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The relationship of dD vs. d 18 O in the surface water and groundwater

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WESTERN GROUNDWATER CONGRESS: Multiple perspectives on groundwater

Evapotranspiration and groundwater inputs control the timing of diel cycling of stream drying during low-flow periods - Frontiers

Plot of δD vs. δ 18 O for precipitation samples. LMWL represents the

9 Risks of Metals Contamination in Coeur d'Alene Lake

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References - Estimating Groundwater Recharge

Oxygen and hydrogen stable isotopes as recharge indicators

Isotopes (δD and δ18O) in precipitation, groundwater and surface

Frontiers Riverbed Temperature and 4D ERT Monitoring Reveals Heterogenous Horizontal and Vertical Groundwater-Surface Water Exchange Flows Under Dynamic Stage Conditions

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Delineation of suitable sites for groundwater recharge based on