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dc.contributor.authorJuo, A.S.R.
dc.contributor.authorOginni, O.O.
dc.date.accessioned2019-12-04T11:08:27Z
dc.date.available2019-12-04T11:08:27Z
dc.date.issued1978
dc.identifier.citationJuo, A.S.R. & Oginni, O. O. (1978). Adsorption and desorption of paraquat in acid tropical soils. Journal of Environmental Quality, 7(1), 9-12.
dc.identifier.issn0047-2425
dc.identifier.urihttps://hdl.handle.net/20.500.12478/1831
dc.description.abstractAdsorption of paraquat (1:1′-dimethyl 4:4′-bipyridylium chloride) by six common soil types from southern Nigeria was studied. Adsorption data conformed with linear Langmuir isotherm. Adsorption maximum (b) calculated from the Langmuir equation ranged from 1,200 to 7,500 µg/g of soil. The iron oxide-rich soil derived from basalts adsorbed the highest amount, while the strongly acidic soils derived from sedimentary rocks adsorbed the least amount of paraquat. Desorption data indicated that a substantial portion (40 to 70%) of the adsorbed paraquat could not be recovered by 12 successive extractions with dilute CaCl2 solution.
dc.format.extent9-12
dc.language.isoen
dc.subjectVltisols
dc.subjectAlfisols
dc.subjectLangmuir Adsorption Maximum
dc.subjectDesorption
dc.subjectSoil
dc.titleAdsorption and desorption of paraquat in acid tropical soils
dc.typeJournal Article
dc.description.versionPeer Review
cg.contributor.affiliationInternational Institute of Tropical Agriculture
cg.coverage.regionAfrica
cg.coverage.regionWest Africa
cg.coverage.countryNigeria
cg.isijournalISI Journal
cg.authorship.typesCGIAR single centre
cg.iitasubjectSoil Fertility
cg.iitasubjectSoil Information
cg.iitasubjectSoil Surveys And Mapping
cg.journalJournal of Environmental Quality
cg.howpublishedFormally Published
cg.accessibilitystatusLimited Access
local.dspaceid83295
cg.targetaudienceScientists
cg.identifier.doihttps://dx.doi.org/10.2134/jeq1978.00472425000700010002x


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