xie XD, Hemley RJ (2003a) Natural occurrence and synthesis of two new postspinel polymorphs of chromite. Proc Nat Acad Sci 100: 14651-14654.
10. 4 polymorph in the Suizhou meteorite and its significance in mantle mineralogy. Geochim Cosmochim Acta 67: 3937-3942.
11. Deer WA, Howie RA, Zussman J (1966) An introduction to the rock forming minerals. London, Longman.
12. Dera P (2007) GSE-ADA and RSV data analysis program for monochromatic single crystal diffraction with area detector. GeoSoilEnviroCARS, Argonne.
13. Dunitz JD, Orgel LE (1960) Stereochemistry of ionic solids. Adv Inorg Radiochem 2: 1-60.
14. 5. J Solid State Chem 182: 389-395.
15. Fan D, Zhou W, Liu C, Liu Y, Jiang X, Wan F, Liu J, Li X, Xie H (2008) Thermal equation of state of natural chromium spinel up to 26. 8 GPa and 628 K. J Mat Sci 43: 5546-5550.
16. 4. Am Mineral 84: 203-206.
17. 4): comparisons with silicate spinels. Phys Chem Miner 13: 215-220.
18. Gatta GD, Kantor I, Ballaran TB, Dubrovinsky L, McCammon L (2007) Effect of non-hydrostatic conditions on the elastic behaviour of magnetite: an in situ single-crystal X-ray diffraction study. Phys Chem Miner 34: 627-635.
19. 13C diamond. Phy Rev B 60: 14660-14664.
20. 2+ ions. J Phys Chem Solids 25: 151-160.
21. Haavik C, Stølen S, Fjellvåg H, Hanfland M, Häusermann D (2000) Equation of state of magnetite and its high-pressure modification: thermodynamics of the Fe-O system at high pressure. Am Mineral 85: 514-523.
22. Hammersley AP (1998) FIT2D v. 9. 129. Reference manual v. 3. 1. ESRF internet report ESRF98HA01T. European synchrotron radiation facility, Grenoble.
23. Holland TJB, Redfern SAT (1997) Unit cell refinement from powder diffraction data: the use of regression diagnostics. Mineral Mag 61: 65-77.
24. Izumi F, Ikeda T (2000) A Rietveld-analysis program RIETAN-98 and its application to zeolites. Mater Sci Forum 321-324: 198-203.
25. Jahn HA, Teller E (1937) Stability of polyatomic molecules in degenerate electronic states I. Orbital degeneracy. Proc R Soc Lond Ser A 161: 220-235.
26. 4 determined by high P-T in situ X-ray diffractometry. Phys Earth Planet Int 136: 11-24.
27. King HE, Finger LW (1979) Diffracted beam crystal centering and its application to high-pressure crystallography. J Appl Cryst 12: 374-378.
28. 4 solid solution series. Phys Chem Miner 31: 633-642.
29. 4) at high pressure from synchrotron X-ray powder diffraction. Phys Chem Miner 27: 638-644.
30. 4, as a function of pressure and temperature. Phys Chem Miner 31: 122-129.
31. Mao HK, Xu J, Bell PM (1986) Calibration of the ruby pressure gauge to 800 kbar under quasi-hydrostatic conditions. J Geophys Res 91: 4673-4676.
32. 4 (A = Mn, Fe, Co, Cu, Zn, Cd; X = O, S, Se). J Phys Soc Jpn 77: 034713.
33. 4: competition between anharmonic lattice potential and spin-orbit coupling. J Phys Condens Matter 22: 176003.
34. Peltier WR, Solheim LP (1992) Mantle phase-transitions and layered chaotic convection. Geophys Res Lett 19: 321-324.
35. Robinson K, Gibbs GV, Ribbe PH (1971) Quadratic elongation: a quantitative measure of distortion in coordination polyhedra. Science 172: 567-570.
36. Shannon RD (1976) Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides. Acta Cryst A32: 751-767.
37. Sheldrick GM (1997) SHELXL97, release 97-2. Program for the refinement of crystal structures. University of Göttingen, Germany.
38. 4 and its relation to the 660-km seismic discontinuity. Nature 411: 571-574.
39. Shu JF, Mao WL, Hemley RJ, Mao HK (2007) Pressure-induced distortive phase transition in chromite-spinel at 29 GPa. In: Manaa MR, Goncharov AF, Hemley RJ, Bini R (eds) Materials research at high pressure, vol 987. Materials Research Society, Warrendale, pp 179-184.
40. 4. Phys Rev 152: 376-402.
41. 2+ ions in oxygen-based rock-forming minerals at temperatures between 297 and 600 K. Phys Chem Miner 28: 199-210.
42. 4 observed by neutron scattering. J Phys Soc Jpn 77: 124703.
43. 4 through electrostatic potential using convergent-beam electron diffraction. Phys Rev B 81: 180102.
44. 4 observed by maximum entropy method at high pressure and low temperature. Phys Rev B80: 134120.