Abstract

Abstract The release of carbonyl sulfide (COS) from 7 unamended paddy soils was estimated under aerobic and waterlogged conditions. The addition of organic materials to the soils increased the amount of COS evolved under waterlogged conditions. To assess the sources of the COS released from the soils, the soils were incubated under aerobic and waterlogged conditions after treatment with 17 inorganic or organic S-containing compounds. It was concluded that the following compounds represented sources of the COS released from the paddy soils: cystine, cysteine, thiocyanate, lanthionine and djenkolic acid.

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