Thermodynamics in Mineral Sciences An Introduction

Thermodynamics is an important tool to interpreting the conditions at which natural geomaterial equilibrate. It allows one to determine, for example, the equilibrium pressures and temperatures and the nature and chemical composition of phases - volved mineralogical and petrological processes. Simple...

Full description

Bibliographic Details
Main Author: Cemic, Ladislav
Format: eBook
Language:English
Published: Berlin, Heidelberg Springer Berlin Heidelberg 2005, 2005
Edition:1st ed. 2005
Subjects:
Online Access:
Collection: Springer eBooks 2005- - Collection details see MPG.ReNa
LEADER 02955nmm a2200349 u 4500
001 EB000373985
003 EBX01000000000000000227037
005 00000000000000.0
007 cr|||||||||||||||||||||
008 130626 ||| eng
020 |a 9783540288084 
100 1 |a Cemic, Ladislav 
245 0 0 |a Thermodynamics in Mineral Sciences  |h Elektronische Ressource  |b An Introduction  |c by Ladislav Cemic 
250 |a 1st ed. 2005 
260 |a Berlin, Heidelberg  |b Springer Berlin Heidelberg  |c 2005, 2005 
300 |a XVI, 386 p. 82 illus  |b online resource 
505 0 |a Definition of thermodynamic terms -- Volume as a state function -- The first law of thermodynamics -- Second law of thermodynamics -- Gibbs free energy and Helmholtz free energy -- Thermal equilibrium -- Chemical reactions -- Geothermometry and geobarometry 
653 |a Geology 
653 |a Complex Systems 
653 |a Chemistry, Physical and theoretical 
653 |a Mineralogy 
653 |a Thermodynamics 
653 |a Theoretical Chemistry 
653 |a System theory 
653 |a Mathematical physics 
653 |a Theoretical, Mathematical and Computational Physics 
041 0 7 |a eng  |2 ISO 639-2 
989 |b Springer  |a Springer eBooks 2005- 
028 5 0 |a 10.1007/3-540-28808-2 
856 4 0 |u https://doi.org/10.1007/3-540-28808-2?nosfx=y  |x Verlag  |3 Volltext 
082 0 |a 549 
520 |a Thermodynamics is an important tool to interpreting the conditions at which natural geomaterial equilibrate. It allows one to determine, for example, the equilibrium pressures and temperatures and the nature and chemical composition of phases - volved mineralogical and petrological processes. Simple chemical model systems, which are often studied in the laboratory in order to understand more complicated natural systems, generally consist of few chemical components. In order to use phase equilibrium results obtained from model systems for interpreting the con- tions of formation of natural geologic materials, extrapolations in compositional space and other P-T conditions are often required. This can only be done using the mathematical formalism that is offered by thermodynamics. An number of excellent books on thermodynamics with regards to the fields of mineralogy, petrology and geochemistry have been published over past 40 years. Many of them are, however, written for more advanced students and experienced - searchers and it is often assumed that the reader already possesses some prior knowledge of the subject. Consequently, discussions and presentations of basic c- cepts, which are necessary for beginning students and others attempting to learn thermodynamics for the first time, are often given short shrift. Therefore, the aim of this book is to explain the basic principles of thermodynamics at an introductory l- el, while trying not to loose much of the mathematical rigor that is one of the most important and central aspects of this subject