Synopsis
Geochemical kinetics as a topic is now of importance to a wide range of geochemists in academia, industry, and government, and all geochemists need a rudimentary knowledge of the field. This book summarizes the fundamentals of geochemical kinetics with examples drawn especially from mineral dissolution and precipitation. It also encompasses discussion of high temperature processes and global geochemical cycle modeling. Analysis of textures of rocks, sediments, and mineral surfaces are incorporated throughout and provide a sub-theme of the book. This volume has textbook potential among upper division undergraduate and graduate students. The book will also be useful as a reference tool for practicing geochemists.
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Kinetics of Water-Rock Interaction
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Kinetics of Water-Rock Interaction (eng)
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Kinetics of Water-Rock Interaction
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Springer New York, 2016
ISBN 10 : 1493939157
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Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. All practitioners of geochemistry today need a thorough understanding of kinetics, including those in academia, government, and industryWill have textbook potential among upper division undergraduate and graduate students. The book will also be us. N° de réf. du vendeur 447955424
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Kinetics of Water-Rock Interaction
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Springer New York Aug 2016, 2016
ISBN 10 : 1493939157
ISBN 13 : 9781493939152
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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Systems at the surface of the Earth are continually responding to energy inputs - rived ultimately from radiation from the Sun or from the radiogenic heat in the - terior. These energy inputs drive plate movements and erosion, exposing metastable mineral phases at the Earth's surface. In addition, these energy uxes are harvested and transformed by living organisms. As long as these processes persist, chemical disequilibrium at the Earth's surface will be perpetuated. In addition, as human populations grow, the need to produce food, extract - ter, and extract energy resources increases. These processes continually contribute to chemical disequilibrium at the Earth surface. We therefore nd it necessary to predict how the surface regolith will change in response to anthropogenic processes as well as long-term climatic and tectonic forcings. To address these questions, we must understand the rates at which reactions occur and the chemical feedbacks that relate these reactions across extreme temporal and spatial scales. Scientists and - gineers who work on soil fertility, nuclear waste disposal, hydrocarbon production, and contaminant and CO sequestration are among the many researchers who need 2 to understand geochemical kinetics. Fundamental questions concerning the lo- term geological, climatic and biological evolution of the planet also rely on g- kinetic information. In this book, we summarize approaches toward measuring and predicting the - netics of water-rock interactions which contribute to the processes mentioned above. 868 pp. Englisch. N° de réf. du vendeur 9781493939152
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Kinetics of Water-Rock Interaction
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Taschenbuch. Etat : Neu. Kinetics of Water-Rock Interaction | Susan Brantley (u. a.) | Taschenbuch | xxiii | Englisch | 2016 | Springer US | EAN 9781493939152 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu. N° de réf. du vendeur 103425680
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Kinetics of Water-Rock Interaction
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Springer New York, Springer US Aug 2016, 2016
ISBN 10 : 1493939157
ISBN 13 : 9781493939152
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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -Systems at the surface of the Earth are continually responding to energy inputs - rived ultimately from radiation from the Sun or from the radiogenic heat in the - terior. These energy inputs drive plate movements and erosion, exposing metastable mineral phases at the Earth¿s surface. In addition, these energy uxes are harvested and transformed by living organisms. As long as these processes persist, chemical disequilibrium at the Earth¿s surface will be perpetuated. In addition, as human populations grow, the need to produce food, extract - ter, and extract energy resources increases. These processes continually contribute to chemical disequilibrium at the Earth surface. We therefore nd it necessary to predict how the surface regolith will change in response to anthropogenic processes as well as long-term climatic and tectonic forcings. To address these questions, we must understand the rates at which reactions occur and the chemical feedbacks that relate these reactions across extreme temporal and spatial scales. Scientists and - gineers who work on soil fertility, nuclear waste disposal, hydrocarbon production, and contaminant and CO sequestration are among the many researchers who need 2 to understand geochemical kinetics. Fundamental questions concerning the lo- term geological, climatic and biological evolution of the planet also rely on g- kinetic information. In this book, we summarize approaches toward measuring and predicting the - netics of water-rock interactions which contribute to the processes mentioned above.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 868 pp. Englisch. N° de réf. du vendeur 9781493939152
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Kinetics of Water-Rock Interaction
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ISBN 10 : 1493939157
ISBN 13 : 9781493939152
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Taschenbuch. Etat : Neu. Druck auf Anfrage Neuware - Printed after ordering - Systems at the surface of the Earth are continually responding to energy inputs - rived ultimately from radiation from the Sun or from the radiogenic heat in the - terior. These energy inputs drive plate movements and erosion, exposing metastable mineral phases at the Earth's surface. In addition, these energy uxes are harvested and transformed by living organisms. As long as these processes persist, chemical disequilibrium at the Earth's surface will be perpetuated. In addition, as human populations grow, the need to produce food, extract - ter, and extract energy resources increases. These processes continually contribute to chemical disequilibrium at the Earth surface. We therefore nd it necessary to predict how the surface regolith will change in response to anthropogenic processes as well as long-term climatic and tectonic forcings. To address these questions, we must understand the rates at which reactions occur and the chemical feedbacks that relate these reactions across extreme temporal and spatial scales. Scientists and - gineers who work on soil fertility, nuclear waste disposal, hydrocarbon production, and contaminant and CO sequestration are among the many researchers who need 2 to understand geochemical kinetics. Fundamental questions concerning the lo- term geological, climatic and biological evolution of the planet also rely on g- kinetic information. In this book, we summarize approaches toward measuring and predicting the - netics of water-rock interactions which contribute to the processes mentioned above. N° de réf. du vendeur 9781493939152
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