Oxidation of thiosulphate (S2O3
2−) and tetrathionate (S4O6
2−), added at 300mgSkg−1 soil, was studied in four arable soils at 25°C, over incubation periods of 0, 3, 7, 10, 20 and 30d. Thiosulphate was oxidised rapidly to S4O6
2−, with most of the oxidation occurring within 3d. In contrast, S4O6
2− was oxidised to SO4
2− much more slowly. Oxidation of S4O6
2− varied with soil type, being slower in a loamy soil (pH 5.8) than in three other soils (clay loam, silty clay loam and loamy sand, pH 6.2–7.0). An incubation experiment using autoclaved Rothamsted soil indicated a large abiotic component in the oxidation of S2O3
2− to S4O6
2−, whereas the oxidation of S4O6
2− to SO4
2− was of a biological nature. Production of SO4
2− was more rapid from the S2O3
2− amendment than from the S4O6
2− amendment, which suggested that either S2O3
2− primed the S4O6
2− oxidisers, or microorganisms were present that could oxidise S2O3
2− to SO4
2−, but not S4O6
2− to SO4
2−.
Xu Fang, Andrea E. Colina Blanco, Iso Christl, Maureen Le Bars, Daniel Straub, Sara Kleindienst, Britta Planer‐Friedrich, Fang-jie Zhao, Andreas Kappler, Ruben Kretzschmar
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