000764009 000__ 02902cam\a2200445Ii\4500 000764009 001__ 764009 000764009 005__ 20230306142354.0 000764009 006__ m\\\\\o\\d\\\\\\\\ 000764009 007__ cr\cnunnnunnun 000764009 008__ 140905s2014\\\\gw\a\\\\ob\\\\000\0\eng\d 000764009 019__ $$a891386495 000764009 020__ $$a9783642313592$$q(electronic book) 000764009 020__ $$a3642313590$$q(electronic book) 000764009 020__ $$z9783642313585 000764009 0247_ $$a10.1007/978-3-642-31359-2$$2doi 000764009 035__ $$aSP(OCoLC)ocn890012002 000764009 035__ $$aSP(OCoLC)890012002$$z(OCoLC)891386495 000764009 040__ $$aGW5XE$$beng$$erda$$epn$$cGW5XE$$dYDXCP$$dUPM$$dCOO$$dOCLCQ$$dOCLCF$$dE7B$$dEBLCP$$dDEBSZ$$dOCLCQ 000764009 049__ $$aISEA 000764009 050_4 $$aQE515 000764009 08204 $$a551.9$$223 000764009 1001_ $$aBauer, Andreas,$$d1969-$$eauthor. 000764009 24510 $$aGeochemistry at the Earth's surface :$$bmovement of chemical elements /$$cAndreas Bauer, Bruce D. Velde. 000764009 264_1 $$aHeidelberg :$$bSpringer,$$c2014. 000764009 300__ $$a1 online resource (xiii, 315 pages) 000764009 336__ $$atext$$btxt$$2rdacontent 000764009 337__ $$acomputer$$bc$$2rdamedia 000764009 338__ $$aonline resource$$bcr$$2rdacarrier 000764009 504__ $$aIncludes bibliographical references. 000764009 5050_ $$aGeology and chemistry at the surface -- Elements in solution -- Weathering: the initial transition to surface materials and the beginning of surface geochemistry -- Soils: Retention and movement of elements at the interface -- Transport: water and wind -- Sediments. 000764009 506__ $$aAccess limited to authorized users. 000764009 520__ $$aGeochemistry at the surface of the earth is dominated by two somewhat antagonistic forces: chemical reactions which attempt to attain a steady state (equilibrium) and geological movement of materials in time and space which changes the parameters that control chemical equilibrium. Another aspect that is extremely important to earth surface geochemistry is the effect of plants on the chemical and physical stability of materials (soils). Plant systems in fact work against the normal chemical changes (loss of silica, potassium, etc.) and the normal physical changes (stabilizing fine grained materials (clays) in the surface zones to avoid erosion). Biological effects are clearly seen in redox effects in the various parts of the earth surface movement cycle; soil formation, stream transport, sedimentation. This book attempts to outline these different parameters and their interactions as they affect earth surface geochemistry in order to give a better understanding of movement and accumulation of elements at the surface of the earth. 000764009 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed Sep. 5, 2014). 000764009 650_0 $$aGeochemistry. 000764009 7001_ $$aVelde, B.$$q(Bruce),$$eauthor. 000764009 77608 $$iPrint version:$$z9783642313585 000764009 852__ $$bebk 000764009 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-642-31359-2$$zOnline Access$$91397441.1 000764009 909CO $$ooai:library.usi.edu:764009$$pGLOBAL_SET 000764009 980__ $$aEBOOK 000764009 980__ $$aBIB 000764009 982__ $$aEbook 000764009 983__ $$aOnline 000764009 994__ $$a92$$bISE