Early Diagenesis : : A Theoretical Approach / / Robert A. Berner.

• Superior document: Title is part of eBook package: De Gruyter Princeton University Press eBook-Package Archive 1927-1999
• VerfasserIn: Berner, Robert A.,
• Place / Publishing House: Princeton, NJ : : Princeton University Press, , [2020]; ©1980
• Year of Publication: 2020
• Language: English
• Series: Princeton Series in Geochemistry ; 1
• Physical Description: 1 online resource (256 p.)
• Other title: Frontmatter --; Contents --; Preface --; List of Symbols --; 1. Introduction --; Part I. THEORY --; 2. General Theory --; 3. Diagenetic Physical and Biological Processes --; 4. Diagenetic Chemical Processes I: Equilibrium, Homogeneous, and Microbial Reactions --; 5. Diagenetic Chemical Processes II: Precipitation, Dissolution, and Authigenic Processes --; Part II. APPLICATIONS --; 6. Marine Sediments of the Continental Margins --; 7. Pelagic (Deep-Sea) Sediments --; 8. Non-Marine Sediments --; References --; Index
• Format: Mode of access: Internet via World Wide Web.
• ISBN: 9780691209401; 9783110442496
• DOI: 10.1515/9780691209401?locatt=mode:legacy
• Access: restricted access
• Hierarchical level: Monograph
• Statement of Responsibility: Robert A. Berner.

Diagenesis refers to changes taking place in sediments after deposition. In a theoretical treatment of early diagenesis, Robert Berner shows how a rigorous development of the mathematical modeling of diagenetic processes can be useful to the understanding and interpretation of both experimental and field observations. His book is unique in that the models are based on quantitative rate expressions, in contrast to the qualitative descriptions that have dominated the field.In the opening chapters, the author develops the mathematical theory of early diagenesis, introducing a general diagenetic equation and discussing it in terms of each major diagenetic process. Included are the derivations of basic rate equations for diffusion, compaction, pore-water flow, burial advection, bioturbation, adsorption, radioactive decay, and especially chemical and biochemical reactions. Drawing on examples from the recent literature on continental-margin, pelagic, and non-marine sediments, he then illustrates the power of these diagenetic models in the study of such deposits.The book is intended not only for earth scientists studying sediments and sedimentary rocks, but also for researchers in fields such as radioactive waste disposal, petroleum and economic geology, environmental pollution, and sea-floor engineering.