Water stable isotopes (18O and 2H) are widely used as ideal tracers to track water through
the soil and to separate evaporation from transpiration. Due to the technical developments in …

Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Partitioning of evapotranspiration (ET) into evaporation from the soil (E) and transpiration
through the stomata of plants (T) is challenging but important in order to assess biomass …

The measurement and simulation of water vapor isotopic composition has matured rapidly
over the last decade, with long‐term data sets and comprehensive modeling capabilities …

Continental precipitation not routed to the oceans as runoff returns to the atmosphere as
evapotranspiration. Partitioning this evapotranspiration flux into interception, transpiration …

Plant root water uptake (RWU) has been documented for the past five decades from water
stable isotopic analysis. By comparing the (hydrogen or oxygen) stable isotopic …

Stable water isotopes are widely used in ecohydrology to trace the transport, storage, and
mixing of water on its journey through landscapes and ecosystems. Evaporation leaves a …

Accurate quantification of evaporative losses to the atmosphere from surface water bodies is
essential for calibration and validation of hydrological models, particularly in remote arid and …

The variations of δ17O and δ18O in recent meteoric waters and in ice cores have proven to
be an important tool for investigating the present and past hydrologic cycle. In order to close …

The theoretical basis for application of stable isotope mass balance of lakes is described for
a range of climatic situations including low latitude, high latitude, high altitude, continental …