Early Diagenesis: A Theoretical ApproachPrinceton University Press, 21 aug 1980 - 241 pagina's 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. |
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Introduction | 8 |
THEORY | 8 |
General Theory | 9 |
THE GENERAL DIAGENETIC EQUATION | 13 |
Diagenetic Physical and Biological Processes | 15 |
DIFFUSION | 31 |
BIOTURBATION | 42 |
TRANSFER ACROSS THE SEDIMENTWATER INTERFACE | 53 |
APPLICATIONS | 133 |
Marine Sediments of the Continental Margins | 135 |
DIAGENESIS WITHIN THE ZONE OF BIOTURBATION | 136 |
DIAGENESIS BELOW THE ZONE OF BIOTURBATION | 148 |
Pelagic DeepSea Sediments | 178 |
OPALINE SILICA DISSOLUTION | 190 |
SUBOXIC ORGANIC MATTER DIAGENESIS | 194 |
DIAGENESIS OF RADIOISOTOPES | 198 |
SUMMARY OF MATHEMATICS OF DIAGENETIC PHYSICAL AND BIOLOGICAL PROCESSES | 55 |
Diagenetic Chemical Processes I Equilibrium Homogeneous and Microbial Reactions | 57 |
HOMOGENEOUS REACTIONS INCLUDING RADIOACTIVE DECAY | 77 |
MICROBIAL METABOLIC REACTIONS | 81 |
Diagenetic Chemical Processes II Precipitation Dissolution and Authigenic Processes | 90 |
DISSOLUTION | 105 |
AUTHIGENIC MINERALDIAGENETIC PROCESSES | 108 |
VOLCANICSEAWATER REACTION | 202 |
NonMarine Sediments | 206 |
HYPERSALINE SEDIMENTS | 222 |
| 225 | |
| 239 | |
