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020 _a9780387735634
_99780387735634
024 7 _a10.1007/9780387735634
_2doi
035 _avtls000332383
039 9 _a201509030226
_bVLOAD
_c201404122126
_dVLOAD
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040 _aMX-SnUAN
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_cMX-SnUAN
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050 4 _aQE514-516.5
100 1 _aBrantley, Susan L.
_eeditor.
_9302160
245 1 0 _aKinetics of Water-Rock Interaction /
_cedited by Susan L. Brantley, James D. Kubicki, Art F. White.
264 1 _aNew York, NY :
_bSpringer New York,
_c2008.
300 _brecurso en línea.
336 _atexto
_btxt
_2rdacontent
337 _acomputadora
_bc
_2rdamedia
338 _arecurso en línea
_bcr
_2rdacarrier
347 _aarchivo de texto
_bPDF
_2rda
500 _aSpringer eBooks
505 0 _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.
520 _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.
590 _aPara consulta fuera de la UANL se requiere clave de acceso remoto.
700 1 _aKubicki, James D.
_eeditor.
_9302161
700 1 _aWhite, Art F.
_eeditor.
_9302162
710 2 _aSpringerLink (Servicio en línea)
_9299170
776 0 8 _iEdición impresa:
_z9780387735627
856 4 0 _uhttp://remoto.dgb.uanl.mx/login?url=http://dx.doi.org/10.1007/978-0-387-73563-4
_zConectar a Springer E-Books (Para consulta externa se requiere previa autentificación en Biblioteca Digital UANL)
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999 _c278493
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