Publication:
Capability of Different Interpolation Models and Pedotransfer Functions to Estimate Soil Hydraulic Properties in Büyükçay Watershed

dc.authorscopusid55614991200
dc.authorscopusid6603263487
dc.authorscopusid16052385200
dc.contributor.authorMiháliková, M.
dc.contributor.authorBaşkan, O.
dc.contributor.authorDengiz, O.
dc.date.accessioned2020-06-21T13:45:51Z
dc.date.available2020-06-21T13:45:51Z
dc.date.issued2015
dc.departmentOndokuz Mayıs Üniversitesien_US
dc.department-temp[Miháliková] Markéta, Department of Water Resources, Czech University of Life Sciences Prague, Prague, Czech Republic; [Başkan] Oǧuz, Soil Fertilizer and Water Resources Central Research Institute, Yenimahalle, Ankara, Turkey; [Dengiz] Orhan, Department of Soil Science and Plant Nutrition, Ondokuz Mayis Üniversitesi, Samsun, Turkeyen_US
dc.description.abstractMany catchment basins have insufficient data to make conservation planning for sustainable natural resources use. In addition, intensive soil sampling is neither feasible nor economical in a large studied area. Therefore, interpolation models and pedotransfer functions (PTFs) have important roles in data mining. Main objectives of this study were to estimate and evaluate the estimates of basic soil hydraulic properties in Büyükçay Watershed (Turkey) using different interpolation geostatistic models and PTFs. Three interpolation models (inverse distance weighting IDW, ordinary kriging and cokriging) and pedotransfer functions (continuous and class) were applied and compared in this study. In 84 soil samples, soil depth, texture, organic matter, pH, electric conductivity, saturation degree, field capacity and permanent wilting point were determined. According to the results, among geostatistical algorithms, ordinary cokriging yields better results for all soil hydraulic properties with lower MAE and MSE values than ordinary kriging and IDW. Within PTFs, soil hydraulic properties were estimated with high reliability using continuous approach; however, class PTFs showed less sensitivity to space variability than geostatistical methods. © 2015, Springer-Verlag Berlin Heidelberg.en_US
dc.identifier.doi10.1007/s12665-015-4246-5
dc.identifier.endpage2437en_US
dc.identifier.isbn9783540959908
dc.identifier.issn1866-6280
dc.identifier.issn1866-6299
dc.identifier.issue3en_US
dc.identifier.scopus2-s2.0-84937526906
dc.identifier.scopusqualityQ2
dc.identifier.startpage2425en_US
dc.identifier.urihttps://doi.org/10.1007/s12665-015-4246-5
dc.identifier.volume74en_US
dc.identifier.wosWOS:000358073800047
dc.identifier.wosqualityQ2
dc.language.isoenen_US
dc.publisherSpringer Verlag service@springer.deen_US
dc.relation.ispartofEnvironmental Earth Sciencesen_US
dc.relation.journalEnvironmental Earth Sciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectBüyükçay Watersheden_US
dc.subjectGeostatisticsen_US
dc.subjectPedotransfer Functionsen_US
dc.subjectSoil Mapen_US
dc.titleCapability of Different Interpolation Models and Pedotransfer Functions to Estimate Soil Hydraulic Properties in Büyükçay Watersheden_US
dc.typeArticleen_US
dspace.entity.typePublication

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