Solid solutions between lead fluorapatite and lead fluorvanadate apatite: compressibility determined by using a diamond-anvil cell coupled with synchrotron X-ray diffraction

Physics and Chemistry of Minerals - Tập 39 - Trang 219-226 - 2011
Qiang He1,2, Xi Liu1,2, Xiaomin Hu1,2, Liwei Deng3, Zhiqiang Chen4, Baosheng Li5, Yingwei Fei3
1Key Laboratory of Orogenic Belts and Crustal Evolution, MOE, Peking University, Beijing, People’s Republic of China
2School of Earth and Space Sciences, Peking University, Beijing, People’s Republic of China
3Geophysical Laboratory, Carnegie Institution of Washington, Washington, USA
4National Synchrotron Light Source, Brookhaven National Laboratory, Upton, New York, USA
5Mineral Physics Institute, State University of New York, Stony Brook, New York, USA

Tóm tắt

The synthetic solid solutions between lead fluorapatite and lead fluorvanadate apatite, Pb10[(PO4)6−x (VO4) x ]F2 with x equal to 0, 1, 2, 3, 4, 5, and 6, were compressed up to about 9 GPa at ambient temperature by using a diamond-anvil cell coupled with synchrotron X-ray radiation. A second-order Birch–Murnaghan equation of state was used to fit the data. As the substitution of the PO4 3− cations by the VO4 3− cations progresses, the isothermal bulk modulus steadily decreases, with a maximum reduction of about 16% (from 68.4(16) GPa for Pb10(PO4)6F2 to 57.2(28) GPa for Pb10(VO4)6F2). For the entire composition range, the a-axis dimension remains more compressible than the c-axis dimension, with the ratio of the axial bulk moduli (K T−c :K T−a ) larger than 1. The ratio of K T−c to K T−a increases from about 1.04(4) to 1.23(14) as the composition parameter x increases from 0 to 6, suggesting that the apatite solid solutions Pb10[(PO4)6−x (VO4) x ]F2 become more elastically anisotropic.

Tài liệu tham khảo

Angel RJ (2000) Equation of state. In: Hazen RM, Downs RT (eds) High-temperature and high-pressure crystal chemistry. Reviews in mineralogy and geochemistry, vol 41. Mineralogical Society of America, Chantilly, pp 35–60 Birch F (1947) Finite elastic strain of cubic crystals. Phys Rev 71:809–924 Blundy JD, Wood BJ (1994) Prediction of crystal-melt partition coefficients from elastic moduli. Nature 372:452–454 Boechat CB, Eon J-G, Rossi AM, Perez CAD, San Gil RAD (2000) Structure of vanadate in calcium phosphate and vanadate apatite solid solutions. Phys Chem Chem Phys 2:4225–4230 Brunet F, Allan DR, Redfern SAT, Angel RJ, Miletich RM, Reichmann HJ, Sergent J, Hanfland M (1999) Compressibility and thermal expansivity of synthetic apatites, Ca5(PO4)3X with X = OH, F and Cl. Eur J Miner 11:1023–1035 Chernorukov NG, Knyazev AV, Bulanov EN (2010) Isomorphism and phase diagram of the Pb5(PO4)3Cl-Pb5(VO4)3Cl system. Russ J Inorg Chem 55:1463–1470 Ching WY, Rulis P, Misra A (2009) Ab initio elastic properties and tensile strength of crystalline hydroxyapatite. Acta Biomater 5:3067–3075 Comodi P, Liu Y, Zanazzi PF, Montagnoli M (2001a) Structural and vibrational behaviour of fluorapatite with pressure. Part I: in situ single-crystal X-ray diffraction investigation. Phys Chem Miner 28:219–224 Comodi P, Liu Y, Frezzotti ML (2001b) Structural and vibrational behaviour of fluorapatite with pressure. Part II: in situ micro-raman spectroscopic investigation. Phys Chem Miner 28:225–231 Fleet ME, Liu X (2007) Hydrogen-carbonate ion in synthetic high-pressure apatite. Am Miner 92:1764–1767 Fleet ME, Pan Y (1997) Rare earth elements in apatite: uptake from H2O-bearing phosphate-fluoride melts and the role of volatile components. Geochim Cosmochim Acta 61:4745–4760 Fleet ME, Liu X, Pan Y (2000a) Site preference of rare earth elements in hydroxyapatite [Ca10(PO4)6(OH)2]. J Solid State Chem 149:391–398 Fleet ME, Liu X, Pan Y (2000b) Rare-earth elements in chlorapatite [Ca10(PO4)6Cl2]: uptake, site preference, and degradation of monoclinic structure. Am Miner 85:1437–1446 Fleet ME, Liu X, Shieh SR (2010) Structural change in lead fluorapatite at high pressure. Phys Chem Miner 37:1–9 Gatta GD, Lee Y, Kao CC (2009) Elastic behavior of vanadinite, Pb10(VO4)6Cl2, a microporous non-zeolitic mineral. Phys Chem Miner 36:311–317 Gilmore RS, Katz JL (1982) Elastic properties of apatites. J Mater Sci 17:1131–1141 Hammersley J (1996) Fit2D report. Europe Synchrotron Radiation Facility, Grenoble, France Hardcastle FD, Wachs IE (1991) Determination of vanadium-oxygen bond distances and bond orders by Raman spectroscopy. J Phys Chem 95:5031–5041 He Q, Liu X, Hu X, Li S, Wang H (2011) Solid solution between lead fluorapatite and lead fluorvanadate apatite: mixing behavior, Raman feature and thermal expansivity. Phys Chem Miner 38:741–752 Hughes JM, Rakovan J (2002) The crystal structure of apatite, Ca5(PO4)3(F, OH, Cl). In: Kohn MJ, Rakovan J, Hughes JM (eds) Phosphates. Reviews in Mineralogy and Geochemistry, vol 48. Mineralogical Society of America, Chantilly, pp 1–12 Kim JY, Fenton RR, Hunter BA, Kennedy BJ (2000) Powder diffraction studies of synthetic calcium and lead apatites. Aust J Chem 53:679–686 Klemme S, Dalpé C (2003) Trace-element partitioning between apatite and carbonatite melt. Am Miner 88:639–646 Klotz S, Chervin JC, Munsch P, Le Marchand G (2009) Hydrostatic limits of 11 pressure transmitting media. J Phys D Appl Phys 42:075413 Liu X, Shieh SR, Fleet ME, Akhmetov A (2008) High-pressure study on lead fluorapatite. Am Miner 93:1581–1584 Liu X, Shieh SR, Fleet ME, Zhang L (2009) Compressibility of a natural kyanite at 300 K. Prog Nat Sci 19:1281–1286 Liu X, Fleet ME, Shieh SR, He Q (2011a) Synthetic lead bromapatite: X-ray structure at ambient pressure and compressibility up to about 20 GPa. Phys Chem Miner 38:397–406 Liu X, Shieh SR, Fleet ME, Zhang L, He Q (2011b) Equation of state of carbonated hydroxylapatite at ambient temperature: significance of carbonate. Am Miner 96:74–80 Mao HK, Bell PM, Shaner JW, Steinberg DJ (1978) Specific volume measurements of Cu, Mo, Pt, and Au and calibration of rub R1 fluorescence pressure gauge for 0.006–1 Mbar. J Appl Phys 49:3276–3283 Matsukage KN, Ono S, Kawamoto T, Kikegawa T (2004) The compressibility of a natural apatite. Phys Chem Miner 31:580–584 Mercier PHJ, Dong J, Baikie T, Page YL, White TJ, Whitfield PS, Mitchel LD (2007) Ab initio constrained crystal-chemical Rietveld refinement of Ca10(VxP1−xO4)6F2 apatites. Acta Cryst B63:37–48 Murayama JK, Nakai S, Kato M, Kumazawa M (1986) A dense polymorph of Ca3(PO4)2: a high pressure phase of apatite decomposition and its geochemical significance. Phys Earth Planet Int 44:293–303 Pan Y, Fleet ME (2002) Compositions of the apatite-group minerals: substitution mechanisms and controlling factors. In: Kohn MJ, Rakovan J, Hughes JM (eds) Phosphates. Reviews in mineralogy and geochemistry, vol 48. Mineralogical Society of America, Chantilly, pp 13–49 Popović L, de Waal D, Boeyens JCA (2005) Correlation between Raman wavenumbers and P–O bond lengths in crystalline inorganic phosphates. J Raman Spectrosc 36:2–11 Prowatke S, Klemme S (2006) Trace element partitioning between apatite and silicate melts. Geochim Cosmochim Acta 70:4513–4527 Sha MC, Li Z, Brad RC (1994) Single-crystal elastic constants of fluorapatite, Ca5F(PO4)3. J Appl Phys 75:7784–7787 Shannon RD (1976) Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides. Acta Cryst A32:751–767 Snyders R, Music D, Sigumonrong D, Schelnberger B, Jensen J, Schneider JM (2007) Experimental and ab initio study of the mechanical properties of hydroxyapatite. Appl Phys Lett 90:193902 Teraoka K, Ito A, Maekawa K, Onuma K, Tateishi T, Tsutsumi S (1998) Mechanical properties of hydroxyapatite and OH-carbonated hydroxyapatite single crystals. J Dent Res 77:1560–1568 Yoon HS, Newnham RE (1969) Elastic properties of fluorapatite. Am Miner 54:1193–1197