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The equation of state of lawsonite to 7 GPa and 873 K, and calculation of its high pressure stability

  • N. Chinnery EMAIL logo , A.R. Pawley and S.M. Clark
Published/Copyright: March 26, 2015
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American Mineralogist
From the journal American Mineralogist Volume 85 Issue 7-8

Abstract

The volume of lawsonite, CaAl2Si2O7(OH)2 · H2O, has been measured up to 7 GPa and 873 K using in situ energy dispersive powder diffraction and a multi-anvil high pressure-temperature cell at the Synchrotron Radiation Source, Daresbury Laboratory, U.K. Measurements were made on isotherms at 298, 323, 373, 473, 573, 673, 773, and 873 K within the pressure range. Sample pressure was measured from a NaCl standard mixed with the sample; the unit-cell volume of lawsonite was taken from the same diffraction pattern. The data gave an ambient temperature isothermal bulk modulus of K298 112 ± 6 GPa, similar to previous values. This value overestimates the temperature stability of lawsonite in thermodynamic calculations. A fit of the Birch-Murnaghan equation of state to the whole high pressure and temperature data set gave an isothermal bulk modulus of K298 = 125 ±5 GPa and a dK/dT of -0.01 ± 0.01/K, with K1 set to a value of 4 and the expansivity set to 3.16 × 10-5/K. Using these values to calculate the pressure-temperature positions of three of lawsonite’s dehydration reactions improved the agreement between observed and calculated positions of the lawsonite dehydration reactions to within experimental and calculation error. This work shows that the ambient temperature bulk modulus and ambient pressure expansivity do not adequately describe the volume behavior of lawsonite at combined high pressure and temperature.

Received: 1999-3-3
Accepted: 2000-2-7
Published Online: 2015-3-26
Published in Print: 2000-7-1

© 2015 by Walter de Gruyter Berlin/Boston

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  7. Uptake of aqueous Pb by Cl-, F–, and OH– apatites: Mineralogic evidence for nucleation mechanisms
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  9. Single-crystal thermometric calibration of Fe-Mg order-disorder in pigeonites
  10. TEM observations on the P1̄ -I1̄ phase transition in feldspars along the join CaAl2Si2O8-SrAl2Si2O8
  11. Phase transitions induced by solid solution in stuffed derivatives of quartz: A powder synchrotron XRD study of the LiAlSiO4-SiO2 join
  12. The transformation of andalusite to mullite and silica: Part I. Transformation mechanism in [001]A direction
  13. The transformation of andalusite to mullite and silica: Part II. Transformation mechanisms in [100]A and [010]A directions
  14. Structure and twinning of tetragonal Ca3Mn2Ge3O12 garnet
  15. The equation of state of lawsonite to 7 GPa and 873 K, and calculation of its high pressure stability
  16. Boron K-edge XANES of borate and borosilicate minerals
  17. 113Cd double-resonance NMR as a probe of clay mineral cation exchange sites
  18. Solid state NMR study of oxygen site exchange and Al-O-Al site concentration in analcime
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https://doi.org/10.2138/am-2000-0715

Articles in the same Issue

  1. Application of new experimental and garnet Margules data to the garnet-biotite geothermometer
  2. Volumes of mixing in aluminosilicate garnets: Solid solution and strain behavior
  3. Cerium anomaly and Th/U fractionation in the 1.85 Ga Flin Flon Paleosol: Clues from REE- and U-rich accessory minerals and implications for paleoatmospheric reconstruction
  4. Os solubility in silicate melts: New efforts and results
  5. Enstatite-forsterite-water equilibria at elevated temperatures and pressures
  6. The OH-F substitution in synthetic pargasite at 1.5 kbar, 850 °C
  7. Uptake of aqueous Pb by Cl-, F–, and OH– apatites: Mineralogic evidence for nucleation mechanisms
  8. Temperature dependence of the hyperfine parameters of synthetic P21/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join
  9. Single-crystal thermometric calibration of Fe-Mg order-disorder in pigeonites
  10. TEM observations on the P1̄ -I1̄ phase transition in feldspars along the join CaAl2Si2O8-SrAl2Si2O8
  11. Phase transitions induced by solid solution in stuffed derivatives of quartz: A powder synchrotron XRD study of the LiAlSiO4-SiO2 join
  12. The transformation of andalusite to mullite and silica: Part I. Transformation mechanism in [001]A direction
  13. The transformation of andalusite to mullite and silica: Part II. Transformation mechanisms in [100]A and [010]A directions
  14. Structure and twinning of tetragonal Ca3Mn2Ge3O12 garnet
  15. The equation of state of lawsonite to 7 GPa and 873 K, and calculation of its high pressure stability
  16. Boron K-edge XANES of borate and borosilicate minerals
  17. 113Cd double-resonance NMR as a probe of clay mineral cation exchange sites
  18. Solid state NMR study of oxygen site exchange and Al-O-Al site concentration in analcime
  19. Isomorphous substitution effect on the vibration frequencies of hydroxyl groups in molecular cluster models of the clay octahedral sheet
  20. Molecular modeling of the structure and dynamics of the interlayer and surface species of mixed-metal layered hydroxides: Chloride and water in hydrocalumite (Friedel’s salt)
  21. VIII(Mg,Fe)0.85VI(Mg,Fe)4IV(Fe,Ge)3O12: A new tetragonal phase and its comparison with garnet
  22. Rietveld analysis of dicalcium aluminate (Ca2Al2O5) – A new high pressure phase with the Brownmillerite-type structure
  23. Suredaite, PbSnS3, a new mineral species, from the Pirquitas Ag-Sn deposit, NW-Argentina: mineralogy and crystal structure
  24. Kozoite-(Nd), Nd(CO3)(OH), a new mineral in an alkali olivine basalt from Hizen-cho, Saga Prefecture, Japan
  25. Florenskyite, FeTiP, a new phosphide from the Kaidun meteorite
  26. Letters. Computer simulation of high-temperature, forsterite-melt partitioning
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