Please use this identifier to cite or link to this item: http://earsiv.odu.edu.tr:8080/xmlui/handle/11489/5270
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dc.contributor.authorDemir, Yusuf-
dc.contributor.authorErsahim, Sabit-
dc.contributor.authorGuler, Mustafa-
dc.contributor.authorCemek, Bilal-
dc.contributor.authorGunal, Hikmet-
dc.contributor.authorArslan, Hakan-
dc.date.accessioned2024-03-26T06:58:16Z-
dc.date.available2024-03-26T06:58:16Z-
dc.date.issued2009-
dc.identifier.citationDemir, Y., Ersahim, S., Güler, M., Cemek, B., Günal, H., Arslan, H. (2009). Spatial variability of depth and salinity of groundwater under irrigated ustifluvents in the Middle Black Sea Region of Turkey. Environ. Monit. Assess., 158(1-4), 279-294. https://doi.org/10.1007/s10661-008-0582-1en_US
dc.identifier.issn0167-6369-
dc.identifier.issn1573-2959-
dc.identifier.urihttp://dx.doi.org/10.1007/s10661-008-0582-1-
dc.identifier.urihttps://www.webofscience.com/wos/woscc/full-record/WOS:000271670200023-
dc.identifier.urihttp://earsiv.odu.edu.tr:8080/xmlui/handle/11489/5270-
dc.descriptionWoS Categories: Environmental Sciencesen_US
dc.descriptionWeb of Science Index: Science Citation Index Expanded (SCI-EXPANDED)en_US
dc.descriptionResearch Areas: Environmental Sciences & Ecologyen_US
dc.description.abstractInformation on the potential risk for soil salinity buildup can be very helpful for soil salinity management in irrigated areas. We evaluated the spatial and temporal variability of groundwater salinity (GWS) and groundwater depth (GWD), which are two of the most important indicators of soil salinity, by indicator kriging technique in a large irrigated area in northern Turkey. GWS and GWD were measured on a monthly basis from irrigation season (August 2003) to rainy season (April 2004) at 60 observation wells in the 8,187-ha irrigated area. Five indicator thresholds were used for GWS and GWD. The semivariogram for each of the thresholds for both variables was analyzed then used together with experimental data to interpolate and map the corresponding conditional cumulative distribution functions (CCDF). Risk for soil salinity buildup was greater in the irrigation season compared to that in the rainy season. The greatest risk for soil salinity buildup occurred in the eastern part of the study area, suffering from poor drainage problem due to malfunctioning drainage infrastructure, as indicated by the CCDF of GWS and GWD obtained in both seasons. It was concluded that a combination of mechanical and cultural measures should be taken in high-risk locations to avoid further salinity problems.en_US
dc.language.isoengen_US
dc.publisherSPRINGER-DORDRECHTen_US
dc.relation.isversionof10.1007/s10661-008-0582-1en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectEvapotranspiration, Groundwater depth, Groundwater salinity, Indicator kriging, Irrigationen_US
dc.subjectSOIL-WATER CONTENT, MAPPING RISK, CONTAMINATIONen_US
dc.titleSpatial variability of depth and salinity of groundwater under irrigated ustifluvents in the Middle Black Sea Region of Turkeyen_US
dc.typearticleen_US
dc.relation.journalENVIRONMENTAL MONITORING AND ASSESSMENTen_US
dc.contributor.departmentOrdu Üniversitesien_US
dc.contributor.authorID0000-0002-9677-6035en_US
dc.contributor.authorID0000-0002-4648-2645en_US
dc.identifier.volume158en_US
dc.identifier.issue1-4en_US
dc.identifier.startpage279en_US
dc.identifier.endpage294en_US
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