Hardcover. Condizione: Very Good. No Jacket. May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less.
EUR 200,44
Quantità: 1 disponibili
Aggiungi al carrelloHardcover. Condizione: Like New. Like New. book.
EUR 225,54
Quantità: Più di 20 disponibili
Aggiungi al carrelloCondizione: New. In.
EUR 246,21
Quantità: Più di 20 disponibili
Aggiungi al carrelloGebunden. Condizione: 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.
EUR 351,87
Quantità: 2 disponibili
Aggiungi al carrelloHardcover. Condizione: Brand New. 1st edition. 833 pages. 9.50x6.25x1.75 inches. In Stock.
Lingua: Inglese
Editore: Springer New York Nov 2007, 2007
ISBN 10: 0387735623 ISBN 13: 9780387735627
Da: AHA-BUCH GmbH, Einbeck, Germania
EUR 305,57
Quantità: 2 disponibili
Aggiungi al carrelloBuch. Condizione: 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.