Titlebook: Soil Acidity; B. Ulrich,M. E. Sumner Book 1991 Springer-Verlag Berlin Heidelberg 1991 Aluminium-Toxit?t.Boden.Bodenchemie.Bodenmineralien.

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Proton Sinks in Soil Controlling Soil Acidification,roperties. As these properties largely manifest themselves via the “carrier” agent, the soil solution, it seems logical to use the proton activity in the soil solution, or soil pH value, as the principal indicator of the status of the soil when discussing the effect of proton addition. The pH contro

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Assessing the Solubilities and Reaction Kinetics of Aluminous Minerals in Soils,lved constituents in soils and other geochemical systems. Soils are thermodynamically open systems subject to atmospheric and biological forces and do not attain overall thermodynamic equilibrium with respect to either mass or time. However, local or partial equilibrium conditions may persist for pa

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Effects of Soil Acidity on Plant Associations,ost striking is the difference in vegetation between soils rich in calcium carbonate with pH ≧ 6 [CO./carbonate-buffer range, according to Ulrich (1981)] and soils poor in calcium, with pH ≦ 4 (aluminium- and iron-buffer range). Only very few plant species grow equally well in both buffer ranges. Sp

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Book 1991 from the solubilization of inorganic oxides as well as aspects of changes in the nutrient status of soils, changes of fertility and processes leading to a transfer of acidity from soils to surface are discussed.

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resulting from the solubilization of inorganic oxides as well as aspects of changes in the nutrient status of soils, changes of fertility and processes leading to a transfer of acidity from soils to surface are discussed.978-3-642-74444-0978-3-642-74442-6