Publication:
Evaluation of the Soil Carbon Sequestration Potential and Toward Digital Soil Mapping Under Semi-Arid Mediterranean Ecological Condition

dc.authorscopusid56297811900
dc.authorscopusid16052385200
dc.authorwosidDengiz, Orhan/Abg-7284-2020
dc.authorwosidAlaboz, Pelin/Abf-5309-2020
dc.contributor.authorAlaboz, Pelin
dc.contributor.authorDengiz, Orhan
dc.contributor.authorIDAlaboz, Pelin/0000-0001-7345-938X
dc.date.accessioned2025-12-11T00:51:26Z
dc.date.issued2024
dc.departmentOndokuz Mayıs Üniversitesien_US
dc.department-temp[Alaboz, Pelin] Isparta Univ Appl Sci, Fac Agr, Dept Soil Sci & Plant Nutr, Isparta, Turkiye; [Dengiz, Orhan] Ondokuz Mayis Univ, Agr Fac, Plant Nutr & Soil Sci Dept, Samsun, Turkiyeen_US
dc.descriptionAlaboz, Pelin/0000-0001-7345-938Xen_US
dc.description.abstractIn this study, it was aimed to evaluate the relationship between the carbon sequestration potential (CSP) of soils and some soil physical properties. In addition, the predictability of CSP with the support vector regression (SVR) algorithm and the most successful interpolation method in distribution maps of observed and predicted values were determined. The CSP of the soils in the study area was determined to be 43.53 t C ha-1 and 78.09 t C ha-1. Negative correlations were found between CSP and macroporosity, sand, and bulk density, and positive statistically significant correlations were found with organic carbon, available water content, permanent wilting point and microporosity. The CSP was predicted by the SVR algorithm. The root mean square error (RMSE), Lin's concordance correlation coefficient (LCCC), and ratio of performance to deviation (RPD) were determined to be 7.67, 0.18, and 0.93, respectively. The predicted interval (PI) was determined to be 47.60 t C ha-1 and 67.03 t Cha-1. In general, it was found that the error rates increased with a higher than 60% sand and 35% clay content. The simple kriging method with the lowest error rate was determined for the spatial distribution of the CSP. The distribution patterns of the predicted map and the actual value map were not found to be similar. It has been evaluated that it is crucial in the follow-up of sensitive areas, especially with the creation of digital maps created with forecasting models.en_US
dc.description.woscitationindexEmerging Sources Citation Index
dc.identifier.doi10.1007/s41207-024-00512-4
dc.identifier.endpage1007en_US
dc.identifier.issn2365-6433
dc.identifier.issn2365-7448
dc.identifier.issue2en_US
dc.identifier.scopus2-s2.0-85191243925
dc.identifier.scopusqualityQ2
dc.identifier.startpage997en_US
dc.identifier.urihttps://doi.org/10.1007/s41207-024-00512-4
dc.identifier.urihttps://hdl.handle.net/20.500.12712/39730
dc.identifier.volume9en_US
dc.identifier.wosWOS:001207681200001
dc.language.isoenen_US
dc.publisherSpringer Heidelbergen_US
dc.relation.ispartofEuro-Mediterranean Journal for Environmental Integrationen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectMachine Learningen_US
dc.subjectCarbon Stocken_US
dc.subjectSoil Structureen_US
dc.subjectPrincipal Component Analysisen_US
dc.titleEvaluation of the Soil Carbon Sequestration Potential and Toward Digital Soil Mapping Under Semi-Arid Mediterranean Ecological Conditionen_US
dc.typeArticleen_US
dspace.entity.typePublication

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