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<p>Riparian groundwater plays a critical role in sustaining river baseflow, supporting ecosystems and ensuring water availability in the hydrologically dynamic regions of the Himalaya. However, hydrological studies in many transboundary catchments like Kishanganga River Basin (KRB) remain unexplored due to the security and logistic reasons. In this study, 225 water samples (70 riparian groundwater and 155 streamwater) collected for major ions, trace metals, and stable isotopes (δ¹⁸O, δ²H) were analyzed to evaluate major geochemical processes controlling solute sources, hydrochemical evolution and hydrological connectivity. The results suggested that the groundwater chemistry is primarily controlled by water-rock interaction with Ca-Mg-HCO₃ type water facies revealing carbonate weathering as a dominant process. Geochemical modeling suggested that groundwater is undersaturated with respect to calcite, dolomite, gypsum and fluorite that facilitates mineral dissolution, while saturation with Fe(III) oxides suggests localized precipitation of ferrous minerals. The regression line of streamwater (δ²H = 6.8 × δ¹⁸O + 18, R² = 0.97) and groundwater (δ²H = 7.2 × δ¹⁸O + 22, R² = 0.97) revealed minor variation in slope, attributed to subtle differences in fractionation processes influenced by local environmental factors that promote evaporation of streamwater. The isotopic similarity between streamwater and riparian groundwater underscores a high degree of hydraulic connectivity. Contaminant assessment highlights arsenic (As) and fluoride (F⁻) as main geogenic pollutants in a few wells and springs, with potential health risks for local populations, particularly infants and children. The Water Quality Index (WQI) and irrigation suitability indices suggest that groundwater is fit for drinking and agricultural use, except at few locations with elevated As and F⁻ concentration. Self-organizing maps (SOM) and Pearson correlation analyses further illustrate the spatial variability of hydrochemical parameters and contamination hotspots. The findings emphasize the need for sustainable groundwater management strategies to mitigate contamination risks and ensure long-term water security in the KRB.</p>

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Hydrological connectivity between riparian groundwater and streamwater system in Kishanganga River Basin (KRB): insights from solutes and stable water isotopes

  • 期刊论文

  • 出版模式：

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  • 发表日期：

    2026年4月3日

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  • Gh Jeelani,
  • G. N. Pintoo,
  • Suhail A. Lone,
  • Abhijit Mukherjee

摘要

Riparian groundwater plays a critical role in sustaining river baseflow, supporting ecosystems and ensuring water availability in the hydrologically dynamic regions of the Himalaya. However, hydrological studies in many transboundary catchments like Kishanganga River Basin (KRB) remain unexplored due to the security and logistic reasons. In this study, 225 water samples (70 riparian groundwater and 155 streamwater) collected for major ions, trace metals, and stable isotopes (δ¹⁸O, δ²H) were analyzed to evaluate major geochemical processes controlling solute sources, hydrochemical evolution and hydrological connectivity. The results suggested that the groundwater chemistry is primarily controlled by water-rock interaction with Ca-Mg-HCO₃ type water facies revealing carbonate weathering as a dominant process. Geochemical modeling suggested that groundwater is undersaturated with respect to calcite, dolomite, gypsum and fluorite that facilitates mineral dissolution, while saturation with Fe(III) oxides suggests localized precipitation of ferrous minerals. The regression line of streamwater (δ²H = 6.8 × δ¹⁸O + 18, R² = 0.97) and groundwater (δ²H = 7.2 × δ¹⁸O + 22, R² = 0.97) revealed minor variation in slope, attributed to subtle differences in fractionation processes influenced by local environmental factors that promote evaporation of streamwater. The isotopic similarity between streamwater and riparian groundwater underscores a high degree of hydraulic connectivity. Contaminant assessment highlights arsenic (As) and fluoride (F⁻) as main geogenic pollutants in a few wells and springs, with potential health risks for local populations, particularly infants and children. The Water Quality Index (WQI) and irrigation suitability indices suggest that groundwater is fit for drinking and agricultural use, except at few locations with elevated As and F⁻ concentration. Self-organizing maps (SOM) and Pearson correlation analyses further illustrate the spatial variability of hydrochemical parameters and contamination hotspots. The findings emphasize the need for sustainable groundwater management strategies to mitigate contamination risks and ensure long-term water security in the KRB.