Abstract
The capacity of soils to oxidize S was measured by incubation with finely divided elemental S in 13 calcareous orchard soils from the southern interior of British Columbia. Sulphur oxidation rates ranged from 3.4 to 26 μg S cm-2 d-1. The magnitude of pH decrease in response to added S varied inversely with initial CaCO3 content and silt content and directly with sand content. Incubation studies with one calcareous orchard soil indicated that finely divided S was more effective over time than other acidulants (FeSO4, Al2(SO4)3 and H2SO4). In a field study on the same soil, incorporated fine S was oxidized to a much greater extent during a 2-year period than was incorporated bentonitic grandulated S. However, when surface applied, they were oxidized equally but slowly. -Authors
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CITATION STYLE
Neilsen, D., Hogue, E. J., Hoyt, P. B., & Drought, B. G. (1993). Oxidation of elemental sulphur and acidulation of calcareous orchard soils in southern British Columbia. Canadian Journal of Soil Science, 73(1), 103–114. https://doi.org/10.4141/cjss93-010
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