Abstract
The pressure–volume–temperature (P–V–T) equation of state (EoS) of two natural garnet samples along spessartine–almandine (Spe–Alm) join has been measured at high temperature up to 800 K and high pressures up to 15.46 and 16.17 GPa for Spe64Alm36 and Spe38Alm62, respectively, using in situ angle-dispersive X-ray diffraction and diamond anvil cell. Analysis of room-temperature P–V data to a third-order Birch–Murnaghan EoS yields: V 0 = 1,544.4 ± 0.4 Å3, K 0 = 180 ± 3 GPa and \( K_{0}^{{\prime }} \) = 4.0 ± 0.4 for Spe38Alm62, and V 0 = 1,557.5 ± 0.3 Å3, K 0 = 176 ± 2 GPa and \( K_{0}^{{\prime }} \) = 4.0 ± 0.3 for Spe64Alm36. Fitting of our P–V–T data by means of the high-temperature third-order Birch–Murnaghan EoS gives the thermoelastic parameters: V 0 = 1,544.6 ± 0.6 Å3, K 0 = 180 ± 4 GPa, \( K_{0}^{{\prime }} \) = 4.0 ± 0.4, (∂K/∂T) P = −0.028 ± 0.005 GPa K−1 and α 0 = (3.16 ± 0.14) × 10−5 K−1 for Spe38Alm62, and V 0 = 1,557.7 ± 0.9 Å3, K 0 = 176 ± 4 GPa, \( K_{0}^{{\prime }} \) = 4.0 ± 0.5, (∂K/∂T) P = −0.029 ± 0.005 GPa K−1 and α 0 = (3.04 ± 0.16) × 10−5 K−1 for Spe64Alm36. The results confirm that almandine content increases the bulk modulus of the spessartine–almandine join following a nearly ideal mixing model. The relation between bulk modulus and almandine mole fraction (X Alm) in this garnet join is derived to be K 0(GPa) = 171.6(±2.6) + 10.9(±1.8)X Alm. Present results are also compared with previously studies determined the thermoelastic properties of other garnets.
Similar content being viewed by others
References
Akaogi M, Akimoto S (1977) Pyroxene-garnet solid-solution equilibria in the systems Mg4Si4O12–Mg3Al2Si3O12 and Fe4Si4O12–Fe3Al2Si3O12 at high pressures and temperatures. Phys Earth Planet Inter 15:90–106
Allred A (1961) Electronegativity values from thermochemical data. J Inorg Nucl Chem 17:215–221
Anderson DL, Bass JD (1984) Mineralogy and composition of the upper mantle. Geophys Res Lett 11:637–640
Angel R (2000) Equation of state. Rev Mineral Geochem 41:35–60
Anovitz LM, Essene EJ, Metz GW, Bohlen SR, Westrum EF Jr, Hemingway BS (1993) Heat capacity and phase equilibria of almandine, Fe3Al2Si3O12. Geochim Cosmochim Acta 57:4191–4204
Babuška V, Fiala J, Kumazawa M, Ohno I, Sumino Y (1978) Elastic properties of garnet solid-solution series. Phys Earth Planet Inter 16:157–176
Bass JD (1989) Elasticity of grossular and spessartite garnets by Brillouin spectroscopy. J Geophys Res 94:7621–7628
Birch F (1986) Equation of state and thermodynamic parameters of NaCl to 300 kbar in the high temperature domain. J Geophys Res 83:1257–1268
Conrad PG (1998) The stability of almandine at high pressure and temperature. Geophys Monogr Ser 101:393–400
Deer WA, Howie RA, Zussman J (1992) An introduction to the rock-forming minerals, 2nd edn. Longman, Harlow
Diella V, Sani A, Levy D, Pavese A (2004) High-pressure synchrotron X-ray diffraction study of spessartine and uvarovite: a comparison between different equation of state models. Am Mineral 89:371–376
Duffy TS, Anderson DL (1989) Seismic velocity in mantle minerals and mineralogy of the upper mantle. J Geophys Res 94:1895–1912
Dymshits AM, Litasov KD, Shatskiy A, Sharygin IS, Ohtani E, Suzuki A, Pokhilenko NP, Funakoshi K (2014) P–V–T equation of state of Na-majorite to 21 GPa and 1673 K. Phys Earth Plant Int 227:68–75
Fan DW, Zhou WG, Liu CQ, Liu YG, Wan F, Xing YS, Liu J, Bai LG, Xie HS (2009) The thermal equation of state of (Fe0.86Mg0.07Mn0.07)3Al2Si3O12 almandine. Mineral Mag 73:95–102
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
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
Gréaux S, Yamada A (2014) P–V–T equation of state of Mn3Al2Si3O12 spessartine garnet. Phys Chem Miner 41:141–149
Gréaux S, Kono Y, Nishiyama N, Kunimoto T, Wada K, Irifune T (2011) P–V–T equation of state of Ca3Al2Si3O12 grossular garnet. Phys Chem Miner 38:85–94
Gwanmesia GD, Liu J, Chen G, Kesson S, Rigden SM, Liebermann RC (2000) Elasticity of the pyrope (Mg3Al2Si3O12)–majorite (MgSiO3) garnets solid solution. Phys Chem Miner 27:445–452
Gwanmesia GD, Zhang J, Darling K, Kung J, Li B, Wang L, Neuville D, Liebermann RC (2006) Elasticity of polycrystalline pyrope Mg3Al2Si3O12 to 9 GPa and 1,000°C. Phys Earth Planet Inter 155:179–190
Gwanmesia GD, Wang L, Triplett R, Liebermann RC (2009) Pressure and temperature dependence of the elasticity of pyrope–majorite [Py60Mj40 and Py50Mj50] garnet solid solution measured by ultrasonic interferometry technique. Phys Earth Plant Inter 174:105–112
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
Huang S, Chen JH (2014) Equation of state of pyrope–almandine solid solution measured using a diamond anvil cell and in situ synchrotron X-ray diffraction. Phys Earth Planet Inter 228:88–91
Irifune T, Ringwood AE (1987) Phase transformations in a harzburgite composition to 26 GPa: implications for dynamical behaviour of the subducting slab. Earth Planet Sci Lett 86:365–376
Irifune T, Ringwood AE (1993) Phase transformation in subducted oceanic crust and buoyancy relationships at depths of 600–800 km in the mantle. Earth Planet Sci Lett 117:101–110
Ita J, Stixrude L (1992) Petrology, elasticity, and composition of the mantle transition zone. J Geophys Res 97:6849–6866
Karato S, Wang Z, Liu B, Fujino K (1995) Plastic deformation of garnets: systematics and implications for the rheology of the mantle transition zone. Earth Planet Sci Lett 130:13–30
Kono Y, Gréaux S, Higo Y, Ohfuji H, Irifune T (2010) Pressure and temperature dependences of elastic properties of grossular garnet up to 17 GPa and 1 650 K. J Earth Sci 21:782–791
Larson AC, Von Dreele RB (2000) GSAS general structure analysis system operation manual. Los Alamos Natl Lab LAUR 86–748:1–179
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
Léger JM, Redon AM, Chateau C (1990) Compressions of synthetic pyrope, spessartine and uvarovite garnets up to 25 GPa. Phys Chem Miner 17:161–167
Liu X, Shieh SR, Fleet ME, Akhmetov A (2008) High-pressure study on lead fluorapatite. Am Mineral 93:1581–1584
Nishihara Y, Takahashi E, Matsukage KN, Iguchi T, Nakayama K, Funakoshi K (2004) Thermal equation of state (Mg0.91Fe0.09)2SiO4 ringwoodite. Phys Earth Planet Inter 143–144:33–46
Nishihara Y, Aoki I, Takahashi E, Matsukage KN, Funakoshi KI (2005) Thermal equation of state of majorite with MORB composition. Phys Earth Planet Inter 148:73–84
Nobes RH, Akhmatskaya EV, Milman V, Winkler B, Pickard CJ (2000) Structure and properties of aluminosilicate garnets and katoite: an ab initio study. Comput Mater Sci 17:141–145
Nyame FK (2001) Petrological significance of manganese carbonate inclusions in spessartine garnet and relation to the stability of spessartine in metamorphosed manganese rich rocks. Contrib Mineral Petrol 141:733–746
Pavese A, Diella V, Pischedda V, Merli M, Bocchio R, Mezouar M (2001) Pressure–volume–temperature equation of state of andradite and grossular, by high-pressure and -temperature powder diffraction. Phys Chem Miner 28:242–248
Pavese A, Levy D, Curetti N, Diella V, Fumagalli P, Sani A (2003) Equation of state and compressibility of phlogopite by in situ high-pressure X-ray powder diffraction. Eur J Mineral 15:455–463
Sani A, Quartieri S, Boscherini F, Antonioli G, Feenstra A, Geiger CA (2004) Fe2+–O and Mn2+–O bonding and Fe2+- and Mn2+-vibrational properties in synthetic almandine-spessartine solid solutions: an X-ray absorption fine structure study. Eur J Mineral 16:801–808
Shannon RD (1976) Revised effective ionic-radii and systematic studies of interatomic distances in halides and chalcogenides. Acta Crystallogr Sect A 32:751–767
Toby BH (2001) EXPGUI, a graphical user interface for GSAS. J Appl Crystallogr 34:210–213
Vinet P, Ferrante J, Smith JR, Rose JH (1986) A universal equation of state for solids. J Phys C: Solid State Phys 19:L467
Vinet P, Ferrante J, Rose JH, Smith JR (1987) Compressibility of solids. J Geophys Res 92:9319–9325
Wang ZC, Ji SC (2001) Elasticity of six polycrystalline silicate garnets at pressure up to 3.0 GPa. Am Miner 86:1209–1218
Wang Y, Weidner DJ, Zhang J, Gwanmesia GD, Liebermann RC (1998) Thermal equation of state of garnets along the pyrope–majorite join. Phys Earth Planet Inter 105:59–71
Weidner DJ, Wang Y (2000) Phase transformations: implications for mantle structure. Geophys Monogr Ser 117:215–235
Yagi T, Akaogi M, Shimomura O, Tamai H, Akimoto SI (1987) High pressure and high temperature equations of state of majorite. High-pressure research in mineral physics. Geophys Monogr Ser 39:141–147
Zhang J (1999) Room-temperature compressibilities of MnO and CdO: further examination of the role of cation type in bulk modulus systematics. Phys Chem Miner 26:644–648
Zhang L, Ahsbahs H, Kutoglu A, Geiger CA (1999) Single-crystal hydrostatic compression of synthetic pyrope, almandine, spessartine, grossular and andradite garnets at high pressure. Phys Chem Miner 27:52–58
Zou Y, Gréaux S, Irifune T, Whitaker ML, Shinmei T, Higo Y (2012) Thermal equation of state of Mg3Al2Si3O12 pyrope garnet up to 19 GPa and 1700 K. Phys Chem Miner 39:589–598
Acknowledgments
This work is 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 Project of Major Research Plan of the National Natural Science Foundation (Grant No. 91014004). The high-pressure X-ray diffraction experiments were taken at the High Pressure Experiment Station (4W2), Beijing Synchrotron Radiation Facility (BSRF).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Fan, D., Xu, J., Ma, M. et al. P–V–T equation of state of spessartine–almandine solid solution measured using a diamond anvil cell and in situ synchrotron X-ray diffraction. Phys Chem Minerals 42, 63–72 (2015). https://doi.org/10.1007/s00269-014-0700-2
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00269-014-0700-2