Effect of temperature on the Raman spectra of Ca5(PO4)3F fluorapatite

被引:11
作者
Xue, Weihong [1 ]
Zhai, Kuan [1 ,2 ]
Lin, Chung-Cherng [3 ]
Zhai, Shuangmeng [1 ]
机构
[1] Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths In, Guiyang 550081, Guizhou, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Acad Sinica, Inst Earth Sci, Taipei 115, Taiwan
基金
中国国家自然科学基金;
关键词
fluorapatite; Ca-5(PO4)(3)F; Raman spectra; high temperature; X-RAY-DIFFRACTION; HIGH-PRESSURE; VIBRATIONAL BEHAVIOR; APATITE; PHASE; COMPRESSIBILITY; DECOMPOSITION; SPECTROSCOPY; PHOSPHORUS; STABILITY;
D O I
10.1127/ejm/2018/0030-2769
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The effect of temperature on the vibrational modes of fluorapatite, Ca-5(PO4)(3)F, were investigated by micro-Raman spectroscopy in the temperature range of 80-1023K at ambient pressure. No phase transition was observed during heating though two vibrations become unresolvable due to weak intensity or overlapping. The Raman frequencies of all observed bands for fluorapatite continuously decrease with increasing temperature. The quantitative analysis of temperature dependences of Raman bands indicates that the v(3) asymmetric stretching vibrations show larger temperature coefficients (from -1.34 x 10(-2) to -1.82 x 10(-2) cm(-1) K-1) whereas the v(4) and v(2) bending vibrations have smaller temperature coefficients (from -0.27 x 10(-2) to -0.85 x 10(-2) cm(-1) K-1), which may be attributed to the temperature-induced structural evolution of the PO4 tetrahedron in fluorapatite at high temperature. The temperature and pressure dependence of the force constant for P-O stretching vibrations in Ca-5(PO4)(3)F was calculated. The isobaric mode Gruneisen parameters and anharmonic mode parameters were calculated, indicating the existence of intrinsic anharmonicity for fluorapatite.
引用
收藏
页码:951 / 956
页数:6
相关论文
共 37 条
[1]   Barometric constraints based on apatite inclusions in garnet [J].
Ashley, Kyle T. ;
Barkoff, Drew W. ;
Steele-MacInnis, Mattatthew .
AMERICAN MINERALOGIST, 2017, 102 (04) :743-749
[2]  
BAUER M, 1993, EUR J MINERAL, V5, P307
[3]  
Brunet F, 1999, EUR J MINERAL, V11, P1023
[4]   A high-temperature and high-pressure Raman spectroscopic study of CaGeO3 garnet [J].
Chaplin, TD ;
Ross, NL ;
Reynard, B .
PHYSICS AND CHEMISTRY OF MINERALS, 2000, 27 (03) :213-219
[5]   Phase Transitions and Thermal Expansion of Apatite-Structured Compounds [J].
Chernorukov, N. G. ;
Knyazev, A. V. ;
Bulanov, E. N. .
INORGANIC MATERIALS, 2011, 47 (02) :172-177
[6]   Geochronology and Thermochronology Using Apatite: Time and Temperature, Lower Crust to Surface [J].
Chew, David M. ;
Spikings, Richard A. .
ELEMENTS, 2015, 11 (03) :189-194
[7]   Structural and vibrational behaviour of fluorapatite with pressure. Part I: in situ single-crystal X-ray diffraction investigation [J].
Comodi, P ;
Liu, Y ;
Zanazzi, PF ;
Montagnoli, M .
PHYSICS AND CHEMISTRY OF MINERALS, 2001, 28 (04) :219-224
[8]   Structural and vibrational behaviour of fluorapatite with pressure. Part II: in situ micro-Raman spectroscopic investigation [J].
Comodi, P ;
Liu, Y ;
Frezzotti, ML .
PHYSICS AND CHEMISTRY OF MINERALS, 2001, 28 (04) :225-231
[9]   Petrochronology Based on REE-Minerals: Monazite, Allanite, Xenotime, Apatite [J].
Engi, Martin .
PETROCHRONOLOGY: METHODS AND APPLICATIONS, 2017, 83 :365-418
[10]  
Fei Y., 1995, THERMAL EXPANSION MI, P29, DOI [10.1029/RF002p0029, DOI 10.1029/RF002P0029]