Abstract
The exchange of COS between wheat soil and atmosphere was investigated by using a dynamic enclosure. The investigated soil type acted as a significant sink for the trace gas COS. Atmospheric COS mixing ratios and temperature were found to be the physicochemical parameters controlling the uptake. The uptake reached maximum about 0.6×10−12 mol · g−1 · h−1 at 15–20°C under natural ambient atmospheric conditions. The measured uptake values agree well with that calculated by Guenther algorithm.
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