High-temperature and high-pressure equation of state for the hexagonal phase in the system NaAlSiO4 MgAl2O4

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Al-Rich Phase, Hexagonal Phase, In Situ X-Ray Diffraction, High-Temperature Equation Of State, Morb Density

Scientific paper

Thermal equation of state of an Al-rich phase with Na1.13Mg1.51Al4.47Si1.62O12 composition has been derived from in situ X-ray diffraction experiments using synchrotron radiation and a multianvil apparatus at pressures up to 24 GPa and temperatures up to 1,900 K. The Al-rich phase exhibited a hexagonal symmetry throughout the present pressure temperature conditions and the refined unit-cell parameters at ambient condition were: a=8.729(1) Å, c=2.7695(5) Å, V 0=182.77(6) Å3 ( Z=1; formula weight=420.78 g/mol), yielding the zero-pressure density ρ0=3.823(1) g/cm3 . A least-square fitting of the pressure-volume-temperature data based on Anderson’s pressure scale of gold (Anderson et al. in J Appl Phys 65:1534 543, 1989) to high-temperature Birch-Murnaghan equation of state yielded the isothermal bulk modulus K 0=176(2) GPa, its pressure derivative K {0/'}=4.9(3), temperature derivative (∂ K T /∂ T) P =-0.030(3) GPa K-1 and thermal expansivity α( T)=3.36(6)×10-5+7.2(1.9)×10-9 T, while those values of K 0=181.7(4) GPa, (∂ K T /∂ T) P =-0.020(2) GPa K-1 and α( T)=3.28(7)×10-5+3.0(9)×10-9 T were obtained when K {0/'} was assumed to be 4.0. The estimated bulk density of subducting MORB becomes denser with increasing depth as compared with earlier estimates (Ono et al. in Phys Chem Miner 29:527 531 2002; Vanpeteghem et al. in Phys Earth Planet Inter 138:223 230 2003; Guignot and Andrault in Phys Earth Planet Inter 143 44:107 128 2004), although the difference is insignificant (<0.6%) when the proportions of the hexagonal phase in the MORB compositions (˜20%) are taken into account.

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