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High-pressure IR-spectra and the thermodynamic properties of chloritoid

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Published/Copyright: March 28, 2015
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Abstract

Using IR radiation from a synchrotron source, high-quality absorbance spectra were obtained from polycrystalline powder of chloritoid (cld) from ambient conditions up to pressures of 10 GPa over 50 to 4000 cm-1. The idealized chemical composition of the chloritoid group is M2Al4O2(SiO4)2(OH)4 where M = Fe or Mg in our experiments. All of the 42 expected fundamental IR modes were observed. These data, combined with the response of the IR bands to substitutions of Fe for Mg, and of D for H, constrained the band assignments. Heat capacity (CP) and entropy (So) for the triclinic and monoclinic polymorphs of Fe- and Mg-cld were calculated from the Kieffer-type model, using our detailed band assignments. The calculated heat capacity and entropy for the monoclinic and triclinic polymorphs differ negligibly. The results at temperatures above 298 K are described by the following polynomial expressions in J/(mol·K): CP = 7.835 · 102 - 5.170 · 103T-0.5 - 1.648 · 107T-2 + 1.934 · 109T-3 for Mg-cld and CP = 7.848 · 102 - 5.185 · 103T-0.5 - 1.548 · 107T-2 + 1.783 · 109T-3 for Fe-cld. At room temperature, So = 293 J/mol·K for Mg-cld and 335 J/mol·K for Fe-cld. These values differ somewhat from entropy estimated from various internally consistent databases (-3 to -9% for Mg-cld and -9 to +5% for Fe-cld). However, using our new So and CP values in conjunction with the enthalpy of formation, Hf = -7101 kJ/mol for Mg-cld or Hf = -6422 kJ/mol for Fe-cld (estimated in this study), we can closely reproduce the experimental data for the reactions Mg-chloritoid + talc = clinochlore + kyanite (Chopin 1985) and Fe-chloritoid = almandine + diaspore + water (Vidal et al. 1994).

Received: 2001-7-31
Accepted: 2001-12-18
Published Online: 2015-3-28
Published in Print: 2002-5-1

© 2015 by Walter de Gruyter Berlin/Boston

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