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Compressibility of the high-pressure polymorph of AlOOH to 17 GPa

Published online by Cambridge University Press:  05 July 2018

A. Suzuki
A. Suzuki*
Affiliation:
Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980- 8578, Japan
*
* E-mail: [email protected]
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Abstract

The equation of state of δ-AlOOH was investigated using powder X-ray diffraction up to 17 GPa. Measurement of the volume at 300 K gave a value of the bulk modulus of K0 = 124(2) GPa, whereas its pressure derivative was K’ = 13.5(7). The b axis of the unit cell is more compressible than the a and c axes – in agreement with a neutron diffraction study at high pressure by Sano-Furukawa et al. (2008). Measurements presented here show that δ-AlOOH has a compressibility 200% higher than in the previously reported equation of state by Vanpeteghem et al. (2002).

Keywords

AlOOHhigh pressureX-ray diffractionequation of state.
Type
Research Article
Information
Mineralogical Magazine , Volume 73 , Issue 3 , June 2009 , pp. 479 - 485
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

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References

Andrault, D., Angel, R.J., Mosenfelder, J.L. and Le Bihan, T. (2003) Equation of state of stishovite to lower mantle pressure. American Mineralogist, 88, 301—307.CrossRefGoogle Scholar
Decker, D.L. (1971) High-pressure equation of state for NaCl, KCl, and CsCl. Journal of Applied Physics, 42, 3239—3244.CrossRefGoogle Scholar
Kawamoto, T. and Holloway, J.R. (1997) Melting temperature and partial melt chemistry of H2O—saturated mantle peridotite to 11 gigapascals. Science, 276, 240—243.CrossRefGoogle ScholarPubMed
Komatsu, K., Kuribayashi, T., Sano, A., Ohtani, E. and Kudoh, Y. (2006) Redetermination of the high- pressure modification of AlOOH from single-crystal synchrotron data. Acta Crystallographica E, 62, i216—i218.Google Scholar
Li, S., Ahuja, R. and Johansson, B. (2006) The elastic and optical properties of the high—pressure hydrous phase 5-AlOOH. Solid State Communications, 137, 101 — 106.CrossRefGoogle Scholar
Miura, H. (2003) CellCalc: A unit-cell parameter refinement program on Windows computer. Journal of the Crystallographic Society of Japan, 45, 145 — 147.CrossRefGoogle Scholar
Momma, K. and Izumi, F. (2008) VESTA: a threedimensional visualization system for electronic and structural analysis. Journal of Applied Crystallography, 41, 653—658.CrossRefGoogle Scholar
Ohtani, E., Litasov, K., Suzuki, A. and Kondo, T. (2001) Stability field of new hydrous phase, δ-AlOOH, with implications for water transport into the deep mantle. Geophysical Research Letters, 28, 3991—3993.CrossRefGoogle Scholar
Ono, S. (1998) Stability of hydrous minerals in sediment and mid-ocean ridge basalt compositions: implications for water transport in subduction zones. Journal of Geophysical Research, 103, 18253-18267 .CrossRefGoogle Scholar
Panero, W.R. and Stixrude, L.P. (2004) Hydrogen incorporation in stishovite at high pressure and symmetric hydrogen bonding in δ-AlOOH. Earth and Planetary Science Letters, 221, 421-431 .CrossRefGoogle Scholar
Rapp, R.P., Irifune, T., Shimizu, N., Nishiyama, N., Norman, M.D. and Inoue, T. (2008) Subduction recycling of continental sediments and the origin of geochemically enriched reservoirs in the deep mantle. Earth and Planetary Science Letters, 271, 14-23 .CrossRefGoogle Scholar
Ringwood, A.E. and Major, A. (1967) High-pressure reconnaissance investigations in the system Mg2SiO4-MgO-H2O. Earth and Planetary Science Letters, 2, 130-133 .CrossRefGoogle Scholar
Ross, N.L., Shu, J.-F., Hazen, R.M. and Gasparik, T. (1990) High-pressure crystal chemistry of stishovite. American Mineralogist, 75, 739-747 .Google Scholar
Rosso, K.M. and Rustad, J.R. (2001) Structures and energies of AlOOH and FeOOH polymorphs from plane wave pseudopotential calculations. American Mineralogist, 86, 312-317 .CrossRefGoogle Scholar
Sano, A., Ohtani, E., Kubo, T. and Funakoshi, K. (2004) In situ X-ray observation of decomposition of hydrous aluminum silicate AlSiO3OH and aluminum oxide hydroxide δ-AlOOH at high pressure and temperature. Journal of Physics and Chemistry of Solids, 65, 1547-1554 .CrossRefGoogle Scholar
Sano, A., Ohtani, E., Kondo, T., Hirao, N., Sakai, T., Sata, N., Ohishi, Y. and Kikegawa, T. (2008) Aluminous hydrous mineral δ-AlOOH as a carrier of hydrogen into the core-mantle boundary. Geophysical Research Letters, 35, L03303.CrossRefGoogle Scholar
Sano-Furukawa, A., Komatsu, K., Vanpeteghem, C.B. and Ohtani, E. (2008) Neutron diffraction study of δ- AlOOH at high pressure and its implication for symmetrization of the hydrogen bond. American Mineralogist, 93, 1558-1567 .CrossRefGoogle Scholar
Suzuki, A., Ohtani, E. and Kamada, T. (2000) A new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000°C. Physics and Chemistry of Minerals, 27, 689-693 .CrossRefGoogle Scholar
Tsuchiya, J., Tsuchiya, T., Tsuneyuki, S. and Yamanaka, T. (2002) First principles calculation of a high- pressure hydrous phase, δ-AlOOH. Geophysical Research Letters, 29, 1909.CrossRefGoogle Scholar
Tsuchiya, J., Tsuchiya, T. and Tsuneyuki, S. (2005) First-principles study of hydrogen bond symmetriza- tion of phase D under high pressure. American Mineralogist, 90, 44-49 .CrossRefGoogle Scholar
Utsumi, W., Funakoshi, K., Katayama, Y., Yamakata, M., Okada, T. and Shimomura, O. (2002) High- pressure science with a multi-anvil apparatus at SPring-8. Journal of Physics: Condensed Matter, 14, 10497-10504 .Google Scholar
Vanpeteghem, C.B., Ohtani, E. and Kondo, T. (2002) Equation of state of the hydrous phase δ-AlOOH at room temperature up to 22.5 GPa. Geophysical Research Letters, 29, 1119, DOI:10.1029/ 2001GL014224.CrossRefGoogle Scholar
Vanpeteghem, C.B., Sano, A., Komatsu, K., Ohtani, E. and Suzuki, A. (2007) Neutron diffraction study of aluminous hydroxide δ-AlOOH. Physics and Chemistry of Minerals, 34, 657-661 .CrossRefGoogle Scholar
Vielzeuf, D. and Schmidt, M.W. (2001) Melting relations in hydrous systems revisited: application to metapelites, metagreywackes and metabasalts. Contributions to Mineralogy and Petrology, 141, 251-267 .CrossRefGoogle Scholar
Xue, X. and Kanzaki, M. (2007) High-pressure phase S- Al(OH)3 and δ-AlOOH phases and isostructural hydroxides/oxyhydroxides: new structural insights from high-resolution 1H and 27Al NMR. The Journal of Physical Chemistry B, 111, 13156-13166 .CrossRefGoogle Scholar
Xue, X., Kanzaki, M., Fukui, H., Ito, E. and Hashimoto, T. (2006) Cation order and hydrogen bonding of high pressure phases in the Al2O3-SiO2-H2O system: an NMR and Raman study. American Mineralogist, 91, 850 861.CrossRefGoogle Scholar