Thermodynamics of Minerals and Melts [electronic resource] /

Today large numbers of geoscientists apply thermodynamic theory to solu­ tions of a variety of problems in earth and planetary sciences. For most problems in chemistry, the application of thermodynamics is direct and rewarding. Geoscientists, however, deal with complex inorganic and organic substances. The complexities in the nature of mineralogical substances arise due to their involved crystal structure and multicomponental character. As a result, thermochemical solutions of many geological-planetological problems should be attempted only with a clear understanding of the crystal-chemical and thermochemical character of each mineral. The subject of physical geochemistry deals with the elucidation and application of physico-chemical principles to geosciences. Thermodynamics of mineral phases and crystalline solutions form an integral part of it. Developments in mineralogic thermody­ namics in recent years have been very encouraging, but do not easily reach many geoscientists interested mainly in applications. This series is to provide geoscientists and planetary scientists with current information on the develop­ ments in thermodynamics of mineral systems, and also provide the active researcher in this rapidly developing field with a forum through which he can popularize the important conclusions of his work. In the first several volumes, we plan to publish original contributions (with an abundant supply of back­ ground material for the uninitiated reader) and thoughtful reviews from a number of researchers on mineralogic thermodynamics, on the application of thermochemistry to planetary phase equilibria (including meteorites), and on kinetics of geochemical reactions.

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Bibliographic Details
Main Authors: Newton, R. C. editor., Navrotsky, A. editor., Wood, B. J. editor., SpringerLink (Online service)
Format: Texto biblioteca
Language:eng
Published: New York, NY : Springer New York, 1981
Subjects:Earth sciences., Inorganic chemistry., Physical chemistry., Mineralogy., Earth Sciences., Physical Chemistry., Inorganic Chemistry.,
Online Access:http://dx.doi.org/10.1007/978-1-4612-5871-1
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id KOHA-OAI-TEST:186527
record_format koha
institution COLPOS
collection Koha
country México
countrycode MX
component Bibliográfico
access En linea
En linea
databasecode cat-colpos
tag biblioteca
region America del Norte
libraryname Departamento de documentación y biblioteca de COLPOS
language eng
topic Earth sciences.
Inorganic chemistry.
Physical chemistry.
Mineralogy.
Earth Sciences.
Mineralogy.
Physical Chemistry.
Inorganic Chemistry.
Earth sciences.
Inorganic chemistry.
Physical chemistry.
Mineralogy.
Earth Sciences.
Mineralogy.
Physical Chemistry.
Inorganic Chemistry.
spellingShingle Earth sciences.
Inorganic chemistry.
Physical chemistry.
Mineralogy.
Earth Sciences.
Mineralogy.
Physical Chemistry.
Inorganic Chemistry.
Earth sciences.
Inorganic chemistry.
Physical chemistry.
Mineralogy.
Earth Sciences.
Mineralogy.
Physical Chemistry.
Inorganic Chemistry.
Newton, R. C. editor.
Navrotsky, A. editor.
Wood, B. J. editor.
SpringerLink (Online service)
Thermodynamics of Minerals and Melts [electronic resource] /
description Today large numbers of geoscientists apply thermodynamic theory to solu­ tions of a variety of problems in earth and planetary sciences. For most problems in chemistry, the application of thermodynamics is direct and rewarding. Geoscientists, however, deal with complex inorganic and organic substances. The complexities in the nature of mineralogical substances arise due to their involved crystal structure and multicomponental character. As a result, thermochemical solutions of many geological-planetological problems should be attempted only with a clear understanding of the crystal-chemical and thermochemical character of each mineral. The subject of physical geochemistry deals with the elucidation and application of physico-chemical principles to geosciences. Thermodynamics of mineral phases and crystalline solutions form an integral part of it. Developments in mineralogic thermody­ namics in recent years have been very encouraging, but do not easily reach many geoscientists interested mainly in applications. This series is to provide geoscientists and planetary scientists with current information on the develop­ ments in thermodynamics of mineral systems, and also provide the active researcher in this rapidly developing field with a forum through which he can popularize the important conclusions of his work. In the first several volumes, we plan to publish original contributions (with an abundant supply of back­ ground material for the uninitiated reader) and thoughtful reviews from a number of researchers on mineralogic thermodynamics, on the application of thermochemistry to planetary phase equilibria (including meteorites), and on kinetics of geochemical reactions.
format Texto
topic_facet Earth sciences.
Inorganic chemistry.
Physical chemistry.
Mineralogy.
Earth Sciences.
Mineralogy.
Physical Chemistry.
Inorganic Chemistry.
author Newton, R. C. editor.
Navrotsky, A. editor.
Wood, B. J. editor.
SpringerLink (Online service)
author_facet Newton, R. C. editor.
Navrotsky, A. editor.
Wood, B. J. editor.
SpringerLink (Online service)
author_sort Newton, R. C. editor.
title Thermodynamics of Minerals and Melts [electronic resource] /
title_short Thermodynamics of Minerals and Melts [electronic resource] /
title_full Thermodynamics of Minerals and Melts [electronic resource] /
title_fullStr Thermodynamics of Minerals and Melts [electronic resource] /
title_full_unstemmed Thermodynamics of Minerals and Melts [electronic resource] /
title_sort thermodynamics of minerals and melts [electronic resource] /
publisher New York, NY : Springer New York,
publishDate 1981
url http://dx.doi.org/10.1007/978-1-4612-5871-1
work_keys_str_mv AT newtonrceditor thermodynamicsofmineralsandmeltselectronicresource
AT navrotskyaeditor thermodynamicsofmineralsandmeltselectronicresource
AT woodbjeditor thermodynamicsofmineralsandmeltselectronicresource
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spelling KOHA-OAI-TEST:1865272018-07-30T23:09:26ZThermodynamics of Minerals and Melts [electronic resource] / Newton, R. C. editor. Navrotsky, A. editor. Wood, B. J. editor. SpringerLink (Online service) textNew York, NY : Springer New York,1981.engToday large numbers of geoscientists apply thermodynamic theory to solu­ tions of a variety of problems in earth and planetary sciences. For most problems in chemistry, the application of thermodynamics is direct and rewarding. Geoscientists, however, deal with complex inorganic and organic substances. The complexities in the nature of mineralogical substances arise due to their involved crystal structure and multicomponental character. As a result, thermochemical solutions of many geological-planetological problems should be attempted only with a clear understanding of the crystal-chemical and thermochemical character of each mineral. The subject of physical geochemistry deals with the elucidation and application of physico-chemical principles to geosciences. Thermodynamics of mineral phases and crystalline solutions form an integral part of it. Developments in mineralogic thermody­ namics in recent years have been very encouraging, but do not easily reach many geoscientists interested mainly in applications. This series is to provide geoscientists and planetary scientists with current information on the develop­ ments in thermodynamics of mineral systems, and also provide the active researcher in this rapidly developing field with a forum through which he can popularize the important conclusions of his work. In the first several volumes, we plan to publish original contributions (with an abundant supply of back­ ground material for the uninitiated reader) and thoughtful reviews from a number of researchers on mineralogic thermodynamics, on the application of thermochemistry to planetary phase equilibria (including meteorites), and on kinetics of geochemical reactions.I General Principles -- 1 The Operational Basis and Mathematical Derivation of the Gibbs Differential Equation, Which is the Fundamental Equation of Chemical Thermodynamics -- II Thermodynamics of Mineral Systems -- 2 Thermodynamic Analysis of Simple Mineral Systems -- 3 Lambda Transitions in Minerals -- 4 Crystal Field Electronic Effects on the Thermodynamic Properties of Fe2+ Minerals -- 5 Isotopic Thermometry -- 6 Calculation of Thermodynamic Properties of End-Member Minerals from Natural Parageneses -- 7 Thermodynamics of the Garnet—Plagioclase—AlcSiO5—Quartz Geobarometer -- 8 The Thermodynamics of the Mg2Si2O6-CaMgSi2O6 Join: A Review and an Improved Model -- III Thermodynamics of Melt Systems -- 9 Thermodynamics of Simple Molten Salt Mixtures -- 10 Thermodynamics of Mixing in Silicate Glasses and Melts -- 11 Thermodynamic Modeling of Silicate Melts -- 12 Calculating Mineral—Melt Equilibria with Stoichiometry, Mass Balance, and Single-Component Distribution Coefficients -- 13 Volatile Interactions in Magmas.Today large numbers of geoscientists apply thermodynamic theory to solu­ tions of a variety of problems in earth and planetary sciences. For most problems in chemistry, the application of thermodynamics is direct and rewarding. Geoscientists, however, deal with complex inorganic and organic substances. The complexities in the nature of mineralogical substances arise due to their involved crystal structure and multicomponental character. As a result, thermochemical solutions of many geological-planetological problems should be attempted only with a clear understanding of the crystal-chemical and thermochemical character of each mineral. The subject of physical geochemistry deals with the elucidation and application of physico-chemical principles to geosciences. Thermodynamics of mineral phases and crystalline solutions form an integral part of it. Developments in mineralogic thermody­ namics in recent years have been very encouraging, but do not easily reach many geoscientists interested mainly in applications. This series is to provide geoscientists and planetary scientists with current information on the develop­ ments in thermodynamics of mineral systems, and also provide the active researcher in this rapidly developing field with a forum through which he can popularize the important conclusions of his work. In the first several volumes, we plan to publish original contributions (with an abundant supply of back­ ground material for the uninitiated reader) and thoughtful reviews from a number of researchers on mineralogic thermodynamics, on the application of thermochemistry to planetary phase equilibria (including meteorites), and on kinetics of geochemical reactions.Earth sciences.Inorganic chemistry.Physical chemistry.Mineralogy.Earth Sciences.Mineralogy.Physical Chemistry.Inorganic Chemistry.Springer eBookshttp://dx.doi.org/10.1007/978-1-4612-5871-1URN:ISBN:9781461258711