Hostname: page-component-78c5997874-m6dg7 Total loading time: 0 Render date: 2024-11-15T23:22:09.920Z Has data issue: false hasContentIssue false
  • English
  • Français

Thermal expansion of andalusite and sillimanite at ambient pressure: a powder X-ray diffraction study up to 1000°C

Published online by Cambridge University Press:  05 July 2018

X. Hu ,
X. Liu ,
Q. He ,
H. Wang ,
S. Qin ,
L. Ren ,
C. M. Wu  and
L. Chang
X. Hu
Affiliation:
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China, Beijing 100871, China School of Earth and Space Sciences, Peking University, Beijing 100871, China
X. Liu*
Affiliation:
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China, Beijing 100871, China School of Earth and Space Sciences, Peking University, Beijing 100871, China
Q. He
Affiliation:
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China, Beijing 100871, China School of Earth and Space Sciences, Peking University, Beijing 100871, China
H. Wang
Affiliation:
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China, Beijing 100871, China School of Earth and Space Sciences, Peking University, Beijing 100871, China
S. Qin
Affiliation:
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China, Beijing 100871, China School of Earth and Space Sciences, Peking University, Beijing 100871, China
L. Ren
Affiliation:
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
C. M. Wu
Affiliation:
College of Earth Science, the Graduate School, Chinese Academy of Sciences, Beijing 100049, China
L. Chang
Affiliation:
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China, Beijing 100871, China School of Earth and Space Sciences, Peking University, Beijing 100871, China
*
*E-mail: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

The unit-cell parameters of andalusite and sillimanite have been measured by high-T powder X-ray diffraction up to 1000°C at ambient pressure. Within the temperature range investigated, all the unit-cell parameters varied smoothly, indicating no phase transition. The volume-temperature data were fitted with a polynomial expression for the thermal expansion coefficient (αT = a0 + a1T + a2T-2). yielding a0 = 2.55(2) × 10–5K–1, al = 0 and a2 = 0 for andalusite, and a0 = 1.40(4) × 10–5K–1a1 = 7.1(8) × 10–9K–2 and a2 = 0 for sillimanite. Using the new thermal expansion data determined in the present study and compressional data from the literature, the P-T phase relations of the kyanite-andalusite-sillimanite system were calculated thermodynamically, with the invariant point located at ∼523°C and 3.93 kbar.

Keywords

andalusitehigh temperaturepowder X-ray diffractionsillimanitethermal expansion
Type
CNMNC Newsletter 8
Information
Mineralogical Magazine , Volume 75 , Issue 2 , April 2011 , pp. 363 - 374
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2011

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Beger, R.M. (1979) Aluminum-silicon ordering in sillimanite and mullite. PhD thesis, Harvard University, Massachusetts, USA, 312 pp. Berman R.G. (1988) Internally-consistent thermodynamic data forminer als in the system Na2O-K2OCaO- MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2 . Journal of Petrology, 29, 445-522.Google Scholar
Brace, W.F., Scholz, C.H. and La Mori, P.N. (1969) Isothermal compressibility of kyanite, andalusite, and sillimanite from synthetic aggregates. Journal of Geophysical Research, 74, 2089-2098.CrossRefGoogle Scholar
Burt, J.B., Ross, N.L., Angel, R.J. and Koch, M. (2006) Equations of state and structures of andalusite to 9.8 GPa and sillimanite to 8.5 GPa. American Mineralogist, 91, 319-326.CrossRefGoogle Scholar
Carpenter, M.A., Salje, E.K.H., Graeme-Barber, A., Wruck, B., Dove, M.T. and Knight, K.S. (1998) Calibration of excess thermodynamic properties and elastic constant variations associated with the α⇌β phase transition in quartz. American Mineralogist, 83, 2-22.CrossRefGoogle Scholar
Comodi, P., Zanazzi, P.F., Poli, S. and Schmidt, M.W. (1997) High-pressure behavior of kyanite: compressibility and structural deformations. American Mineralogist, 82, 452-459.CrossRefGoogle Scholar
Friedrich, A., Kunz, M., Winkler, B. and Le Bihan, T. (2004) High-pressure behavior of sillimanite and kyanite: compressibility, decomposition and indications of a new high-pressure phase. Zeitschrift für Kristallogrphie, 219, 324-329.Google Scholar
Gatta, G.D., Nestola, F. and Walter, J.M. (2006) On the thermo-elastic behaviour of kyanite: a neutron powderd iffraction study up to 1200°C. Mineralogical Magazine, 70, 309-317.CrossRefGoogle Scholar
Hazen, R.M. and Finger, L.W. (1982) Comparative Crystal Chemistry. Wiley, New York.Google Scholar
Hoisch, T.D. (1989) A muscovite-biotite geothermometer. American Mineralogist, 74, 565-572.Google Scholar
Holdaway, M.J. (1971) Stability of andalusite and the aluminum silicate phase diagram. American Journal of Science, 271, 97-131.CrossRefGoogle Scholar
Holdaway, M.J. and Mukdhopadhyay, B. (1993) A reevaluation of the stability relations of andalusite: thermochemical data and phase diagram for the alumino silicates. American Mineralogist, 78, 298-315.Google Scholar
Holland, T.J.B. and Powell, R. (1985) An internally consistent thermodynamic dataset with uncertainties and correlations: 2. Data and results. Journal of Metamorphic Geology, 3, 343-370.CrossRefGoogle Scholar
Irifune, T., Kuroda, K., Minagawa, T. and Unemoto, M. (1995) Experimental study of the decomposition of kyanite at high pressure and high temperature. Pp. 35-44 in: The Earth's Central Part: Its Structure and Dynamics (Yukutake, T., editors). Terra Scientific publishing, Tokyo.Google Scholar
Kerrick, D.M. (1990) The Al2SiO5 Polymorphs. Reviews in Mineralogy, 22. Mineralogical Society of American, Washington, D.C., 406 pp.CrossRefGoogle Scholar
Liu, L. (1974) Disproportionation of kyanite to corundum plus stishovite at high pressure and high temperature. Earth and Planetary Science Letters, 24, 224-228.CrossRefGoogle Scholar
Liu, X., Nishiyama, N., Sanehira, T., Inoue, T., Higo, Y. and Sakamoto, S. (2006) Decomposition of kyanite and solubility of Al2O3 in stishovite at high pressure and high temperature conditions. Physics and Chemistry of Minerals, 33, 711-721.CrossRefGoogle Scholar
Liu, X., Shieh, S.R., Fleet, M.E. and Zhang, L. (2009) Compressibility of a natural kyanite to 17.5 GPa. Progress in Natural Science, 19, 1281-1286.CrossRefGoogle Scholar
Liu, X., He, Q., Wang, H., Fleet, M.E. and Hu, X. (2010) Thermal expansion of kyanite at ambient pressure: an X-ray powder diffraction study up to 1000°C. Geoscience Frontiers, 1, 91-97.CrossRefGoogle Scholar
Matsui, M. (1996) Moleculardynamics study of the structures and moduli of crystals in the system CaOMgO-Al2O3-SiO2 . Physics and Chemistry of Minerals, 23, 345-353.CrossRefGoogle Scholar
Oganov, A.R. and Brodholt, J.P. (2000) High-pressure phases in the Al2SiO5 system and the problem of aluminous phase in the Earth's lower mantle: ab initio calculations. Physics and Chemistry of Minerals, 27, 430-439.CrossRefGoogle Scholar
Ono, S., Nakajima, Y. and Funakoshi, K. (2007) In situ observation of the decomposition of kyanite at high pressures and high temperatures. American Mineralogist, 92, 1624-1629.CrossRefGoogle Scholar
Ralph, R.L., Finger, L.W., Hazen, R.M. and Ghose, S. (1984) Compressibility and crystal structure of andalusite at high pressure. American Mineralogist, 69, 513-519.Google Scholar
Ren, L., Geng, Y., Wang, Y. and Zhao, Y. (2007) On the protolith of the sillimanite gneisses in the Larsemann Hills, East Antarctica. Earth Science Frontiers, 14, 75-84.Google Scholar
Ren, L., Yang, C., Wang, Y., Liu, X. and Zhao, Y. (2009) Formation of sillimanite in the high-grade quartzofeldspathic gneisses and its relations with deformation-metamorphism-anatexis: a case study in the Larsemann Hills, East Antarctica. Acta Petrologica Sinica, 25, 1937-1946.Google Scholar
Robie, R.A. and Hemingway, B.S. (1995) Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar(105 pascals) pressure and at high temperatures. US Geological Survey Bulletin, 2131, 461 pp.Google Scholar
Schmidt, M.W., Poli, S., Comodi, P. and Zanazzi, P.F. (1997) High-pressure behavior of kyanite: decomposition of kyanite into stishovite and corundum. American Mineralogist, 82, 460-466.CrossRefGoogle Scholar
Skinner, B.J., Clark, S.P. and Appleman, D.E. (1961) Molarvolumes and thermal expansions of andalusite, kyanite, and sillimanite. American Journal of Science, 259, 651-668.CrossRefGoogle Scholar
Todd, S.S. (1950) Heat capacities at low temperatures and entropies at 298.16 K of andalusite, kyanite, and sillimanite. Journal of the American Chemical Society, 72, 4742-4743.CrossRefGoogle Scholar
Vaughan, M.T. and Weidner, D.J. (1978) The relationship of elasticity and crystal structure in andalusite and sillimanite. Physics and Chemistry of Minerals, 3, 133-144.CrossRefGoogle Scholar
Whitney, D.L. (2002) Coexisting andalusite, kyanite, and sillimanite: sequential formation of three Al2SiO5 polymorphs during progressive metamorphism near the triple point, Sivrihisar, Turkey. American Mineralogist, 87, 405-416.CrossRefGoogle Scholar
Winkler, B., Hytha, M., Warren, M.C., Milman, V., Gale, J.D. and Schreuer, J. (2001) Calculation of the elastic constants of the Al2SiO5 polymorphs andalusite, sillimanite and kyanite. Zeitschrift für Kristallogrphie, 216, 67-70.Google Scholar
Winter, J.K. and Ghose, S. (1979) Thermal expansion and high-temperature crystal chemistry of the Al2SiO5 polymorphs. American Mineralogist, 64, 573-586.Google Scholar
Yang, H., Downs, R.T., Finger, L.W., Hazen, R.M. and Prewitt, C.T. (1997a) Compressibility and crystal structure of kyanite, Al2SiO5, at high pressure. American Mineralogist, 82, 467-474.CrossRefGoogle Scholar
Yang, H., Hazen, R.M., Finger, L.W., Prewitt, C.T. and Downs, R.T. (1997b) Compressibility and crystal structure of sillimanite, Al2SiO5, at high pressure. Physics and Chemistry of Minerals, 25, 39-47.CrossRefGoogle Scholar
Zhou, S. and Feng, Z. (1999) Mineralogical characteristics and usage of macrocrystal andalusite from Xixia, Henan. Mineral Resources and Geology, 13, 40-43.Google Scholar