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Physicochemical fate of sulfate in soils

Journal Article · · J. Air Pollut. Control Assoc.; (United States)
Sulfur occurs in soils in organic and inorganic forms, with the inorganic S accounting for <5 percent of the total S in most soils from humid and semihumid regions. Sulfate in soils may occur as water-soluble salts, adsorbed by soil colloids, or as insoluble forms. Considerable seasonal fluctuations in the concentration of soluble SO/sub 4//sup 2 -/ in surface soils occur as a result of interaction of seasonal conditions on the mineralization of organic S, leaching, and uptake by plants. Soils vary widely in their capacity to adsorb SO/sub 4//sup 2 -/. Sulfate adsorption is readily reversible and the amount SO/sub 4//sup 2 -/ adsorbed is concentration and temperature dependent. The capacity of soil to adsorb SO/sub 4//sup 2 -/ depends upon clay content, nature of clay minerals, pH, associated cation, and the amount of hydrous Al and Fe oxides. The mechanisms of SO/sub 4//sup 2 -/ retention by soils involve coordination with hydrous oxides, exchange on edges of silicate clays, incorporation in mineral structures, and molecular adsorption. For acid soils, SO/sub 4//sup 2 -/ adsorption essentially involves the chemistry of Fe and Al. Sulfate adsorption increases as the pH decreases below zero point of charge. Several forms of insoluble SO/sub 4//sup 2 -/ are likely to occur in soils, including BaSO/sub 4/, SrSO/sub 4/, SO/sub 4//sup 2 -/ associated with CaCO/sub 3/, and basic Fe and Al sulfates.
Research Organization:
Iowa State Univ., Ames
OSTI ID:
7095424
Journal Information:
J. Air Pollut. Control Assoc.; (United States), Journal Name: J. Air Pollut. Control Assoc.; (United States) Vol. 37:1; ISSN JPCAA
Country of Publication:
United States
Language:
English