“…39 Yet, it has been demonstrated that the analysed water mixing ratio in CRDS has a strong impact on obtained δ 2 H and δ 18 O values, 37,38,40 which has high relevance for studies, where the isotopic composition is measured directly (and is difficult to control) in the water vapour, such as soil evaporation, soil water vapour, atmospheric water vapour, plant transpiration or xylem water in the gas phase. 12,41,42 With the development and application of new water stable isotopologue measurement techniques, 2,8,10,12,43,44 which are based on the direct measurement of water vapour of different mixing ratios, the water mixing ratio-dependency of stable water isotopologues with CRDS is gaining relevance. The direct equilibration method to sample, for instance, soil water vapour is based on thermodynamic equilibrium and full water vapour saturation, which is controlled by the ambient temperature that typically varies considerably under natural conditions.…”