Principles of Stable Isotope Distribution

Author:   Robert E. Criss (Professor, Department of Earth and Planetary Sciences, Professor, Department of Earth and Planetary Sciences, Washington University, St Louis, Missouri)
Publisher:   Oxford University Press Inc
ISBN:  

9780195117752


Pages:   264
Publication Date:   29 July 1999
Format:   Hardback
Availability:   To order   Availability explained
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Principles of Stable Isotope Distribution


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Author:   Robert E. Criss (Professor, Department of Earth and Planetary Sciences, Professor, Department of Earth and Planetary Sciences, Washington University, St Louis, Missouri)
Publisher:   Oxford University Press Inc
Imprint:   Oxford University Press Inc
Dimensions:   Width: 16.40cm , Height: 1.80cm , Length: 24.30cm
Weight:   0.467kg
ISBN:  

9780195117752


ISBN 10:   0195117751
Pages:   264
Publication Date:   29 July 1999
Audience:   Professional and scholarly ,  Professional & Vocational
Format:   Hardback
Publisher's Status:   Active
Availability:   To order   Availability explained
Stock availability from the supplier is unknown. We will order it for you and ship this item to you once it is received by us.

Table of Contents

1: Abundance and Measurement of Stable Isotopes 1.1: Discovery of Isotopes 1.2: Nuclide Types, Abundances, and Atomic Weights 1.3: Properties and Fractionation of Isotopic Molecules 1.4: Material Balance Relationships 1.5: Mass Spectrometers 1.6: Notation and Standards 1.7: Summary 1.8: Problems References 2: Isotopic Exchange and Equilibrium Fractionation 2.1: Isotopic Exchange Reactions 2.2: Basic Equations 2.3: Molecular Models 2.4: Theory of Isotopic Fractionation 2.5: Temperature Dependence of Isotopic Fractionation Factors 2.6: Rule of the Mean 2.7: Isotopic Thermometers 2.8: Summary 2.9: Problems References 3: Isotope Hydrology 3.1: Variations of D and (1)]8O in the Hydrosphere 3.2: Variations of D and (1)]8O in Waters from Deep Geologic Environments 3.3: Liquid-Vapor and Ice-Vapor Equilibria 3.4: Rayleigh Fractionation 3.5: Examples of Natural Meteoric Precipitation 3.6: Isotopic Variations in Streamflow 3.7: Isotopic Variations in Groundwaters 3.8: Summary 3.9: Problems References 4: Nonequilibrium Fractionation and Isotopic Transport 4.1: Kinetics of Isotopic Exchange 4.2: Examples of Isotopic Exchange Kinetics 4.3: Evaporation 4.4: Lake Balance 4.5: Isotopic Flux and Soil Evaporation 4.6: Kinetic Fractionation Factors 4.7: Isotopic Distribution in the Atmosphere 4.8: Mass-Independent Fractionation 4.9: Summary 4.10: Problems References 5: Igneous Rocks, Meteorites, and Fluid-Rock Interactions 5.1: Oxygen and Hydrogen Isotope Geochemistry of Rocks 5.2: Igneous Rocks: Primary Crystallization 5.3: Igneous Rocks: Subsolidus Processes 5.4: Hydrothermal Systems 5.5: Extraterrestrial Oxygen and Hydrogen Isotopic Compositions 5.6: Summary 5.7: Problems References Appendices A.1 Important Nuclides of Light Elements A.2 Selected Physical Constants A.3 Definitions, Formulas, and Approximations A.4 Selected Oxygen Isotope Fractionation Factors between Various Phases and Water Index

Reviews

<br> Reacting to what he sees as an unfortunate migration of funding from fundamental scientific research to applications deemed politically important, Criss seeks to reconnect the diverse observations of isotope distributions to the quantitative theories of physical chemistry emphasized by earlier scientists. Instead of case histories, which he cites only when they exemplify quantitative principles or convey new and important possibilities, he offers translations of the principles of statistical and classical thermodynamics, kinetics, and diffusion theory into the language of isotope distribution, the fundamental variable of which is the isotope ration. --SciTech Book News<p><br>


Reacting to what he sees as an unfortunate migration of funding from fundamental scientific research to applications deemed politically important, Criss seeks to reconnect the diverse observations of isotope distributions to the quantitative theories of physical chemistry emphasized by earlier scientists. Instead of case histories, which he cites only when they exemplify quantitative principles or convey new and important possibilities, he offers translations of the principles of statistical and classical thermodynamics, kinetics, and diffusion theory into the language of isotope distribution, the fundamental variable of which is the isotope ration. --SciTech Book News<br>


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