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 …

Recent work in ecohydrology has shown that in some forested watershed systems, streams
and trees appear to return different pools of water to the hydrosphere. Thus far, evidence for …

Current land surface models assume that groundwater, streamflow and plant transpiration
are all sourced and mediated by the same well mixed water reservoir—the soil. However …

In this commentary, we summarize and build upon discussions that emerged during the
workshop “Isotope-based studies of water partitioning and plant–soil interactions in forested …

The role of groundwater as a resource in sustaining terrestrial vegetation is widely
recognized. But the global prevalence and magnitude of groundwater use by vegetation is …

Here we present a theoretical interpretation of high‐frequency, high‐quality tracer time
series from the Hafren catchment at Plynlimon in mid‐Wales. We make use of the …

Recent studies using water‐stable isotopes (δ18O and δ2H) have suggested an
ecohydrological separation of water flowing to streams or recharging groundwater and water …

Ecohydrological studies in seasonally dry climatic regions have revealed isotopic separation
of the sources of water used by trees and those that generate stream flow, also referred to as …

Using stable isotope data from soil and vegetation xylem samples across a range of
landscape positions, this study provides preliminary insights into spatial patterns and …

Recent tracer-based studies using stable isotopes of hydrogen and oxygen showed that
different methods for extracting water from plant tissues can return different isotopic …