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Role of Fe-oxides for predicting phosphorus sorption in calcareous soils

dc.contributor.authorMemon, Mehruinsa*
dc.date.accessioned2021-02-12T02:27:27Z
dc.date.available2021-02-12T02:27:27Z
dc.date.issued2008*
dc.date.submitted2019-07-30 20:01:59*
dc.identifier34761*
dc.identifier.issn16182677*
dc.identifier.urihttps://directory.doabooks.org/handle/20.500.12854/58579
dc.description.abstractAgronomic efficiency and management of environmental P inputs can be improved by understanding soil-phosphorus interaction. Iron oxides and other clay minerals, P forms, and P sorption in young alluvial and weathered residual soils were determined. Phosphorus retention related to crystallinity and phase distribution of iron oxides. CBD and oxalate extractable iron and aluminum and smectite and kaolinite explained 90% variation while soil CaCO3 role was only insignificant in explaining P sorption.*
dc.languageEnglish*
dc.relation.ispartofseriesKarlsruher mineralogische und geochemische Hefte : Schriftenreihe des Instituts für Mineralogie und Geochemie*
dc.subjectQC1-999*
dc.subject.classificationthema EDItEUR::P Mathematics and Science::PH Physicsen_US
dc.subject.othergoethite*
dc.subject.otherP-fractionation*
dc.subject.otherhematite*
dc.subject.otherFe-oxides*
dc.subject.otherphosphorus sorption*
dc.subject.othercalcareous soils*
dc.titleRole of Fe-oxides for predicting phosphorus sorption in calcareous soils*
dc.typebook
oapen.identifier.doi10.5445/KSP/1000008093*
oapen.relation.isPublishedBy68fffc18-8f7b-44fa-ac7e-0b7d7d979bd2*
oapen.relation.isbn9783866442412*
oapen.pagesXIII, 144 p.*
oapen.volume34*
peerreview.review.typeFull text
peerreview.anonymityAll identities known
peerreview.reviewer.typeEditorial board member
peerreview.reviewer.typeExternal peer reviewer
peerreview.review.stagePre-publication
peerreview.open.reviewNo
peerreview.publish.responsibilityBooks or series editor
peerreview.id51a542ec-eaeb-47c2-861d-6022e981a97a
peerreview.titleDissertations in Series (Dissertationen in Schriftenreihe)


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