Stable isotope compositions (δ2H, δ18O and δ17O) of rainfall and snowfall in the central United States
δD vs δ 18 O values and d-excess vs δ 18 O values for natural water
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The evolution of 17O-excess in surface water of the arid environment during recharge and evaporation
δD vs δ 18 O values and d-excess vs δ 18 O values for natural water
HESS - Controls on leaf water hydrogen and oxygen isotopes: a local investigation across seasons and altitude
Isotopic variability in tropical cyclone precipitation is controlled by Rayleigh distillation and cloud microphysics
Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area
The △δD and △δ 18 O values from the cities. Here, △δD (or △δ 18