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Compressibility and equation of state of beryl (Be3Al2Si6O18) by using a diamond anvil cell and in situ synchrotron X-ray diffraction

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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 (PV) 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 c = 0.67:1.00. On the other hand, the pressure–volume–temperature (PVT) 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 PV 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 PVT 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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References

  • Adamo I, Gatta GD, Rotiroti N, Diella V, Pavese A (2008) Gemmological investigation of a synthetic blue beryl: a multi-methodological study. Miner Mag 72:799–808

    Article  Google Scholar 

  • Aines RD, Rossman GR (1984) The high-temperature behaviour of water and carbon dioxide in cordierite and beryl. Am Miner 69:319–327

    Google Scholar 

  • Andersson LO (2006) The position of H+, Li+ and Na+ impurities in beryl. Phys Chem Miner 33:403–416

    Article  Google Scholar 

  • Angel R (2000) Equation of state. Rev Miner Geochem 41:35–60

    Article  Google Scholar 

  • Angel RJ, Bujak M, Zhao J, Gatta GD, Jacobsen SD (2007) Effective hydrostatic limits of pressure media for high-pressure crystallographic studies. J Appl Crystallogr 40:26–32

    Article  Google Scholar 

  • Artioli G, Rinaldi R, Ståhl K, Zanazzi PF (1993) Structure refinements of beryl by single-crystal neutron and X-ray diffraction. Am Miner 78:762–768

    Google Scholar 

  • Aurisicchio C, Fioravanti G, Grubessi O, Zanazzi PF (1988) Reappraisal of the crystal chemistry of beryl. Am Miner 73:826–837

    Google Scholar 

  • Barton MD (1986) Phase equilibria and thermodynamic properties of minerals in the BeO–Al2O3–SiO2–H2O (BASH) system, with petrologic applications. Am Miner 71:277–300

    Google Scholar 

  • Brown GE Jr, Mills BA (1986) High-temperature structure and crystal chemistry of hydrous alkali-rich beryl from the Harding pegmatite, Taos County, New Mexico. Am Miner 71:547–556

    Google Scholar 

  • Burt DM (1978) Multisystems analysis of beryllium mineral stabilities: the system BeO–Al2O3–SiO2–H2O. Am Miner 63:664–676

    Google Scholar 

  • Čemić L, Franz G, Langer K (1986) Experimental determination of melting relationships of beryl in the system BeO–Al2O3–SiO2–H2O between 10 and 25 kbar. Miner Mag 50:55–61

    Article  Google Scholar 

  • Charoy B (1999) Beryllium speciation in evolved granitic magmas: phosphates versus silicates. Eur J Miner 11:135–148

    Article  Google Scholar 

  • Charoy B, De Donato P, Barres O, Pinto-Coelho C (1996) Channel occupancy in alkali-poor beryl from Serra Branca (Goias, Brasil): spectroscopic characterization. Am Miner 81:395–403

    Google Scholar 

  • de Almeida Sampaio Filho H, Sighinolfi G, Galli E (1973a) Contribution to crystal chemistry of beryl. Contrib Miner Petr 38:279–290

    Article  Google Scholar 

  • de Almeida Sampaio Filho H, Sighinolfi GP, Galli E (1973b) Contribution to the crystal chemistry of beryl. Contrib Miner Petrol 38:270–290

    Article  Google Scholar 

  • Dera P, Zhuravlev K, Prakapenka V, Rivers ML, Finkelstein GJ, Grubor-Urosevic O, Tschauner O, Clark SM, Downs RT (2013) High-pressure single-crystal micro-X-ray diffraction (SCμXRD) analysis with GSE_ADA/RSV software. High Press Res 33:466–484

    Article  Google Scholar 

  • Evensen JM, London D, Wendlandt RF (1999) Solubility and stability of beryl in granitic melts. Am Miner 84:733–745

    Google Scholar 

  • Fan DW, Zhou WG, Wei SY, Liu YG, Ma MN, Xie HS (2010) A simple external resistance heating diamond anvil cell and its application for synchrotron radiation x-ray diffraction. Rev Sci Instrum 81:053903

    Article  Google Scholar 

  • Fei YW, Ricolleau A, Frank M, Mibe K, Shen GY, Prakapenka V (2007) Toward an internally consistent pressure scale. Proc Natl Acad Sci 104:9182–9186

    Article  Google Scholar 

  • Gatta GD, Nestola F, Bromiley GD, Mattauch S (2006) The real topological configuration of the extra-framework content in alkali-poor beryl: a multi-methodological study. Am Miner 91:29–34

    Article  Google Scholar 

  • Gibbs GV, Breck DW, Meagher EP (1968) Structural refinement of hydrous and anhydrous synthetic beryl Al2(Be3Si6)O18 and emerald, Al1.9Cr0.1(Be3Si6)O18. Lithos 1:275–285

    Article  Google Scholar 

  • Goldman DS, Rossman GR, Parkin KM (1978) Channel constituents in beryl. Phys Chem Miner 3:225–235

    Article  Google Scholar 

  • Hammersley AP, Svensson SO, Hanfland M, Fitch AN, Hausermann D (1996) Two-dimensional detector software: from real detector to idealized image or two-theta scan. High Press Res 14:235–248

    Article  Google Scholar 

  • Hawthorne FC, Černý P (1977) The alkali-metal positions in Cs–Li beryl. Can Miner 15:414–421

    Google Scholar 

  • Hazen RM, Finger LW (1982) Comparative crystal chemistry. Wiley, New York

    Google Scholar 

  • Hazen RM, Finger LW (1987) High-temperature crystal chemistry of phenakite (Be2SiO4) and chrysoberyl (BeAl2O4). Phys Chem Miner 14:426–434

    Article  Google Scholar 

  • Hazen RM, Au AY, Finger LW (1986) High-pressure crystal chemistry of beryl (Be3Al2Si6O18) and euclase (BeAlSiO4OH). Am Miner 71:977–984

    Google Scholar 

  • Holland TJB, Redfern SAT (1997) Unit cell refinement from powder diffraction data: the use of regression diagnostics. Miner Mag 61:65–77

    Article  Google Scholar 

  • Kolesov BA, Geiger CA (2000) The orientation and vibrational states of H2O in synthetic alkali-free beryl. Phys Chem Miner 27:557–564

    Article  Google Scholar 

  • Larson AC, Von Dreele RB (2000) GSAS general structure analysis system operation manual. Los Alamos Natl Lab LAUR 86–748:1–179

    Google Scholar 

  • Le Bail A, Duroy H, Fourquet JL (1988) Ab initio structure determination of LiSbWO6 by X-ray powder diffraction. Mater Res Bull 23:447–452

    Article  Google Scholar 

  • Mao HK, Bell PM, Shaner JW, Steinberg DJ (1978) Specific volume measurements of Cu, Mo, Pd, and Ag and calibration of the ruby R1 fluorescence pressure gauge from 0.06 to 1 Mbar. J Appl Phys 49:3276–3283

    Article  Google Scholar 

  • Morosin B (1972) Structure and thermal expansion of beryl. Acta Cryst B28:1899–1903

    Article  Google Scholar 

  • Pankrath R, Langer K (2002) Molecular water in beryl, VIAl2[Be3Si6O18nH2O, as a function of pressure and temperature: an experimental study. Am Miner 87:238–244

    Google Scholar 

  • Piermarini GJ, Block S, Barnett JD (1973) Hydrostatic limits in liquids and solids to 100 kbar. J Appl Phys 44:5377–5382

    Article  Google Scholar 

  • Prencipe M, Nestola F (2005) Quantum-mechanical modeling of minerals at high pressure. The role of the Hamiltonian in a case study: the beryl (Al4Be6Si12O36). Phys Chem Miner 32:471–479

    Article  Google Scholar 

  • Prencipe M, Scanavino I, Nestola F, Merlini M, Civalleri B, Bruno M, Dovesi R (2011) High-pressure thermo-elastic properties of beryl (Al4Be6Si12O36) from ab initio calculations, and observations about the source of thermal expansion. Phys Chem Miner 38:223–239

    Article  Google Scholar 

  • Qin S, Liu J, Li HJ, Zhu XP, Li XD (2008) In-situ high-pressure X-ray diffraction of natural beryl. Chin J High Press Phys 22:1–5 (in chinese)

    Google Scholar 

  • Schlenker JL, Gibbs GV, Hill EG, Crews SS, Myers RH (1977) Thermal expansion coefficients for indialite, emerald, and beryl. Phys Chem Miner 1:243–255

    Article  Google Scholar 

  • Sheriff BL, Grundy DH, Hartman JS, Hawthorne FC, Černý P (1991) The incorporation of alkalis in beryl: multi-nuclear MAS NMR and crystal structure study. Can Miner 29:271–285

    Google Scholar 

  • Toby BH (2001) EXPGUI, a graphical user interface for GSAS. J Appl Crystallogr 34:210–213

    Article  Google Scholar 

  • Wood DL, Nassau K (1968) The characterization of beryl and emerald by visible and infrared absorption spectroscopy. Am Miner 53:777–800

    Google Scholar 

  • Yoon HS, Newnham RE (1973) The elastic properties of beryl. Acta Cryst A29:507–509

    Article  Google Scholar 

Download references

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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