Titlebook: Geochemistry at the Earth’s Surface; Movement of Chemical Andreas Bauer,Bruce D. Velde Book 2014 Springer-Verlag Berlin Heidelberg 2014

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Transport: Water and Wind,gases, oxygen and CO.) and unstable silicate minerals coming from rocks. The material formed by alteration is then “processed” by plants in the soil zone where different chemical constraints can be imposed such as changes in Eh and pH. The fine grained material, clays and oxides and some more coarse

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https://doi.org/10.1007/978-3-642-91421-8are deposited and become essentially closed systems isolated from the surface chemical effects of air and rainwater where the sediments will be subjected to changes in pressure and temperature. The basic context of surface geochemistry is that of element migration and change under different chemical