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Titlebook: Applied Mineralogical Thermodynamics; Selected Topics Niranjan D. Chatterjee Textbook 1991 Springer-Verlag Berlin Heidelberg 1991 Kristallc

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期刊全稱Applied Mineralogical Thermodynamics
期刊簡(jiǎn)稱Selected Topics
影響因子2023Niranjan D. Chatterjee
視頻videohttp://file.papertrans.cn/160/159965/159965.mp4
圖書(shū)封面Titlebook: Applied Mineralogical Thermodynamics; Selected Topics Niranjan D. Chatterjee Textbook 1991 Springer-Verlag Berlin Heidelberg 1991 Kristallc
影響因子Thermodynamic treatment of mineral equilibria, a topic central to mineralogical thermodynamics, can be traced back to the tum of the century, when J. H. Van‘t Hoff and his associates pioneered in applying thermodynamics to the mineral assemblages observed in the Stassfurt salt deposit. Although other renowned researchers joined forces to develop the subject - H. E. Boeke even tried to popularize it by giving an overview of the early developments in his "Grundlagen der physikalisch-chemischen Petrographie", Berlin, 1915 - it remained, on the whole, an esoteric subject for the majority of the contemporary geological community. Seen that way, mineralogical thermodynamics came of age during the last four decades, and evolved very rapidly into a mainstream discipline of geochemistry. It has contributed enormously to our understanding of the phase equilibria of mineral systems, and has helped put mineralogy and petrology on a firm quantitative basis. In the wake of these developments, academic curricula now require the students of geology to take a course in basic thermodynamics, traditionally offered by the departments of chemistry. Building on that foundation, a supplementary course is
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,Abkürzungen und Formelzeichnen,f time and space, most such processes are not accessible to direct observation, but they can be reconstructed by deciphering the physicochemical frameworks of formation of rocks and mineral deposits which formed in response to them. Supposing the observed mineral assemblage preserved in a rock recor
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,L?ndergruppen und Entwicklungspfade, without a pure fluid or a fluid mixture. Yet another subject, which can be handled at the present stage, is the derivation of an internally consistent thermodynamic database, which is indispensable for obtaining a geologically reliable phase diagram. However, the computation of the phase relations
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https://doi.org/10.1007/978-3-642-77665-6t is also geologically relevant, because the natural fluids are mixtures of a number of species including H.O, CO., CH., etc. The computation of the mixed-volatile equilibria demands that the thermodynamic properties of the fluid mixtures be known. Accordingly, research work on the equations of stat
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