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dc.contributor.authorB.R Nasibov
dc.contributor.authorB.D. Abdullaev
dc.contributor.authorR.I.Razzakov
dc.contributor.authorA.B Ruzimurodov
dc.date.accessioned2025-10-21T12:14:42Z
dc.date.available2025-10-21T12:14:42Z
dc.date.issued2025
dc.identifier.urihttps://dspace.kstu.uz/xmlui/handle/123456789/740
dc.descriptionThis study provides evidence for groundwater-surface water interaction in the Kashkadarya River Basin. While discharge decreases downstream due to anthropogenic uses, EC increases significantly, especially during low-flow periods, suggesting the influence of saline groundwater and irrigation return flows. Temperature generally increases downstream due to the arid climate and shallow water depths.en_US
dc.description.abstractUnderstanding the interplay between groundwater and surface water systems is crucial for effective water resource management and the preservation of aquatic ecosystems. River water chemistry and temperature are profoundly influenced by groundwater discharge, particularly in arid and semi-arid regions like the Kashkadarya River Basin [1-3]. Groundwater typically provides a relatively stable source of water that can buffer against extreme temperature fluctuations and dilute the effects of surface runoff. This study aims to investigate the spatial and temporal dynamics of groundwater-surface water interactions within the Kashkadarya River Basin, focusing on their impact on river water chemistry and temperature [4-7]. We hypothesize that groundwater input will be characterized by relatively stable temperature and higher concentrations of dissolved solids compared to surface water, resulting in observable changes in these parameters along the river course, particularly downstream in the Karshi Steppe region.en_US
dc.description.sponsorshipUnderstanding the interplay between groundwater and surface water systems is crucial for effective water resource management and the preservation of aquatic ecosystems. River water chemistry and temperature are profoundly influenced by groundwater discharge, particularly in arid and semi-arid regions like the Kashkadarya River Basin [1-3]. Groundwater typically provides a relatively stable source of water that can buffer against extreme temperature fluctuations and dilute the effects of surface runoff. This study aims to investigate the spatial and temporal dynamics of groundwater-surface water interactions within the Kashkadarya River Basin, focusing on their impact on river water chemistry and temperature [4-7]. We hypothesize that groundwater input will be characterized by relatively stable temperature and higher concentrations of dissolved solids compared to surface water, resulting in observable changes in these parameters along the river course, particularly downstream in the Karshi Steppe region.en_US
dc.language.isoenen_US
dc.publisher"Экономика и социум" №5(132) 2025en_US
dc.subjectGroundwater-Surface Water Interaction, Streamflow, River Water Chemistry, Temperature Gradients, Baseflow, Stable Isotopes, Kashkadarya River Basin, Karshi Steppeen_US
dc.titleTHE RELATIONSHIP BETWEEN THE CHARACTERISTICS OF GROUNDWATER AND SURFACE WATER IN THE KASHKADARYA REGIONen_US
dc.title.alternativeЭкономика и социумen_US
dc.typeArticleen_US


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