Sulfur isotope fractionation during the oxidation of elemental sulfur by thiobacilli in a Solonetzic soil.

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Abstract

The oxidation rate of elemental S added to a Solonetzic soil was compared between an uninoculated soil and soils inoculated with two species of thiobacilli. Twelve weeks after S was added, 24% was oxidized to soluble S anions in the uninoculated soil, 34% in soil inoculated with Thiobacillus thiooxidans, and 84% in soil inoculated with Thiobacillus thiparus.-from Authors

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McCready, R. G. L., & Krouse, H. R. (1982). Sulfur isotope fractionation during the oxidation of elemental sulfur by thiobacilli in a Solonetzic soil. Canadian Journal of Soil Science, 62(1), 105–110. https://doi.org/10.4141/cjss82-012

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