Skip to main content
Log in

Raman spectra of sillimanite, andalusite, and kyanite at various temperatures

  • Original Paper
  • Published:
Physics and Chemistry of Minerals Aims and scope Submit manuscript

Abstract

High-temperature Raman spectra of natural sillimanite, andalusite and kyanite were measured in the temperature range of 296–1273 K at ambient pressure. No phase transition was observed over the temperature range in this study. Raman modes for the three samples vary with temperature linearly. The temperature and pressure dependence of the force constants for Si–O stretching vibrations in Al2SiO5 polymorphs were determined. The isobaric mode Grüneisen parameters of sillimanite, andalusite, and kyanite were determined from the temperature dependent of present high-temperature Raman spectra and previous results of thermal expansion coefficients. The intrinsic anharmonic mode parameters were estimated and nonzero, indicating the existence of intrinsic anharmonicity for sillimanite, andalusite and kyanite. Based on Kieffer model, the thermodynamic parameters, including isochoric heat capacity and entropy, were calculated.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Aguilar-Santillan J, Cuenca-Alvarez R, Balmori-Ramirez H, Bradt RC (2002) Mechanical activation of the decomposition and sintering of kyanite. J Am Ceram Soc 85:2425–2431

    Google Scholar 

  • Bell PM (1963) Aluminum silicate system: experimental determination of the triple point. Science 139:1055–1056

    Google Scholar 

  • Birch F (1961) The velocity of compressional waves in rocks to 10 kilobars: 2. J Geophys Res 66:2199–2224

    Google Scholar 

  • Bohlen SR, Montana A, Kerrick DM (1991) Precise determinations of the equilibria kyanite-sillimanite and kyanite-andalusite and a revised triple point for Al2SiO5 polymorphs. Am Mineral 76:677–680

    Google Scholar 

  • Brace WF, Scholz CH, La Mori PN (1969) Isothermal compressibility of kyanite, andalusite, and sillimanite from synthetic aggregates. J Geophys Res 74:2089–2098

    Google Scholar 

  • Bradt RC (2008) The sillimanite minerals: andalusite, kyanite, and sillimanite. In: Shackelford JF, Doremus RH (eds) Ceramic and glass materials. Springer, Boston, pp 41–48

    Google Scholar 

  • Burnham CW (1963a) Refinement of the crystal structure of sillimanite. Z Kristallogr 118:127–148

    Google Scholar 

  • Burnham CW (1963b) Refinement of the crystal structure of kyanite. Z Kristallogr 118:337–360

    Google Scholar 

  • Burnham CW, Buerger MJ (1961) Refinement of the crystal structure of kyanite. Z Kristallogr 115:269–290

    Google Scholar 

  • Burt JB, Ross NL, Angel RJ, Koch M (2006) Equations of state and structures of andalusite to 9.8 GPa and sillimanite to 8.5 GPa. Am Mineral 91:319–326

    Google Scholar 

  • Comodi P, Zanazzi PF, Poli S, Schmidt MW (1997) High-pressure behavior of kyanite: Compressibility and structural deformations. Am Mineral 82:452–459

    Google Scholar 

  • Fei Y (1995) Thermal expansion. In: Ahrens TJ (ed) Mineral physics and crystallography: a handbook of physical constants, vol 2. American Geophysical Union, Washington, pp 29–44

    Google Scholar 

  • Fortes AD (2019) Thermal expansion of the Al2SiO5 polymorphs, kyanite, andalusite and sillimanite, between 10 and 1573 K determined using time-of-flight neutron powder diffraction. Phys Chem Miner 46:687–704

    Google Scholar 

  • Friedrich A, Kunz M, Winkler B, Le Bihan T (2004) High-pressure behavior of sillimanite and kyanite: compressibility, decomposition and indications of a new high-pressure phase. Z Kristallogr 219:324–329

    Google Scholar 

  • Gatta GD, Nestola F, Walter JM (2006) On the thermo-elastic behaviour of kyanite: a neutron powder diffraction study up to 1200 ℃. Mineral Mag 70:309–317

    Google Scholar 

  • Gillet P, Guyot F, Malezieux JM (1989) High-pressure, high-temperature Raman spectroscopy of Ca2GeO4 (olivine form): some insights on anharmonicity. Phys Earth Planet Inter 58:141–154

    Google Scholar 

  • Gillet P, Fiquet G, Malezieux JM, Geiger CA (1992) High-pressure and high-temperature Raman spectroscopy of end-member garnets: pyrope, grossular and andradite. Eur J Mineral 4:651–664

    Google Scholar 

  • Hemingway BS, Robie RA, Evans HT, Kenick DM (1991) Heat capacities and entropies of sillimanite, fibrolite, andalusite, kyanite, and quartz and the Al2SiO5 phase diagram. Am Mineral 76:1597–1613

    Google Scholar 

  • Hofmeister AM, Chopelas A (1991) Thermodynamic properties of pyrope and grossular from vibrational spectroscopy. Am Miner 76:880–891

    Google Scholar 

  • Holdaway MJ (1971) Stability of andalusite and the alumino-silicate phase diagram. Am J Sci 271:97–131

    Google Scholar 

  • Hu X, Liu X, He Q, Wang H, Qin S, Ren L, Chang L (2011) Thermal expansion of andalusite and sillimanite at ambient pressure: a powder X-ray diffraction study up to 1000 ℃. Mineral Mag 75:363–374

    Google Scholar 

  • Iishi K, Salje E, Werneke C (1979) Phonon spectra and rigid-ion model calculations on andalusite. Phys Chem Miner 4:173–188

    Google Scholar 

  • Irifune T, Kuroda K, Minagawa T, Unemoto M (1995) Experimental study of the decomposition of kyanite at high pressure and high temperature. In: Yukutake T (ed) The Earth’s central part: its structure and dynamics, Tokyo, pp 35–44

  • Kerrick DM (1990) The Al2SiO5 polymorphs. Reviews in mineralogy, vol 22. Mineralogical Society of American, Chantilly

    Google Scholar 

  • Kieffer SW (1979a) Thermodynamics and lattice vibrations of minerals: 1. Mineral heat capacities and their relationships to simple lattice vibrational models. Rev Geophys 17:1–19

    Google Scholar 

  • Kieffer SW (1979b) Thermodynamics and lattice vibrations of minerals: 3. Lattice dynamics and an approximation for minerals with application to simple substances and framework silicates. Rev Geophys 17:35–59

    Google Scholar 

  • Kieffer SW (1980) Thermodynamics and lattice vibrations of minerals: 4. Application to chain and sheet silicate and orthosilicates. Rev Geophys 18:862–886

    Google Scholar 

  • Kojitani H, Nishimura K, Kubo A, Sakashita M, Aoki K, Akaogi M (2003) Raman spectroscopy and heat capacity measurement of calcium ferrite type MgAl2O4 and CaAl2O4. Phys Chem Miner 30:409–415

    Google Scholar 

  • Lazarev AN (1972) Vibrational spectra and structure of silicates. Consultants Bureau, New York-London

    Google Scholar 

  • Liu LG (1974) Disproportionation of kyanite to corundum plus stishovite at high pressure and temperature. Earth Planet Sci Lett 24:224–228

    Google Scholar 

  • Liu X, Nishiyama N, Sanehira T, Inoue T, Higo Y, Sakamoto S (2006) Decomposition of kyanite and solubility of Al2O3 in stishovite at high pressure and high temperature conditions. Phys Chem Miner 33:711–721

    Google Scholar 

  • Liu X, Shieh SR, Fleet ME, Zhang L (2009) Compressibility of a natural kyanite to 17.5 GPa. Prog Nat Sci Mater 19:1281–1286

    Google Scholar 

  • Liu X, He Q, Wang H, Fleet ME, Hu X (2010) Thermal expansion of kyanite at ambient pressure: an X-ray powder diffraction study up to 1000 ℃. Geosci Front 1:91–97

    Google Scholar 

  • Lv MD (2016) Crystal structure and spectroscopy of aluminosilicate isomorphism. Dissertation, Peking University

  • Mammone JF, Sharma S (1979) Pressure and temperature dependence of the Raman spectra of rutile-structure oxides. Carnegie Institution Year Book, Washington, pp 369–373

    Google Scholar 

  • Matsui M (1996) Molecular dynamics study of the structures and moduli of crystals in the system CaO-MgO-Al2O3–SiO2. Phys Chem Miner 23:345–353

    Google Scholar 

  • McMillan P, Piriou B (1982) The structures and vibrational spectra of crystals and glasses in the silica-alumina system. J Non Cryst Solids 53:279–298

    Google Scholar 

  • Mernagh TP, Liu LG (1991) Raman spectra from the Al2SiO5 polymorphs at high pressures and room temperature. Phys Chem Miner 18:126–130

    Google Scholar 

  • Momma K, Izumi F (2011) VESTA 3 for three-dimensional visualization of crystal, volumetric and morphology data. J Appl Crystallogr 44:1272–1276

    Google Scholar 

  • Nakamoto K (2009) Infrared and raman spectra of inorganic and coordination compounds. Part B: applications in coordination, organometallic, and bioinorganic chemistry, 6th Edition, Wiley

  • Náray-Szabo S, Taylor WH, Jackson WW (1929) The structure of kyanite. Z Kristallogr 71:117–130

    Google Scholar 

  • Oganov AR, Brodholt JP (2000) High-pressure phases in the Al2SiO5 system and the problem of aluminous phase in the Earth's lower mantle: ab initio calculations. Phys Chem Miner 27:430–439

    Google Scholar 

  • Okada T, Narita T, Nagai T, Yamanaka T (2008) Comparative Raman spectroscopic study on ilmenite-type MgSiO3 (akimotoite), MgGeO3, and MgTiO3 (geikielite) at high temperatures and high pressures. Am Mineral 93:39–47

    Google Scholar 

  • Ono S, Nakajima Y, Funakoshi K (2007) In situ observation of the decomposition of kyanite at high pressures and high temperatures. Am Mineral 92:1624–1629

    Google Scholar 

  • Pan F, Yu XH, Mo XX, You JL, Wang C, Chen H, Jiang GC (2006) Raman active vibrations of aluminosilicates. Spectrosc Spect Anal 26:1871–1875

    Google Scholar 

  • Pankratz LB, Kelley KK (1964) High temperature heat contents and entropies of andalusite, kyanite and sillimanite. US Bur Mines Rep Invest 1964:6370

    Google Scholar 

  • Ralph RL, Finger LW, Hazen RM, Ghose S (1984) Compressibility and crystal structure of andalusite at high pressure. Am Mineral 69:513–519

    Google Scholar 

  • Rao MN, Chaplot SL, Choudhury N, Rao KR, Azuah RT, Montfrooij WT, Bennington SM (1999) Lattice dynamics and inelastic neutron scattering from sillimanite and kyanite Al2SiO5. Phys Rev B 60:12061–12068

    Google Scholar 

  • Reynard B, Price GD, Gillet P (1992) Thermodynamic and anharmonic properties of forsterite, α-Mg2SiO4: computer modelling versus high-pressure and high-temperature measurements. J Geophys Res 97:19791–19801

    Google Scholar 

  • Richardson SW, Gilbert MC, Bell PM (1969) Experimental determination of kyanite-andalusite and andalusite-sillimanite equilibria; the aluminum silicate triple point. Am J Sci 267:259–272

    Google Scholar 

  • Robie RA, Hemingway BS (1984) Entropies of kyanite, andalusite, and sillimanite: additional constraints on the pressure and temperature of the Al2SiO5 triple point. Am Mineral 69:298–306

    Google Scholar 

  • Salje E (1986) Heat capacities and entropies of andalusite and sillimanite: the influence of fibrolitization on the phase diagram of the Al2SiO5 polymorphs. Am Mineral 71:1366–1371

    Google Scholar 

  • Salje E, Werneke C (1982) The phase equilibrium between sillimanite and andalusite as determined from lattice vibrations. Contrib Mineral Petrol 79:56–67

    Google Scholar 

  • Schmidt MW, Poli S, Comodi P, Zanazzi PF (1997) High-pressure behavior of kyanite: decomposition of kyanite into stishovite and corundum. Am Mineral 82:460–466

    Google Scholar 

  • Schneider H, Majdic A (1979) Kinetics and mechanism of the solid state high temperature transformation of andalusite (Al2SiO5) into 3/2 mullite, 3Al2O3·2SiO2, and silica, SiO2. Ceramurgia Int 5:31–36

    Google Scholar 

  • Schneider H, Majdic A (1980) Kinetics of the thermal decomposition of kyanite. Ceram Int 6:32–37

    Google Scholar 

  • Schneider H, Majdic A (1981) Preliminary investigation on the kinetics of the high-temperature transformation of sillimanite to 3/2 mullite, 3Al2O3·2SiO2, and silica, SiO2, and comparison with the behavior of andalusite and kyanite. Sci Ceram 11:191–196

    Google Scholar 

  • Skinner BJ, Clark SP, Appleman DE (1961) Molar volumes and thermal expansions of andalusite, kyanite, and sillimanite. Am J Sci 259:651–668

    Google Scholar 

  • Taylor WH (1928) The structure of sillimanite and mullite. Z Kristallogra 68:503–521

    Google Scholar 

  • Taylor WH (1929) The structure of andalusite, Al2SiO5. Z Kristallogr 71:205–218

    Google Scholar 

  • Todd SS (1950) Heat capacities at low temperatures and entropies at 298.16° K of andalusite, kyanite, and sillimanite. J Am Chem Soc 72:4742–4743

    Google Scholar 

  • Vaughan MT, Weidner DJ (1978) The relationship of elasticity and crystal structure in andalusite and sillimanite. Phys Chem Miner 3:133–144

    Google Scholar 

  • Winkler B, Hytha M, Warren MC, MilmanV GJD, Schreuer J (2001) Calculation of the elastic constants of the Al2SiO5 polymorphs andalusite, sillimanite and kyanite. Z Kristallogr 216:67–70

    Google Scholar 

  • Winter JK, Ghose S (1979) Thermal expansion and high-temperature crystal chemistry of the Al2SiO5 polymorphs. Am Mineral 64:573–586

    Google Scholar 

  • Wu C, Zhao G (2007) The metapelitic garnet-biotite-muscovite-aluminosilicate- quartz (GBMAQ) geobarometer. Lithos 97:365–372

    Google Scholar 

  • Xue W, Zhai K, Lin CC, Zhai S (2018) Effect of temperature on the Raman spectra of Ca5(PO4)3F fluorapatite. Eur J Mineral 30:951–956

    Google Scholar 

  • Yang H, Downs RT, Finger LW, Hazen RM, Prewitt CT (1997a) Compressibility and crystal structure of kyanite, Al2SiO5, at high pressure. Am Mineral 82:467–474

    Google Scholar 

  • Yang H, Hazen RM, Finger LW, Prewitt CT, Downs RT (1997b) Compressibility and crystal structure of sillimanite, Al2SiO5, at high pressure. Phys Chem Miner 25:39–47

    Google Scholar 

  • Zhou Y, Irifune T, Ohfuji H, Kuribayashi T (2018) New high-pressure forms of Al2SiO5. Geophys Res Lett 45:8167–8172

    Google Scholar 

Download references

Acknowledgements

This work was financially supported by the National Natural Science Foundation of China (Grant No. 41872045). We thank Dr. H. Yang at the University of Arizona for providing us with studied samples from the RRUFF Project.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Weihong Xue.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Zhai, K., Xue, W., Wang, H. et al. Raman spectra of sillimanite, andalusite, and kyanite at various temperatures. Phys Chem Minerals 47, 23 (2020). https://doi.org/10.1007/s00269-020-01092-9

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s00269-020-01092-9

Keywords

Navigation