Publication:
Determination of Soil Thermal Properties Across Seasons in Alkaline–Nonalkaline Soils of Igdır, Türkiye

dc.authorscopusid58923153400
dc.authorscopusid57201773581
dc.authorscopusid7101841888
dc.authorscopusid56027542500
dc.authorscopusid12795801900
dc.contributor.authorMikail, R.
dc.contributor.authorErdel, E.
dc.contributor.authorMamedov, A.I.
dc.contributor.authorHazar, E.
dc.contributor.authorMikailsoy, F.
dc.date.accessioned2025-12-11T00:35:40Z
dc.date.issued2025
dc.departmentOndokuz Mayıs Üniversitesien_US
dc.department-temp[Mikail] R., Department of Mathematics, Iğdır Üniversitesi, Igdir, Turkey; [Erdel] Erhan, Department of Soil Science and Plant Nutrition, Iğdır Üniversitesi, Igdir, Turkey; [Mamedov] A. I., Arid Land Research Center, Tottori University, Tottori, Tottori, Japan, Department of Soil Science and Plant Nutrition, Ondokuz Mayis Üniversitesi, Samsun, Turkey, Department of Ecology and Environment, Western Caspian University Baku, Baku, Azerbaijan; [Hazar] Elman, Department of Mathematics, Iğdır Üniversitesi, Igdir, Turkey; [Mikailsoy] Fariz D., Department of Soil Science and Plant Nutrition, Iğdır Üniversitesi, Igdir, Turkeyen_US
dc.description.abstractClimate, which has important effects on pedogenesis, affects soils and its structure and mass transport through temperature and precipitation. Soil salinity or alkalinity, which is caused by the effects of climate, parent material, topography, and anthropogenic factors, is one of the important problems of arid and semi-arid regions and has negative effects on soil quality, requiring specific attention due to limited research. In this study, thermal properties were calculated using various classical and improved models in winter, spring, summer, and fall for alkaline and non-alkaline soil. For this purpose, temperature sensors were placed at depths of 0, 0.05, 0.10, 0.15, 0.20, and 0.40 m in non-alkaline and alkaline lands, and temperature data were collected from the sensors for 365 days. This study showed that (i) the thermal properties of both soils vary depending on the seasons of the year, and (ii) the thermal properties (thermal conductivity, thermal conductivity coefficient, thermal conductivity, attenuation depth, thermal conductivity coefficient, speed and length of the heat wave) were lower in the alkaline soil. These results could be used for consideration of climate change mitigation in similar semi-arid zones. © 2025 by the authors.en_US
dc.identifier.doi10.3390/land14112266
dc.identifier.issue11en_US
dc.identifier.scopus2-s2.0-105022934688
dc.identifier.urihttps://doi.org/10.3390/land14112266
dc.identifier.urihttps://hdl.handle.net/20.500.12712/37699
dc.identifier.volume14en_US
dc.language.isoenen_US
dc.publisherMultidisciplinary Digital Publishing Institute (MDPI)en_US
dc.relation.ispartofLanden_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectAlkalinityen_US
dc.subjectImproved Methoden_US
dc.subjectModelingen_US
dc.subjectSeasonsen_US
dc.subjectSoilen_US
dc.subjectThermal Conductivityen_US
dc.subjectThermal Diffusivityen_US
dc.titleDetermination of Soil Thermal Properties Across Seasons in Alkaline–Nonalkaline Soils of Igdır, Türkiyeen_US
dc.typeArticleen_US
dspace.entity.typePublication

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