Impact of land cover types on soil aggregate stability and erodibility

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dc.authoridilay, Remzi/0000-0002-3558-3125
dc.contributor.authorIlay, Remzi
dc.contributor.authorKavdir, Yasemin
dc.date.accessioned2025-01-27T21:01:44Z
dc.date.available2025-01-27T21:01:44Z
dc.date.issued2018
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractGok double dagger eada is the biggest island, and it is also known as the organic island of Turkey. Approximately 65% of the Gok double dagger eada lands have slope > 12%. Climate, topography, land cover, and soil characteristics are considered to be the main natural factors affecting soil erosion severity in the Gok double dagger eada. Prevention of soil degradation, hence the preservation or improvement of the overall quality of the soil, is directly related to the presence of stable soil aggregates. In addition, the resistance to weathering and replacement of soil particles are also relevant aspects in terms of sustainability. Aggregate stability (AS) and erodibility of land (Kfac) are related to soil properties. However, this relationship can vary under different circumstances. In this study, 248 surface soil samples have been taken from forest and semi-natural areas (FSNA) and agricultural areas (AGRA) according to CORINE 2006. Eleven selected soil properties were measured, and their impacts on AS and Kfac (RUSLE-K) were determined by using the CRT (classification and regression tree) in Gok double dagger eada. Results showed that the relations among soil characteristics changed according to the land cover classes. Total organic carbon is much more associated with AS in AGRA, while total carbon is associated with AS in FSNA. The effect of calcium carbonate on Kfac was higher than other soil properties when the land cover type was ignored. On the other hand, in AGRA, the effect of between clay content on Kfac was greater than those of FSNA.
dc.description.sponsorshipCOMU-BAP Project [2012/17]
dc.description.sponsorshipThis study was supported by the COMU-BAP Project 2012/17.
dc.identifier.doi10.1007/s10661-018-6847-4
dc.identifier.issn0167-6369
dc.identifier.issn1573-2959
dc.identifier.issue9
dc.identifier.pmid30117012
dc.identifier.scopus2-s2.0-85051709067
dc.identifier.scopusqualityQ2
dc.identifier.urihttps://doi.org/10.1007/s10661-018-6847-4
dc.identifier.urihttps://hdl.handle.net/20.500.12428/27172
dc.identifier.volume190
dc.identifier.wosWOS:000442034000001
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakPubMed
dc.language.isoen
dc.publisherSpringer
dc.relation.ispartofEnvironmental Monitoring and Assessment
dc.relation.publicationcategoryinfo:eu-repo/semantics/openAccess
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectGokceada
dc.subjectLand cover class
dc.subjectSoil erodibility
dc.subjectAggregate stability
dc.subjectKfac (RUSLE-K)
dc.titleImpact of land cover types on soil aggregate stability and erodibility
dc.typeArticle

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