000			03587nam a22005055i 4500
001			978-0-387-73563-4
003			DE-He213
005			20250710084017.0
007			cr nn 008mamaa
008			100715s2008 xxu| s |||| 0|eng d
020			_a9780387735634 _a99780387735634
024	7		_a10.1007/978-0-387-73563-4 _2doi
082	0	4	_a551.9 _223
100	1		_aBrantley, Susan L. _eeditor.
245	1	0	_aKinetics of Water-Rock Interaction _h[recurso electrónico] / _cedited by Susan L. Brantley, James D. Kubicki, Art F. White.
264		1	_aNew York, NY : _bSpringer New York, _c2008.
300			_bonline resource.
336			_atext _btxt _2rdacontent
337			_acomputer _bc _2rdamedia
338			_arecurso en línea _bcr _2rdacarrier
347			_atext file _bPDF _2rda
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.
650		0	_aGEOGRAPHY.
650		0	_aLIFE SCIENCES.
650		0	_aGEOCHEMISTRY.
650		0	_aHYDRAULIC ENGINEERING.
650		0	_aSOIL CONSERVATION.
650		0	_aSURFACES (PHYSICS).
650	1	4	_aEARTH SCIENCES.
650	2	4	_aGEOCHEMISTRY.
650	2	4	_aSURFACES AND INTERFACES, THIN FILMS.
650	2	4	_aBIOGEOSCIENCES.
650	2	4	_aHYDROGEOLOGY.
650	2	4	_aSOIL SCIENCE & CONSERVATION.
700	1		_aKubicki, James D. _eeditor.
700	1		_aWhite, Art F. _eeditor.
710	2		_aSpringerLink (Online service)
773	0		_tSpringer eBooks
776	0	8	_iPrinted edition: _z9780387735627
856	4	0	_uhttp://dx.doi.org/10.1007/978-0-387-73563-4 _zVer el texto completo en las instalaciones del CICY
912			_aZDB-2-EES
942			_2ddc _cER
999			_c58480 _d58480