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000 namKi
001 2210080897411
003 OCoLC
005 20210225115021
006 m d
007 cr cnu---unuuu
008 210109s1980 njua ob 001 0 eng d
020 a9780691209401q(electronic bk.)
020 a0691209405q(electronic bk.)
020 z0691082588
020 z9780691082585
020 z069108260X
020 z9780691082608
035 a2378084b(NT)
035 a(OCoLC)1229956186
040 aNbengerdaepncNd221008
050 aQE571b.B47eb
080 a552.5bBE
082 a552/.5222
083 aSedimentary rocks. Diagenesis
084 a38.412bcl
084 a38.282bcl
084 aOB 212blsrissc
084 ageo 195.12rvk
100 aBerner, Robert A.,d1935-
245 00 aEarly diagenesis :ba theoretical approach /cRobert A. Berner.
260 aPrinceton, N.J. :bPrinceton University Press,c짤1980.
300 a1 online resource (xii, 241 pages) :billustrations.
336 atextbtxt2rdacontent
337 acomputerbc2rdamedia
338 aonline resourcebcr2rdacarrier
490 aPrinceton series in geochemistry
504 aIncludes bibliographical references (pages 225-237) and index.
505 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 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 aPrint version record.
590 aAdded to collection customer.56279.3
650 aDiagenesis.
650 aDiagene?se.
650 aDiagenesis.2fast0(OCoLC)fst00892271
650 aDiagenese.2gtt
650 aSedimenten.2gtt
650 aBiologische aspecten.2gtt
650 aChemische producten.2gtt
650 aDiagenesis.2nli
650 aGeochemistry.2nli
650 aDiagene?se.2ram
655 aElectronic books.
776 iPrint version:aBerner, Robert A., 1935-tEarly diagenesis.dPrinceton, N.J. : Princeton University Press, 짤1980z0691082588w(DLC) 80007510w(OCoLC)6142505
830 aPrinceton series in geochemistry.
856 3EBSCOhostuhttp://search.ebscohost.com/login.aspx?direct=true&scope=site&db=nlebk&db=nlabk&AN=2378084
938 aEBSCOhostbEBSCn2378084
994 a92bN
Early diagenesis :a theoretical approach /Robert A. Berner
종류
전자책
서명
Early diagenesis :a theoretical approach /Robert A. Berner
저자명
발행사항
Princeton, N.J. : Princeton University Press 짤1980.
형태사항
1 online resource (xii, 241 pages) : illustrations.
주기사항
Includes bibliographical references (pages 225-237) and index. / 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.
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