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Early diagenesis : a theoretical approach /
The approach to diagenesis in this book is unorthodox in that it is entirely on the third level. This means that diagenesis is described quantitatively in terms of mathematical rate expression. Our goals will be to develop theoretical models, based on a combination of sediment observations and a pri...
| Clasificación: | Libro Electrónico |
|---|---|
| Autor principal: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Princeton, N.J. :
Princeton University Press,
c1980.
|
| Colección: | Princeton series in geochemistry.
|
| Temas: | |
| Acceso en línea: | Texto completo |
MARC
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| 072 | 7 | |a SCI019000 |2 bisacsh | |
| 080 | |a 552.5 |b BE | ||
| 082 | 0 | 0 | |a 552/.5 |
| 083 | 0 | |a Sedimentary rocks. Diagenesis | |
| 084 | |a 38.41 |2 bcl | ||
| 084 | |a 38.28 |2 bcl | ||
| 084 | |a OB 21 |2 blsrissc | ||
| 084 | |a geo 195.1 |2 rvk | ||
| 049 | |a UAMI | ||
| 100 | 1 | |a Berner, Robert A., |d 1935- | |
| 245 | 1 | 0 | |a Early diagenesis : |b a theoretical approach / |c Robert A. Berner. |
| 260 | |a Princeton, N.J. : |b Princeton University Press, |c c1980. | ||
| 300 | |a 1 online resource (xii, 241 p.) | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 347 | |a text file |b PDF |2 rda | ||
| 490 | 1 | |a Princeton series in geochemistry | |
| 504 | |a Bibliography: p. [225]-237. | ||
| 500 | |a Includes index. | ||
| 588 | |a Description based on print version record and CIP data provided by publisher; resource not viewed. | ||
| 505 | 0 | 0 | |t General Theory -- |t The General Diagenetic Equation -- |t Diagenetic Physical and Biological Processes -- |t Advective Processes -- |t Compaction -- |t Rate of deposition -- |t Some additional useful relations -- |t Factors affecting porosity and compaction -- |t Diffusion -- |t Molecular diffusion -- |t Benthic boundary diffusion -- |t Bioturbation -- |t Transfer across the Sediment-Water Interface -- |t Summary of Mathematics of Diagenetic Physical and Biological Processes -- |t Diagenetic Chemical Processes I: Equilibrium, Homogeneous, and Microbial Reactions -- |t Equilibrium Processes -- |t Determination of equilibrium -- |t Solubility equilibrium -- |t Equilibrium adsorption and ion exchange -- |t Inclusion of equilibrium processes in diagenetic equations -- |t Homogeneous Reactions (Including Radioactive Decay) -- |t Microbial (Metabolic) Reactions -- |t Diagenetic Chemical Processes II: Precipitation, Dissolution, and Authigenic Processes -- |t Precipitation -- |t Energetics of precipitation -- |t Nucleation -- |t Crystal growth -- |t Transport-Controlled Growth -- |t Surface-Reaction Controlled Growth -- |t Dissolution -- |t Authigenic (Mineral-Diagenetic) Processes -- |t Diagenetic redistribution -- |t Flow vs diffusion -- |t Precipitation (replacement) from an external source -- |t Causative factors in authigenic processes -- |t Applications -- |t Marine Sediments of the Continental Margins -- |t Diagenesis Within the Zone of Bioturbation -- |t Diagenesis Below the Zone of Bioturbation -- |t Sulfate reduction -- |t Ammonia formation -- |t Phosphate diagenesis -- |t Methane formation -- |t Pelagic (Deep-Sea) Sediments. |
| 520 | 3 | |a The approach to diagenesis in this book is unorthodox in that it is entirely on the third level. This means that diagenesis is described quantitatively in terms of mathematical rate expression. Our goals will be to develop theoretical models, based on a combination of sediment observations and a priori reasoning, which describe and interrelate in a quantitative manner the various diagenetic processes that affect a given sediment property during early diagensis. Although many important diagenetic problems will be addressed, it is not our purpose to discuss each mineral type, sediment type, etc., in terms of natural observations and thermodynamic equilibrium (levels one and two). The topics covered in the last three chapters are chosen merely to illustrate the power of the mathematical models developed in the previous three chapters and not to provide a survey either of diagenetic processes or of the products of these processes. Thus, the scope of the book is narrow but very deep. This is done partly out of necessity because much of the rate data upon which diagenetic models must rest has not yet been obtained | |
| 546 | |a In English | ||
| 590 | |a Knovel |b ACADEMIC - Earth Sciences | ||
| 590 | |a JSTOR |b Books at JSTOR Demand Driven Acquisitions (DDA) | ||
| 590 | |a JSTOR |b Books at JSTOR Evidence Based Acquisitions | ||
| 650 | 0 | |a Diagenesis. | |
| 650 | 6 | |a Diagenèse. | |
| 650 | 7 | |a SCIENCE / Earth Sciences / General. |2 bisacsh | |
| 650 | 7 | |a Diagenesis. |2 fast |0 (OCoLC)fst00892271 | |
| 650 | 1 | 7 | |a Diagenese. |2 gtt |
| 650 | 1 | 7 | |a Sedimenten. |2 gtt |
| 650 | 1 | 7 | |a Biologische aspecten. |2 gtt |
| 650 | 1 | 7 | |a Chemische producten. |2 gtt |
| 650 | 7 | |a Diagenesis. |2 nli | |
| 650 | 7 | |a Geochemistry. |2 nli | |
| 650 | 7 | |a Diagenèse. |2 ram | |
| 776 | 0 | 8 | |i Print version: |t Early diagenesis |d Princeton, N.J. : Princeton University Press, c1980. |z 0691082588 : |w (DLC) 80007510 |
| 830 | 0 | |a Princeton series in geochemistry. | |
| 856 | 4 | 0 | |u https://appknovel.uam.elogim.com/kn/resources/kpEDATA005/toc |z Texto completo |
| 938 | |a EBSCOhost |b EBSC |n 2378084 | ||
| 938 | |a YBP Library Services |b YANK |n 16665723 | ||
| 938 | |a ProQuest Ebook Central |b EBLB |n EBL6128558 | ||
| 938 | |a Askews and Holts Library Services |b ASKH |n AH37294136 | ||
| 938 | |a De Gruyter |b DEGR |n 9780691209401 | ||
| 994 | |a 92 |b IZTAP | ||