TY - JOUR
T1 - Thermodynamic properties of magnesiochloritoid
AU - Grevel, Klaus Dieter
AU - Kahl, Wolf Achim
AU - Majzlan, Juraj
AU - Navrotsky, Alexandra
AU - Lathe, Christian
AU - Fockenberg, Thomas
PY - 2005
Y1 - 2005
N2 - Calorimetric and P-V-T data of synthetic magnesiochloritoid (MgAl2SiO5(OH)2) have been obtained. The P-V-T behaviour of monoclinic and triclinic magnesiochloritoid has been determined in situ up to 8.5 GPa and 800°C using a MAX 80 cubic anvil high-pressure apparatus. The samples were mixed with vaseline to ensure hydrostatic pressure transmitting conditions; NaCl served as an internal standard for pressure calibration. By fitting a Birch-Murnaghan EOS to the data, the bulk modulus of the triclinic polytype was determined as 127.9 ± 2.1 GPa, (K' = 4), VT,0 = 456.58 Å3 exp [∫(0.304 ± 0.022) × 10-4 dT], (∂KT/∂T)P = -0.017 ± 0.009 GPa K-1. The resulting fit parameters for the monoclinic polytype are very similar. The enthal py of drop-solution was measured by high-temperature oxide melt calorimetry in two laboratories (UC Davis, California, nd Ruhr-University Bochum, Germany) using lead borate (2 PbO·B2O3) at 700°C as solvent. The resulting values were used to calculate the enthalpy of formation from the elements; -3538.9 ± 4.9 kJ mol-1 (Davis) and -3543.4 ± 6.2 kJ mol-1 (Bochum) were obtained. Heat capacity measurements of MgAl2SiO5(OH)2 were obtained by differential scanning calorimetry (DSC) in the temperature range from -10°C to 295°C. Two runs confirmed heat capacity data of Koch-Müller et al. (2002), represented by the Berman & Brown (1985) type four-term equation: Cp = (391.75 - 2585.00 × T-0.5 - 8240000.0 × T-2 + 967000000.0 × T-3) J K-1mol-1. Consistenc y of the thermodynamic data obtained for magnesiochloritoid with phase equilibrium data reported in the literature was checked by mathematical programming analysis. The best agreement was obtained with ΔfH0298 (magnesiochloritoid) = -3551.7 kJ mol-1, and S0298 (magnesiochloritoid) = 142.2 J K-1mol-1.
AB - Calorimetric and P-V-T data of synthetic magnesiochloritoid (MgAl2SiO5(OH)2) have been obtained. The P-V-T behaviour of monoclinic and triclinic magnesiochloritoid has been determined in situ up to 8.5 GPa and 800°C using a MAX 80 cubic anvil high-pressure apparatus. The samples were mixed with vaseline to ensure hydrostatic pressure transmitting conditions; NaCl served as an internal standard for pressure calibration. By fitting a Birch-Murnaghan EOS to the data, the bulk modulus of the triclinic polytype was determined as 127.9 ± 2.1 GPa, (K' = 4), VT,0 = 456.58 Å3 exp [∫(0.304 ± 0.022) × 10-4 dT], (∂KT/∂T)P = -0.017 ± 0.009 GPa K-1. The resulting fit parameters for the monoclinic polytype are very similar. The enthal py of drop-solution was measured by high-temperature oxide melt calorimetry in two laboratories (UC Davis, California, nd Ruhr-University Bochum, Germany) using lead borate (2 PbO·B2O3) at 700°C as solvent. The resulting values were used to calculate the enthalpy of formation from the elements; -3538.9 ± 4.9 kJ mol-1 (Davis) and -3543.4 ± 6.2 kJ mol-1 (Bochum) were obtained. Heat capacity measurements of MgAl2SiO5(OH)2 were obtained by differential scanning calorimetry (DSC) in the temperature range from -10°C to 295°C. Two runs confirmed heat capacity data of Koch-Müller et al. (2002), represented by the Berman & Brown (1985) type four-term equation: Cp = (391.75 - 2585.00 × T-0.5 - 8240000.0 × T-2 + 967000000.0 × T-3) J K-1mol-1. Consistenc y of the thermodynamic data obtained for magnesiochloritoid with phase equilibrium data reported in the literature was checked by mathematical programming analysis. The best agreement was obtained with ΔfH0298 (magnesiochloritoid) = -3551.7 kJ mol-1, and S0298 (magnesiochloritoid) = 142.2 J K-1mol-1.
KW - Calorimetry
KW - High-pressure
KW - Magnesiochloritoid
KW - Thermodynamics
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U2 - 10.1127/0935-1221/2005/0017-0587
DO - 10.1127/0935-1221/2005/0017-0587
M3 - Article
AN - SCOPUS:23044473360
SN - 0935-1221
VL - 17
SP - 587
EP - 598
JO - European Journal of Mineralogy
JF - European Journal of Mineralogy
IS - 4
ER -