High-pressure synchrotron x-ray diffraction and Raman spectroscopic study of plumbogummite

doi:10.1088/1674-1056/27/1/017402

Abstract PbAl₃(PO₄)₂(OH,H₂O)₆, an important environmental mineral, is in-situ studied by synchrotron x-ray diffraction (XRD) and Raman scattering combined with diamond anvil cells (DACs) at pressures up to~11.0 GPa and room temperature. The XRD results indicate that plumbogummite does not undergo a phase transition between 0 GPa and 10.9 GPa. Moreover, the c axis is more compressible than the a axis, revealing its anisotropic behavior. The pressure-volume data are fitted to the third-order Birch-Murnaghan equation of state to yield the plumbogummite bulk modulus K₀ of 68(1) GPa and K'₀ of 6.1. The[PO₄]^3- and[HPO₄]^2- Raman vibrational modes exhibit scale nearly linearly as a function of pressure. The[PO₄]^3- stretching modes are generally more sensitive to pressure than the bending modes. The Grüneisen parameters range from -0.07 to 1.19, with an arithmetic mean of approximately 0.39.

Keywords: plumbogummite equation of state Grüneisen parameter diamond anvil cell

Received: 18 April 2017
Revised: 18 October 2017
Accepted manuscript online:

PACS:	74.25.nd	(Raman and optical spectroscopy)
	74.25.Ld	(Mechanical and acoustical properties, elasticity, and ultrasonic Attenuation)

Fund: Project supported by the National Natural Science Foundation of China (Grant Nos. 41473056 and 41472037).

Corresponding Authors: Xiang Wu
E-mail: wuxiang@cug.edu.cn

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Duan Kang(康端), Xiang Wu(巫翔), Guan Yuan(袁冠), Sheng-Xuan Huang(黄圣轩), Jing-Jing Niu(牛菁菁), Jing Gao(高静), Shan Qin(秦善) High-pressure synchrotron x-ray diffraction and Raman spectroscopic study of plumbogummite 2018 Chin. Phys. B 27 017402

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High-pressure synchrotron x-ray diffraction and Raman spectroscopic study of plumbogummite

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