The equation of state and high-pressure behaviour of a natural sample of prehnite from Kuruman, South Africa, Ca2.07(Al0.98, Mn0.02)(AlSi3.09O10)(OH)2, have been investigated using single crystal X-ray diffraction up to 9.75(3) GPa. A second-order Birch-Murnaghan equation-of-state fit to the isothermal P-V data below 8.7 GPa yields values of K0T = 109.29(18) GPa and K 0' = 4. A third-order Birch-Murnaghan equation fit to the P-V data results in K' values equal to four, within an estimated standard deviation. The compressibility of a, b, and c unit-cell parameters is non-linear and strongly anisotropic, with room-pressure moduli of Ka0 = 83.5(7) GPa, K b0 = 113(1) GPa, and KCO = 146(3) GPa and K'a0 = 4.5(3), K'b0 = 1.3(3), and K'CO = 8.8(8). Intensity data were collected over the entire pressure range. Bond lengths and angles, refined in the average space group Pncm, suggest that the structure compresses uniformly. Above 8.7 GPa there is an additional softening of the volume and the b-axis, but the average structure is maintained across the transition.

Equation of state and structure of prehnite to 9.8 GPa / T. A. Detrie, N.L. Ross, R.J. Angel, G.D. Gatta. - In: EUROPEAN JOURNAL OF MINERALOGY. - ISSN 0935-1221. - 21:3(2009 Apr), pp. 561-570. [10.1127/0935-1221/2009/0021-1924]

Equation of state and structure of prehnite to 9.8 GPa

G.D. Gatta
Ultimo
2009

Abstract

The equation of state and high-pressure behaviour of a natural sample of prehnite from Kuruman, South Africa, Ca2.07(Al0.98, Mn0.02)(AlSi3.09O10)(OH)2, have been investigated using single crystal X-ray diffraction up to 9.75(3) GPa. A second-order Birch-Murnaghan equation-of-state fit to the isothermal P-V data below 8.7 GPa yields values of K0T = 109.29(18) GPa and K 0' = 4. A third-order Birch-Murnaghan equation fit to the P-V data results in K' values equal to four, within an estimated standard deviation. The compressibility of a, b, and c unit-cell parameters is non-linear and strongly anisotropic, with room-pressure moduli of Ka0 = 83.5(7) GPa, K b0 = 113(1) GPa, and KCO = 146(3) GPa and K'a0 = 4.5(3), K'b0 = 1.3(3), and K'CO = 8.8(8). Intensity data were collected over the entire pressure range. Bond lengths and angles, refined in the average space group Pncm, suggest that the structure compresses uniformly. Above 8.7 GPa there is an additional softening of the volume and the b-axis, but the average structure is maintained across the transition.
English
Equation of state; High-pressure; Prehnite; Single crystal; X-ray diffraction
Settore GEO/06 - Mineralogia
Settore GEO/09 - Georisorse Miner.Appl.Mineral.-Petrogr.per l'amb.e i Beni Cul
Articolo
Sì, ma tipo non specificato
apr-2009
Schweizerbart'sche Verlagsbuchhandlung
21
3
561
570
Periodico con rilevanza internazionale
info:eu-repo/semantics/article
Equation of state and structure of prehnite to 9.8 GPa / T. A. Detrie, N.L. Ross, R.J. Angel, G.D. Gatta. - In: EUROPEAN JOURNAL OF MINERALOGY. - ISSN 0935-1221. - 21:3(2009 Apr), pp. 561-570. [10.1127/0935-1221/2009/0021-1924]
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Prodotti della ricerca::01 - Articolo su periodico
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262
Article (author)
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T. A. Detrie, N.L. Ross, R.J. Angel, G.D. Gatta
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/141760
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