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 …

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 …

The hydrogen isotope ratio of water cryogenically extracted from plant stem samples
(δ2Hstem_CVD) is routinely used to aid isotope applications that span hydrological …

Leaf water contains naturally occurring stable isotopes of oxygen and hydrogen in
abundances that vary spatially and temporally. When sufficiently understood, these can be …

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 …

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 analysis of the stable isotopic composition of hydrogen and oxygen in water samples
from soils and plants can help to identify sources of vegetation water uptake. This approach …

Stable isotopic analyses of soil-emitted N 2 O (δ 15 N bulk, δ 18 O and δ 15 N sp= 15 N site
preference within the linear N 2 O molecule) may help to quantify N 2 O reduction to N 2, an …

Stable isotope ratios of water (δ18O, δ2H) have long been used to study a core question in
plant ecology and ecohydrology:'From where do plants take up water?'Indeed, decades of …

Measurements of δ2H and δ18O composition of pore waters in saturated and unsaturated
soil samples are routinely performed in hydrological studies. A variety of in‐situ and lab …