LEADER 03842nam 2200661 a 450 001 9910811745303321 005 20200520144314.0 010 $a1-281-21678-X 010 $a9786611216788 010 $a0-387-73563-1 024 7 $a10.1007/978-0-387-73563-4 035 $a(CKB)1000000000410645 035 $a(EBL)338031 035 $a(OCoLC)233971378 035 $a(SSID)ssj0000187502 035 $a(PQKBManifestationID)11177546 035 $a(PQKBTitleCode)TC0000187502 035 $a(PQKBWorkID)10136501 035 $a(PQKB)11635021 035 $a(DE-He213)978-0-387-73563-4 035 $a(MiAaPQ)EBC338031 035 $a(Au-PeEL)EBL338031 035 $a(CaPaEBR)ebr10222979 035 $a(CaONFJC)MIL121678 035 $a(PPN)123736897 035 $a(EXLCZ)991000000000410645 100 $a20070911d2008 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 00$aKinetics of water-rock interaction /$fedited by Susan L. Brantley, James D. Kubicki, Art F. White 205 $a1st ed. 2008. 210 $aNew York $cSpringer Verlag$dc2008 215 $a1 online resource (852 p.) 300 $aDescription based upon print version of record. 311 $a0-387-73562-3 320 $aIncludes bibliographical references and index. 327 $aAnalysis of Rates of Geochemical Reactions -- Transition State Theory and Molecular Orbital Calculations Applied to Rates and Reaction Mechanisms in Geochemical Kinetics -- The Mineral-Water Interface -- Kinetics of Sorption?Desorption -- Kinetics of Mineral Dissolution -- Data Fitting Techniques with Applications to Mineral Dissolution Kinetics -- Nucleation, Growth, and Aggregation of Mineral Phases: Mechanisms and Kinetic Controls -- Microbiological Controls on Geochemical Kinetics 1: Fundamentals and Case Study on Microbial Fe(III) Oxide Reduction -- Microbiological Controls on Geochemical Kinetics 2: Case Study on Microbial Oxidation of Metal Sulfide Minerals and Future Prospects -- Quantitative Approaches to Characterizing Natural Chemical Weathering Rates -- Geochemical Kinetics and Transport -- Isotope Geochemistry as a Tool for Deciphering Kinetics of Water-Rock Interaction -- Kinetics of Global Geochemical Cycles. 330 $aSystems at the surface of the Earth are continually responding to energy inputs derived from solar radiation or from the radiogenic heat in the interior. These energy inputs drive plate movements and erosion, exposing metastable mineral phases at the Earth?s surface. In addition, these energy fluxes are harvested and transformed by living organisms. As long as these processes persist, chemical disequilibrium at the Earth?s surface will be perpetuated. Chemical disequilibrium is also driven by human activities related to production of food, extraction of water and energy resources, and burial of wastes. To understand how the surface of the Earth will change over time, we must understand the rates at which reactions occur and the chemical feedbacks that relate these reactions across extreme temporal and spatial scales. This book addresses fundamental and applied questions concerning the rates of water-rock interactions driven by tectonic, climatic, and anthropogenic forcings. 606 $aWater-rock interaction 606 $aGeochemistry 606 $aHydrogeology 615 0$aWater-rock interaction. 615 0$aGeochemistry. 615 0$aHydrogeology. 676 $a552.06 701 $aBrantley$b Susan Louise$01661011 701 $aKubicki$b James David$01661012 701 $aWhite$b Art F$01200105 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910811745303321 996 $aKinetics of water-rock interaction$94016653 997 $aUNINA