Thermodynamic Data on Oxides and Silicates
An Assessed Data Set Based on Thermochemistry and High Pressure Phase Equilibrium
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An Assessed Data Set Based on Thermochemistry and High Pressure Phase Equilibrium
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Various solid solution models were discussed by Fei et al. (1986). There are two different groups of solution models. The first group of models has their origin in the Flory-Huggins model (Flory, 1953), in whi...
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There are different sources of data available for establishing an internally consistent data set: calorimetric measurements, phase equilibrium data, measured thermophysical properties of a phase, and heat capa...
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Various techniques are adopted in the systematization, depending upon the complexity of a problem, to construct the internally consistent data base. The phases considered in this study can be classified into f...
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The high pressure phase equilibrium calculations require a special consideration of both the P-V-T properties of the solids and fluids and the high-temperature extrapolation of the heat capacity data. The appropr...
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The change in Gibbs free energy (ΔG) as a function of temperature (T) and pressure (P) can be obtained from the relations:
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Recently, through experimental study, much data have accumulated on the stability of oxides and silicates. In this chapter, an internally consistent thermodynamic data base on some oxides and silicates is pres...
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Long range order-disorder phenomena in silicates differ from those in alloys in several important respects. First, as opposed to alloys, silicates contain structural sites with definite polyhedral geometries a...
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Although important information on crystal structure and experimental phase relationship has been accumulating for decades, it is only recently that attempts have been made to use such information in understand...
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This monograph is written for advanced students and research workers in the fields of mineralogy, petrology and physical geochemistry. It introduces the reader to the popular solution theories and the special ...
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Composition of coexisting minerals occurring in rocks or in experiments are the main source of data to be used in obtaining the information on the thermodynamic behaviour of silicate crystalline solutions. It ...
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An experimental measurement of activities of components in a crystalline solution, particularly the silicates, is beset with difficulties and the measured values are subject to large errors. Therefore, obtaini...
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Orthopyroxene is one of the few important rock-forming minerals that can be considered as quasi-binary without significant loss of accuracy. Usually more than 95% of the mineral is a crystalline solution of th...
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Olivines (Fe, Mg, Ca)2Si2O4 are important constituents of many igneous and metamorphic rocks. The thermodynamic properties of olivines have been studied recently by several workers (Kitayama and Katsura, 1968; Na...
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The concept of metamorphic facies evolved through the attempts of the petrologists to distinguish the mineral assemblages formed at different P and T in the field. In several cases, the physical and chemical cond...
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Thermodynamic relations between the concentration of a component in a solution and its chemical potential and other thermodynamic functions of mixing are presented here. The details of the simplifying assumpti...
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For binary or multi-component crystalline solutions, the stability is determined by the diffusion processes. Above a certain temperature two end member crystals may form a complete crystalline solution series....
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Experimental data on the distribution of a component between two coexisting crystalline solutions at a fixed P and T for systems such as olivine and pyroxene have been collected by Nafziger and Muan (1967), Larim...