Importance of sulphur in crop production

Sulphur in agricultural soils occurs in organic and inorganic forms, with organic S accounting for > 95% of the total S. Analysis of a wide range of soils shows that from 25 to 75% of the organic S in soils is HI-reducible, from 7 to 30% is C-bonded, and from 11 to 22% is unidentified S. Nitrogen is associated with S in soil organic matter in a ratio of about 8 : 1, although the extreme ratios may vary from 5: 1 to 13: 1. Laboratory studies showed that humus S is depleted faster than humus N. Mineralization of S in crop residues varied with type of crop residue and soil studied The amounts of S fertilizers (gypsum, elemental S, and sulfuric acid) used in the United States in 1981 and 1982 were 1.9 × 106 and 1.5 × 106 tons, respectively. Of the total amount used in 1982, 3, 5, 20, and 71% were used in the West North Central, Mountain, South Atlantic, and Pacific regions, respecitively. A survey of S deposition at about 100 sites in the United States and many other sites in Canada in 1980 showed that annual addition by precipitation in North America ranged from 0.5 to slightly above 10 kg/ha. The usual ranges of values in concentrations and spatial rates of N, P, and S in precipitation is well within the ranges of these elements in natural waters. Atmospheric sources are important components in meeting crops S requirements and should be considered in benefit-cost analyses relating to S emissions.