The orthorhombic-hexagonal phase transformation in the system BaCO3-SrCO3 to pressures of 7000 bar |
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Authors: | S. Weinbruch H. Büttner M. Rosenhauer |
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Affiliation: | 1. Mineralogisch-Petrologisches Institut der Universit?t G?ttingen, Goldschmidtstrasse 1, W-3400, G?ttingen, Germany
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Abstract: | The orthorhombic-hexagonal phase transformation in the system BaCO3-SrCO3 has been investigated to 7000 bar by differential thermal analysis. The pressure dependence of the orthorhombic-hexagonal transformation temperature T p may be represented by the polynomial T p =933.4?443.3 · X BaCO 3+323.7 · X BaCO 3+P(8.59?2.48)·X BaCO 3 where X BaCO 3=mol fraction of witherite, P the pressure in kbar and T the temperature in °C. Lattice parameters refined by powder X-ray diffraction measurements of the orthorhombic solid solution can be fitted to a linear relationship V orthorh [Å3]=259.30+X BaCO 3 with no evidence of any excess volume. The experimental transformation temperatures are modeled by assuming a symmetric regular solution and a diffusionless transformation. |
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