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American Mineralogist; October; v. 93; no. 10; p. 1581-1584; DOI: 10.2138/am.2008.2816
© 2008 Mineralogical Society of America
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High-pressure study on lead fluorapatite

Xi Liu, Sean R. Shieh*, Michael E. Fleet and Arslan Akhmetov

Department of Earth Sciences, University of Western Ontario, London, Ontario, N6A 5B7, Canada

Correspondence: * E-mail: sshieh{at}uwo.ca

The compressional behavior of a synthetic lead fluorapatite [Pb9.35(PO4)6F2] has been investigated in situ up to about 16.7 GPa at 300 K, using a diamond-anvil cell and synchrotron X-ray diffraction. We find that the compressibility of lead fluorapatite is significantly different from that of fluorapatite [Ca10(PO4)6F2], chlorapatite [Ca10(PO4)6Cl2], and hydroxylapatite [Ca10(PO4)6(OH)2]: lead fluorapatite is much more compressible, and elastically isotropic in the investigated pressure range. The pressure-volume data fitted to the third-order Birch-Murnaghan equation yield an isothermal bulk modulus (KT) of 54.3(18) GPa and the pressure derivative (KT') of 8.1(6). If KT' is fixed at 4, the obtained KT is 68.4(16) GPa, which is approximately only two-thirds of the isothermal bulk modulus of the calcium apatites.

Key Words: Lead fluorapatite • compressibility • synchrotron X-ray diffraction • isothermal bulk modulus • high pressure




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S. Zhai, X. Liu, S. R. Shieh, L. Zhang, and E. Ito
Equation of state of {gamma}-tricalcium phosphate, {gamma}-Ca3(PO4)2, to lower mantle pressures
American Mineralogist, October 1, 2009; 94(10): 1388 - 1391.
[Abstract] [Full Text] [PDF]




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