Transformations of applied magnesium in soil

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dc.contributor.authorPrema, L
dc.contributor.authorJose, A I
dc.contributor.authorKAU
dc.date.accessioned2019-01-17T07:19:00Z
dc.date.available2019-01-17T07:19:00Z
dc.date.issued1995
dc.description.abstractAil incubation study was taken up with two acid soils (laterite and Kuttanad alluvium), three sources of Mg (MgSO4.7H2O, magnesite and dolomite) and three levels of Mg (1250, 2500 and 3750 MgO kg ha'1) at field capacity. The rate of release of Mg from different sources was in the order of their solubility i.e., MgSO4.7H2O > magnesite > dolomite. The retention of available Mg was more in treatments with magnesite. The Mg fractions and pH were found to increase with increased levels of application MgO. Magnesite was superior to other sources in supplying available Mg and exchangeable Mg in both the soils.en_US
dc.identifier.citationJournal of Tropical Agriculture, 33(1), 27-31.en_US
dc.identifier.urihttp://krishikosh.egranth.ac.in/handle/1/5810091048
dc.keywordsAcid soils, available Mg, exchangeable Mg, magnesium dynamics, magnesium fertilizers.en_US
dc.language.isoenen_US
dc.pages5en_US
dc.publisherKerala Agricultural Universityen_US
dc.subjectnullen_US
dc.titleTransformations of applied magnesium in soilen_US
dc.typeArticleen_US
dc.volume33(1)en_US
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