소장자료
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| 001 | 0100556354▲ | ||
| 003 | OCoLC▲ | ||
| 005 | 20230315172606▲ | ||
| 006 | m d ▲ | ||
| 007 | cr cnu---unuuu▲ | ||
| 008 | 210109s1980 njua ob 001 0 eng d▲ | ||
| 020 | ▼a9780691209401▼q(electronic bk.)▲ | ||
| 020 | ▼a0691209405▼q(electronic bk.)▲ | ||
| 020 | ▼z0691082588▲ | ||
| 020 | ▼z9780691082585▲ | ||
| 020 | ▼z069108260X▲ | ||
| 020 | ▼z9780691082608▲ | ||
| 035 | ▼a2378084▼b(N$T)▲ | ||
| 035 | ▼a(OCoLC)1229956186▲ | ||
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| 050 | 4 | ▼aQE571▼b.B47eb▲ | |
| 080 | ▼a552.5▼bBE▲ | ||
| 082 | 0 | 4 | ▼a552/.5▼222▲ |
| 083 | 0 | ▼aSedimentary rocks. Diagenesis▲ | |
| 084 | ▼a38.41▼2bcl▲ | ||
| 084 | ▼a38.28▼2bcl▲ | ||
| 084 | ▼aOB 21▼2blsrissc▲ | ||
| 084 | ▼ageo 195.1▼2rvk▲ | ||
| 100 | 1 | ▼aBerner, Robert A., ▼d1935-▲ | |
| 245 | 1 | 0 | ▼aEarly diagenesis▼h[electronic resource] :▼ba theoretical approach /▼cRobert A. Berner.▲ |
| 260 | ▼aPrinceton, N.J. :▼bPrinceton University Press, ▼c©1980.▲ | ||
| 300 | ▼a1 online resource (xii, 241 pages) :▼billustrations.▲ | ||
| 336 | ▼atext▼btxt▼2rdacontent▲ | ||
| 337 | ▼acomputer▼bc▼2rdamedia▲ | ||
| 338 | ▼aonline resource▼bcr▼2rdacarrier▲ | ||
| 490 | 1 | ▼aPrinceton series in geochemistry▲ | |
| 504 | ▼aIncludes bibliographical references (pages 225-237) and index.▲ | ||
| 505 | 0 | 0 | ▼tGeneral Theory --▼tThe General Diagenetic Equation --▼tDiagenetic Physical and Biological Processes --▼tAdvective Processes --▼tCompaction --▼tRate of deposition --▼tSome additional useful relations --▼tFactors affecting porosity and compaction --▼tDiffusion --▼tMolecular diffusion --▼tBenthic boundary diffusion --▼tBioturbation --▼tTransfer across the Sediment-Water Interface --▼tSummary of Mathematics of Diagenetic Physical and Biological Processes --▼tDiagenetic Chemical Processes I: Equilibrium, Homogeneous, and Microbial Reactions --▼tEquilibrium Processes --▼tDetermination of equilibrium --▼tSolubility equilibrium --▼tEquilibrium adsorption and ion exchange --▼tInclusion of equilibrium processes in diagenetic equations --▼tHomogeneous Reactions (Including Radioactive Decay) --▼tMicrobial (Metabolic) Reactions --▼tDiagenetic Chemical Processes II: Precipitation, Dissolution, and Authigenic Processes --▼tPrecipitation --▼tEnergetics of precipitation --▼tNucleation --▼tCrystal growth --▼tTransport-Controlled Growth --▼tSurface-Reaction Controlled Growth --▼tDissolution --▼tAuthigenic (Mineral-Diagenetic) Processes --▼tDiagenetic redistribution --▼tFlow vs diffusion --▼tPrecipitation (replacement) from an external source --▼tCausative factors in authigenic processes --▼tApplications --▼tMarine Sediments of the Continental Margins --▼tDiagenesis Within the Zone of Bioturbation --▼tDiagenesis Below the Zone of Bioturbation --▼tSulfate reduction --▼tAmmonia formation --▼tPhosphate diagenesis --▼tMethane formation --▼tPelagic (Deep-Sea) Sediments.▲ |
| 520 | 3 | ▼aThe 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.▲ | |
| 588 | 0 | ▼aPrint version record.▲ | |
| 590 | ▼aAdded to collection customer.56279.3▲ | ||
| 650 | 0 | ▼aDiagenesis.▲ | |
| 650 | 6 | ▼aDiagenèse.▲ | |
| 650 | 7 | ▼aDiagenesis.▼2fast▼0(OCoLC)fst00892271▲ | |
| 650 | 1 | 7 | ▼aDiagenese.▼2gtt▲ |
| 650 | 1 | 7 | ▼aSedimenten.▼2gtt▲ |
| 650 | 1 | 7 | ▼aBiologische aspecten.▼2gtt▲ |
| 650 | 1 | 7 | ▼aChemische producten.▼2gtt▲ |
| 650 | 7 | ▼aDiagenesis.▼2nli▲ | |
| 650 | 7 | ▼aGeochemistry.▼2nli▲ | |
| 650 | 7 | ▼aDiagenèse.▼2ram▲ | |
| 655 | 4 | ▼aElectronic books.▲ | |
| 776 | 0 | 8 | ▼iPrint version:▼aBerner, Robert A., 1935-▼tEarly diagenesis.▼dPrinceton, N.J. : Princeton University Press, ©1980▼z0691082588▼w(DLC) 80007510▼w(OCoLC)6142505▲ |
| 830 | 0 | ▼aPrinceton series in geochemistry.▲ | |
| 856 | 4 | 0 | ▼3EBSCOhost▼uhttp://search.ebscohost.com/login.aspx?direct=true&scope=site&db=nlebk&db=nlabk&AN=2378084▲ |
Early diagenesis : a theoretical approach
자료유형
국외eBook
서명/책임사항
Early diagenesis [electronic resource] : a theoretical approach / Robert A. Berner.
발행사항
Princeton, N.J. : Princeton University Press , ©1980.
형태사항
1 online resource (xii, 241 pages) : illustrations.
서지주기
Includes bibliographical references (pages 225-237) and index.
내용주기
General Theory -- The General Diagenetic Equation -- Diagenetic Physical and Biological Processes -- Advective Processes -- Compaction -- Rate of deposition -- Some additional useful relations -- Factors affecting porosity and compaction -- Diffusion -- Molecular diffusion -- Benthic boundary diffusion -- Bioturbation -- Transfer across the Sediment-Water Interface -- Summary of Mathematics of Diagenetic Physical and Biological Processes -- Diagenetic Chemical Processes I: Equilibrium, Homogeneous, and Microbial Reactions -- Equilibrium Processes -- Determination of equilibrium -- Solubility equilibrium -- Equilibrium adsorption and ion exchange -- Inclusion of equilibrium processes in diagenetic equations -- Homogeneous Reactions (Including Radioactive Decay) -- Microbial (Metabolic) Reactions -- Diagenetic Chemical Processes II: Precipitation, Dissolution, and Authigenic Processes -- Precipitation -- Energetics of precipitation -- Nucleation -- Crystal growth -- Transport-Controlled Growth -- Surface-Reaction Controlled Growth -- Dissolution -- Authigenic (Mineral-Diagenetic) Processes -- Diagenetic redistribution -- Flow vs diffusion -- Precipitation (replacement) from an external source -- Causative factors in authigenic processes -- Applications -- Marine Sediments of the Continental Margins -- Diagenesis Within the Zone of Bioturbation -- Diagenesis Below the Zone of Bioturbation -- Sulfate reduction -- Ammonia formation -- Phosphate diagenesis -- Methane formation -- Pelagic (Deep-Sea) Sediments.
요약주기
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.
주제
기타형태저록
ISBN
9780691209401 0691209405
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