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dc.contributorAwan, Usmanen_US
dc.contributorGeorge, Biju Alummoottilen_US
dc.contributorLiaqat, Umar Waqasen_US
dc.creatorIbrakhimov, Mirzakhayoten_US
dc.date2018-03-31en_US
dc.date.accessioned2021-06-23T22:31:15Z
dc.date.available2021-06-23T22:31:15Z
dc.identifierhttps://mel.cgiar.org/dspace/limiteden_US
dc.identifier.citationMirzakhayot Ibrakhimov, Usman Awan, Biju Alummoottil George, Umar Waqas Liaqat. (31/3/2018). Understanding surface water-groundwater interactions for managing large irrigation schemes in the multi-country Fergana valley, Central Asia. Agricultural Water Management, 201, pp. 99-106.en_US
dc.identifier.urihttps://hdl.handle.net/20.500.11766/13274
dc.description.abstractTraditionally, surface water supplies are the sole sources to satisfy crop water requirements in large irrigation schemes such as those in the Fergana Valley, Central Asia. Recent studies indicate that 23–30% of these requirements are met from shallow groundwater, but this is not usually quantified. To manage favorable groundwater levels – i.e., without increasing soil salinity and nutrient leaching and reducing crop yields – information on, and quantification of, groundwater recharge and discharge rates at large spatial and temporal scales, as well as understanding their mechanisms of interaction, is indispensable. With the aim to quantify groundwater recharge, discharge and their interaction, a conceptual water balance model at a scale of a Water Consumers’ Association was established on a monthly basis for a 10-year period. Average groundwater recharge was estimated as 780 ± 75.7 mm, representing 62% of surface water supplies. The highest average annual recharge (930 mm) driven by excessive precipitation and water supply was in 2010 and the lowest (667–726 mm) was in years of lower water availability: 2006–2008 and 2012. The net groundwater recharge was 82.4 ± 79 mm, and determined the groundwater level fluctuations. The highest positive net groundwater recharge rate (247 mm) and the shallowest groundwater level (123 cm) also occurred in 2010. The negative net recharge in 2006 (–11 mm), 2008 (–41 mm) and 2012 (–5 mm) indicated deeper groundwater levels during these periods. The groundwater recharge values were excessively high even for this large irrigation scheme. To save limited freshwater resources, groundwater discharge should be reduced, with one option being to reduce excessive drainage outflow.en_US
dc.languageenen_US
dc.publisherElsevier (12 months)en_US
dc.rightsCopyrighted; all rights reserveden_US
dc.sourceAgricultural Water Management;201,(2018) Pagination 99,106en_US
dc.subjectnet groundwater rechargeen_US
dc.subjectcrop water requirementsen_US
dc.titleUnderstanding surface water-groundwater interactions for managing large irrigation schemes in the multi-country Fergana valley, Central Asiaen_US
dc.typeJournal Articleen_US
cg.creator.idAwan, Usman: 0000-0001-8663-5688en_US
cg.creator.idGeorge, Biju Alummoottil: 0000-0002-8427-3350en_US
cg.creator.ID-typeORCIDen_US
cg.creator.ID-typeORCIDen_US
cg.subject.agrovocwater balanceen_US
cg.subject.agrovocgroundwater rechargeen_US
cg.contributor.centerKhorezm Rural Advisory Support Service - KRASSen_US
cg.contributor.centerInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.contributor.centerSungkyunkwan Universityen_US
cg.contributor.funderInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.contributor.projectCommunication and Documentation Information Services (CODIS)en_US
cg.contributor.project-lead-instituteInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.date.embargo-end-dateTimelessen_US
cg.coverage.regionGlobalen_US
cg.contactu.k.awan@cgiar.orgen_US
cg.identifier.doihttps://dx.doi.org/10.1016/j.agwat.2018.01.016en_US
dc.identifier.statusTimeless limited accessen_US
mel.impact-factor4.021en_US


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