Please use this identifier to cite or link to this item: http://earsiv.odu.edu.tr:8080/xmlui/handle/11489/5108
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dc.contributor.authorIbrikci, H.-
dc.contributor.authorCetin, M.-
dc.contributor.authorKarnez, E.-
dc.contributor.authorKirda, C.-
dc.contributor.authorTopcu, S.-
dc.contributor.authorRyan, J.-
dc.contributor.authorOztekin, E.-
dc.contributor.authorDingil, M.-
dc.contributor.authorKorkmaz, K.-
dc.contributor.authorOguz, H.-
dc.date.accessioned2024-03-26T06:36:22Z-
dc.date.available2024-03-26T06:36:22Z-
dc.date.issued2012-
dc.identifier.citationIbrikci, H., Cetin, M., Karnez, E., Kirda, C., Topcu, S., Ryan, J., Oztekin, E., Dingil, M., Korkmaz, K., Oguz, H. (2012). Spatial and Temporal Variability of Groundwater Nitrate Concentrations in Irrigated Mediterranean Agriculture. Commun. Soil Sci. Plant Anal., 43(1-2), 47-59. https://doi.org/10.1080/00103624.2012.631413en_US
dc.identifier.issn0010-3624-
dc.identifier.issn1532-2416-
dc.identifier.urihttp://dx.doi.org/10.1080/00103624.2012.631413-
dc.identifier.urihttps://www.webofscience.com/wos/woscc/full-record/WOS:000301639200005-
dc.identifier.urihttp://earsiv.odu.edu.tr:8080/xmlui/handle/11489/5108-
dc.descriptionWoS Categories: Agronomy; Plant Sciences; Chemistry, Analytical; Soil Scienceen_US
dc.descriptionWeb of Science Index: Science Citation Index Expanded (SCI-EXPANDED)en_US
dc.descriptionResearch Areas: Agriculture; Plant Sciences; Chemistryen_US
dc.description.abstractAs nitrogen (N) fertilizer-use efficiency rarely exceeds 50% in most agricultural systems, the potential leaching of N to the groundwater, particularly under irrigated conditions, has economic, health, and environmental implications. Research in the Akarsu irrigation district in the Lower Seyhan Plain in southern Turkey sought to determine spatial and temporal variability of groundwater (GW) nitrate (NO3) concentrations in 2007-2008. Shallow groundwater observation wells 3 m deep were installed at different locations to represent the whole irrigation district. Groundwater samples were collected (February, April, July, October) and analyzed for ammonium (NH4) and NO3 concentrations. Because NH4 values were negligible, only NO3 data were processed to determine spatial and temporal variability and then used to develop regional NO3 maps using geographic information systems. Groundwater NO3 concentrations ranged between 0.17 and 55.96 mg L-1 during the 2 years, only exceeding the critical 50 mg L-1 concentration in 1% of the area sampled. The areal mean of NO3 concentration was greatest in February, indicating a potential N leaching of unused N from the early season with intensive rainfall, especially in wheat-growing areas. Groundwater NO3 concentrations decreased after February; however, during the peak irrigation season in July, NO3 was relatively low because of crop uptake during spring and summer. In about half the area, groundwater NO3 concentrations ranged between 20 and 50 mg L-1 and were thus marginal relative to the critical pollution level. As N fertilizer use will continue to increase, especially with the expanded irrigation that is now occurring in the Mediterranean region, regular monitoring of groundwater NO3 is advisable under such conditions.en_US
dc.description.sponsorshipEuropean Union [INCO-CT-2005-015031]; Cukurova University Academic Research Projects Unit [ZF2006KAP1, ZF2008BAP8]en_US
dc.language.isoengen_US
dc.publisherTAYLOR & FRANCIS INC-PHILADELPHIAen_US
dc.relation.isversionof10.1080/00103624.2012.631413en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectDrainage observation wells, groundwater nitrate, irrigation schemes, Mediterranean region, potential nitrate pollutionen_US
dc.subjectNITROGEN DYNAMICS, CROPPING SYSTEM, CONTAMINATION, SOIL, BALANCE, WATERen_US
dc.titleSpatial and Temporal Variability of Groundwater Nitrate Concentrations in Irrigated Mediterranean Agricultureen_US
dc.typearticleen_US
dc.relation.journalCOMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSISen_US
dc.contributor.departmentOrdu Üniversitesien_US
dc.contributor.authorID0000-0001-5751-0958en_US
dc.identifier.volume43en_US
dc.identifier.issue1-2en_US
dc.identifier.startpage47en_US
dc.identifier.endpage59en_US
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