Soil profile development of the Korudağı toposequence, northwest Turkey

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dc.authorid-en_US
dc.authorid-en_US
dc.authorid0000-0002-3670-2114en_US
dc.authorid0000-0002-2943-9207en_US
dc.authorscopusid57196789809en_US
dc.authorscopusid58790456100en_US
dc.authorscopusid57201772026en_US
dc.authorscopusid25224170800en_US
dc.authorwosid-en_US
dc.authorwosid-en_US
dc.authorwosidABF-4048-2021en_US
dc.authorwosidAAG-4899-2019en_US
dc.contributor.authorÖzcan, Hasan
dc.contributor.authorÖzger, İ.
dc.contributor.authorEverest, Timuçin
dc.contributor.authorSungur, Ali
dc.date.accessioned2024-02-21T05:53:37Z
dc.date.available2024-02-21T05:53:37Z
dc.date.issued2024en_US
dc.departmentFakülteler, Ziraat Fakültesi, Toprak Bilimi ve Bitki Besleme Bölümü
dc.departmentMeslek Yüksekokulları, Lapseki Meslek Yüksekokulu, Park ve Bahçe Bitkileri Bölümü
dc.description.abstractThe main objective of this study was to determine the relation between soil profile development and landscape. For this purpose, a field survey was carried out on the same topography and climate to determine the soil profile development degree on different parent materials in the Korudağ Catena (Çanakkale, northwest Turkey). Seven soil profiles were excavated (each 50 m elevation between 350 and 50 m) and described based on soil taxonomy. Profile development index values of soils were calculated to compare and quantify soil horizon properties with their parent materials. The data were collected through field study and physicochemical analyses. Nine characteristics including rubification, color paling, color lightening, melanization, carbonate morphology, moist consistence, dry consistence, pH, texture and structure, were evaluated to calculate the profile development index. This index was calculated as P7 > P1 > P2 > P3 > P5 > P6 > P4, respectively. The P7 profile on the footslope position has the highest profile development due to higher moisture content and the chemical weathering process. The lowest profile development was observed in P4. This profile's topographic position (shoulder) and vegetative density are the major reason. The effect of steepness, curvature, and vegetation on controlling profile development was obvious at the P4 on the shoulder position. In the Korudağ Catena, vegetative density, slope and slope length, elevation difference, and moisture content control the pedogenic process and profile development. This study also showed the profile development changing in a catena with the same aspect, where morphological changes occur on similar parent materials at similar ages but at short distances due to erosion storage processes.en_US
dc.identifier.citationÖzcan, H., Özger, İ., Everest, T., & Sungur, A. (2024). Soil profile development of the Korudağı toposequence, northwest Turkey. International Journal of Environmental Science and Technology, 1–14. doi: 10.1007/s13762-023-05403-9en_US
dc.identifier.doi10.1007/s13762-023-05403-9
dc.identifier.isbn1735-1472 / 1735-2630
dc.identifier.scopus2-s2.0-85181189718
dc.identifier.urihttps://doi.org/10.1007/s13762-023-05403-9
dc.identifier.urihttps://hdl.handle.net/20.500.12428/5696
dc.identifier.wosWOS:001132853700005
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorÖzcan, Hasan
dc.institutionauthorÖzger, İ.
dc.institutionauthorEverest, Timuçin
dc.institutionauthorSungur, Ali
dc.language.isoen
dc.publisherInstitute for Ionicsen_US
dc.relation.ispartofInternational Journal of Environmental Science and Technologyen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectLandscape morphologyen_US
dc.subjectPedogenesisen_US
dc.subjectProfile development indexen_US
dc.subjectSoil evolutionen_US
dc.titleSoil profile development of the Korudağı toposequence, northwest Turkey
dc.typeArticle

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