Kinetics water rock interaction (16 Ergebnisse)

Paperback. Zustand: Very Good.

Zustand: New. pp. xvii + 569 Illus.

Hardcover. Zustand: Gut. 569 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w04929 9780939950843 Sprache: Englisch Gewicht in Gramm: 1100.

Paperback. Zustand: Brand New. 588 pages. 9.02x6.18x1.38 inches. In Stock.

Zustand: New. In English.

Zustand: New. 2018. Paperback. . . . . . Books ship from the US and Ireland.

Taschenbuch. Zustand: Neu. Thermodynamics and Kinetics of Water-Rock Interaction | Jacques Schott (u. a.) | Taschenbuch | XVII | Englisch | 2018 | Boston | EAN 9780939950843 | Verantwortliche Person für die EU: Walter de Gruyter GmbH, De Gruyter GmbH, Genthiner Str. 13, 10785 Berlin, productsafety[at]degruyterbrill[dot]com | Anbieter: preigu. …

hardcover. Zustand: Very Good.

Zustand: New. In English.

Zustand: New. In English.

Taschenbuch. Zustand: 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.…

Gebunden. Zustand: New. 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.

Taschenbuch. Zustand: 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.…

Hardcover. Zustand: Brand New. 1st edition. 833 pages. 9.50x6.25x1.75 inches. In Stock.

Buch. Zustand: Neu. 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.…

Zustand: New. pp. 868.