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Stable isotopic and geochemical identification of groundwater evolution and recharge sources in the arid Shule River Basin of Northwestern China
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inferred← citeshttps://doi.org/10.5194/hess-29-4417-2025openalex-snapshot
Groundwater–surface water interactions across an arid river basin: spatial patterns revealed by stable isotopes and hydrochemistry
inferred← citeshttps://doi.org/10.6084/m9.figshare.13065749openalex-snapshot
Additional file 1 of Is salinity the main ecological factor that influences foliar nutrient resorption of desert plants in a hyper-arid environment?
inferred← citeshttps://doi.org/10.70675/4fa2ce1azbf16z4533zb11dzd0adb44f686dopenalex-snapshot
Characterizing groundwater recharge processes in a semiarid mountain-front using stable isotopes, hydrochemistry and heat as a tracer (Ourika basin, Tensift, Central Morocco)
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