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Wiley Surface Complexation Modeling: Gibbsite - Soil Science

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Description

Master the complexities of mineral interactions with Surface Complexation Modeling: Gibbsite by Wiley. This specialized text provides a comprehensive description of the generalized two layer surface complexation model, making it an essential resource for researchers and professionals in soil science and geochemistry. This book covers critical data treatment procedures and thermodynamic constants for the sorption of metal cations and anions on gibbsite. As the most common form of aluminum oxide in nature and one of the most abundant minerals found in soils, sediments, and natural waters, understanding gibbsite is fundamental to environmental science. Readers will find a clear synopsis of various aluminum oxide forms and a well-defined nomenclature to ensure precision in their work. The text includes detailed compilations of available data regarding the sorption of metal cations and anions, alongside the results of surface complexation model fitting. Whether you are studying natural water systems or soil composition, this book provides the technical foundation needed to model mineral-water interfaces accurately.

Key Features

Detailed explanation of the generalized two layer surface complexation model for accurate environmental modeling.

Comprehensive guide to data treatment procedures and thermodynamic constants for metal cation and anion sorption.

In-depth analysis of gibbsite, the most common aluminum oxide found in soils, sediments, and natural waters.

Clear nomenclature and a complete synopsis of various aluminum oxide forms for professional scientific use.

Extensive compilations of available data for the sorption of metal cations and anions on gibbsite surfaces.

Practical application through presented results of surface complexation model fitting for existing data sets.

Product Specifications

Brand
Wiley
Format
hardcover
Domain
Amazon UK
Release Date
27 October 2010
Listed Since
31 August 2009

Barcode

No barcode data available

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