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.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
