“…In recent years, there has been an increase in S deficiency in soils for several reasons (Coleman, 1966;Haque and Walmsly, 1974b): (1) the increased use of fertilizers that are low in S; (2) the lower amount of sulfur dioxide (SOg) emissions from powerplants and industries; (3) the decreased use of S containing fungicides and pesticides; (4) the higher crop yields and thus, the greater demand for all nutrients; (5) decreased levels of organic matter due to less use of organic manures; and (6) cropping on poor soils where S can be a limiting factor for plant growth. The plant availability of SO/' in soils is controlled by the factors that affect the adsorption capacity of the soils (such as SO/" concentration, solution pH, hydrous Fe and A1 oxides, type and amount of clay minerals, and competing anions), soil texture, rainfall, drainage characteristics, and the mineralization-immobilization relationships (Stevenson, 1986;Tabatabai, 1987).…”