Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/25009
Full metadata record
DC FieldValueLanguage
dc.contributor.authorMukherjee, Irani-
dc.contributor.authorKumar, Aman-
dc.contributor.authorDas, T K-
dc.date.accessioned2013-12-24T11:16:03Z-
dc.date.available2013-12-24T11:16:03Z-
dc.date.issued2013-06-
dc.identifier.issn0975-2412 (Online); 0771-7706 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25009-
dc.description52-54en_US
dc.description.abstractPersistence of tribenuron in different soil types (namely alluvial, black and red soil) having different pH values maintained at field capacity moisture regime and in water at three different pH levels i.e. 4, 7 and 9.2, respectively was studied under laboratory conditions at two levels of application, 1.0 and 2.0 mg–1. Samples were processed periodically and analyzed by HPLC. Tribenuron dissipated to 91.04-90. 41% in alluvial and black soil, whereas in red soil with pH 6.64, it dissipated to 94.7% by day 5 after fortification. The half-life values calculated from the first order dissipation kinetics varied from 1.67 in red soil with pH 6.1 to 3.47 in alluvial soil with pH 8.1, indicating that tribenuron is more persistent in soil with basic pH and degrades faster in acidic soil. Slowest dissipation was recorded at neutral and basic pH.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceBVAAP Vol.21(1) [June 2013]en_US
dc.titleFate of tribenuron-methyl in soil and wateren_US
dc.typeArticleen_US
Appears in Collections:BVAAP Vol.21(1) [June 2013]

Files in This Item:
File Description SizeFormat 
BVAAP 21(1) 52-54.pdf62.04 kBAdobe PDFView/Open


Items in NOPR are protected by copyright, with all rights reserved, unless otherwise indicated.