Publication:
Sequential Micronutrients Extraction from Toposequences of Pasture Soils

dc.authorscopusid7006109214
dc.authorscopusid9038789000
dc.authorscopusid6505470166
dc.authorscopusid23487395700
dc.contributor.authorÖzdemir, Nutullah
dc.contributor.authorKızılkaya, R.
dc.contributor.authorHepşen, S.
dc.contributor.authorYakupoǧlu, T.
dc.date.accessioned2020-06-21T15:19:01Z
dc.date.available2020-06-21T15:19:01Z
dc.date.issued2007
dc.departmentOndokuz Mayıs Üniversitesien_US
dc.department-temp[Özdemir] Nutullah, Department of Soil Sciences, Ondokuz Mayis Üniversitesi, Samsun, Turkey; [KIZILKAYA] RIDVAN BATUHAN, Department of Soil Sciences, Ondokuz Mayis Üniversitesi, Samsun, Turkey; [Hepşen] Şüheda, Department of Soil Sciences, Ondokuz Mayis Üniversitesi, Samsun, Turkey; [Yakupoǧlu] Tugrul, Department of Soil Sciences, Ondokuz Mayis Üniversitesi, Samsun, Turkeyen_US
dc.description.abstractThe objective of this study was to determine changes in soil properties and micronutrient content (Fe, Cu, Mn and Zn) development along a slope in pasture soils. The study area is located in Kocadag, Samsun, Turkey. Three landscape positions i.e., summit, backslope and footslope, were selected. Soil samples for all genetic horizons were taken from all landscape positions of pasture. Some physico-chemical properties such as organic matter content, pH, CaCO <inf>3</inf>, exchangeable cations and sequential micronutrient fractions (exchangeable, organically complexed, manganese oxide bounded, amorphous and crystalline iron oxide bounded and residual) were determined. All micronutrient pools, horizons were affected by slope position. The micronutrient fractions and particularly the exchangeable (EX-), organically complexed (OM-) fractions tended to decline with soil dept. The residual fraction (R-) was proportionally the largest fraction and EX- and OM- fraction were the smallest fractions at all horizon and landscape position. In footslope position, the soils had generally the higher total micronutrient contents and their R- fractions than the other positions at all genetic horizons. In all positions, except for R- fraction, micronutrient fractions in soils decreased from the surface downward indicating that the major part of the location is existed to the A horizon.en_US
dc.identifier.endpage4034en_US
dc.identifier.issn0970-7077
dc.identifier.issue5en_US
dc.identifier.scopus2-s2.0-34347256341
dc.identifier.scopusqualityQ4
dc.identifier.startpage4025en_US
dc.identifier.volume19en_US
dc.identifier.wosWOS:000246955400105
dc.language.isoenen_US
dc.publisherChemical Publishing Co.en_US
dc.relation.ispartofAsian Journal of Chemistryen_US
dc.relation.journalAsian Journal of Chemistryen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectFractionsen_US
dc.subjectLandscape Positionsen_US
dc.subjectMicronutrienten_US
dc.subjectPasture Soilen_US
dc.titleSequential Micronutrients Extraction from Toposequences of Pasture Soilsen_US
dc.typeArticleen_US
dspace.entity.typePublication

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