Abstract
High-pressure single-crystal synchrotron X-ray diffraction was carried out on a single crystal of natural beryl compressed in a diamond anvil cell. The pressure–volume (P–V) data from room pressure to 9.51 GPa were fitted by a third-order Birch–Murnaghan equation of state (BM-EoS) and resulted in unit-cell volume V 0 = 675.5 ± 0.1 Å3, isothermal bulk modulus K 0 = 180 ± 2 GPa, and its pressure derivative \(K_{0}^{{\prime }}\) = 4.2 ± 0.5. We also calculated V 0 = 675.5 ± 0.1 Å3 and K 0 = 181 ± 1GPa with fixed \(K_{0}^{{\prime }}\) at 4.0 and then obtained the axial moduli for a (K a0)-axis and c (K c0)-axis of 209 ± 1 and 141 ± 2 GPa by “linearized” BM-EoS approach. The axial compressibilities of a-axis and c-axis are β a = 1.59 × 10−3 GPa−1 and β c = 2.36 × 10−3 GPa−1 with an anisotropic ratio of β a :β c = 0.67:1.00. On the other hand, the pressure–volume–temperature (P–V–T) EoS of the natural beryl has also been measured at temperatures up to 750 K and at pressures up to 16.81 GPa, using diamond anvil cell in conjunction with in situ synchrotron angle-dispersive powder X-ray diffraction. The P–V data at room temperature and at a pressure range of 0.0001–15.84 GPa were then analyzed by third-order BM-EoS and yielded V 0 = 675.3 ± 0.1 Å3, K 0 = 180 ± 2 GPa, \(K_{0}^{{\prime }}\) = 4.2 ± 0.3. With \(K_{0}^{{\prime }}\) fixed to 4.0, we also obtained V 0 = 675.2 ± 0.1 Å3 and K 0 = 182 ± 1 GPa. Consequently, we fitted the P–V–T data with high-temperature BM-EoS approach using the resultant \(K_{0}^{{\prime }}\) (4.2) from room-temperature BM-EoS and then obtained the thermoelastic parameters of V 0 = 675.3 ± 0.2 Å3, K 0 = 180 ± 1 GPa, temperature derivative of the bulk modulus (∂K/∂T) P = −0.017 ± 0.004 GPa K−1, and thermal expansion coefficient at ambient conditions α 0 = (2.82 ± 0.74) × 10−6 K−1. Present results were also compared with previous studies for beryl. From the comparison of these fittings, we propose to constrain K 0 = 180 GPa and \(K_{0}^{{\prime }}\) = 4.2 for beryl. And we also observed that beryl exhibits anisotropic thermal expansion at relatively low temperatures, which is very consistent with previous studies. Furthermore, no phase transition was observed in the entire pressure and temperature range (up to 16.84 GPa and 750 K) of this study for the natural beryl.
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Acknowledgments
The authors would like to thank Prof. Abby Kavner for the editorial handling, two anonymous reviewers for the constructive comments and suggestions, and Su-ying Chien at the Center for High Pressure Science and Technology Advanced Research for her help in English improvements of the manuscript. This work was supported by the National Natural Science Foundation of China (Grant No. 41374107), the youth innovative technology talents program of Institute of Geochemistry, Chinese Academy of Sciences (2013, to Dawei Fan), the western doctor special fund of the West Light Foundation of Chinese Academy of Sciences (2011, to Dawei Fan). The high-temperature and high-pressure powder X-ray diffraction experiments were taken at the High Pressure Experiment Station (4W2), Beijing Synchrotron Radiation Facility (BSRF). The room-temperature and high-pressure single-crystal X-ray diffraction experiments were taken at the BL15U1 of the Shanghai Synchrotron Radiation Facility (SSRF).
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Fan, D., Xu, J., Kuang, Y. et al. Compressibility and equation of state of beryl (Be3Al2Si6O18) by using a diamond anvil cell and in situ synchrotron X-ray diffraction. Phys Chem Minerals 42, 529–539 (2015). https://doi.org/10.1007/s00269-015-0741-1
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DOI: https://doi.org/10.1007/s00269-015-0741-1