Evapotranspiration (ET) is a major part of ecosystem water loss. This thesis aims to develop methods that partition soil water loss into evaporation (E) and transpiration (T). Water balance methods may improve with relative contributions of evaporation (E) and transpiration (T). Isotopic fractionation distinguishes soil water loss due to evaporation from that of plant uptake. This provides a means to assess E and T in retrospect rather than only measuring ET fluxes. To measure the isotopic composition of soil water, we used a liquid-vapor equilibration method following Wassenaar (2008). Experimental trials of different soil amounts and equilibration times were performed to adapt the liquid-vapor equilibration method for dry desert soils. We...
Until recently, it had been thought that humid catchment woody plants transpired primarily mobile so...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceStable isotopes of water (O-18 and ...
Partitioning evapotranspiration (ET) into soil evaporation E and plant transpiration T is important,...
Water stable isotopes are powerful tracers for partitioning of the terrestrial ecosystem water vapor...
Recent studies of plant water uptake assume that soil water isotopic composition can be used to infe...
International audienceIn this study, we performed a partitioning of evapotranspiration (ET) under fu...
Agricultural production in the hot and arid low desert systems of southern California relies heavily...
The stable isotopic composition of soil water is controlled by precipitation inputs, antecedent cond...
Disentangling ecosystem evapotranspiration (ET) into evaporation (E) and transpiration (T) is of hig...
Water stable isotopes are powerful tools for partitioning net into raw water fluxes such as evapotra...
Knowledge of the water fluxes within the soil-vegetation-atmosphere system is crucial to improve wat...
Total evapotranspiration (ET) is the key process that links the land and the atmosphere via water, e...
Knowledge of the water fluxes within the soil-vegetation-atmosphere system is crucial to improve wat...
Until recently, it had been thought that humid catchment woody plants transpired primarily mobile so...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceStable isotopes of water (O-18 and ...
Partitioning evapotranspiration (ET) into soil evaporation E and plant transpiration T is important,...
Water stable isotopes are powerful tracers for partitioning of the terrestrial ecosystem water vapor...
Recent studies of plant water uptake assume that soil water isotopic composition can be used to infe...
International audienceIn this study, we performed a partitioning of evapotranspiration (ET) under fu...
Agricultural production in the hot and arid low desert systems of southern California relies heavily...
The stable isotopic composition of soil water is controlled by precipitation inputs, antecedent cond...
Disentangling ecosystem evapotranspiration (ET) into evaporation (E) and transpiration (T) is of hig...
Water stable isotopes are powerful tools for partitioning net into raw water fluxes such as evapotra...
Knowledge of the water fluxes within the soil-vegetation-atmosphere system is crucial to improve wat...
Total evapotranspiration (ET) is the key process that links the land and the atmosphere via water, e...
Knowledge of the water fluxes within the soil-vegetation-atmosphere system is crucial to improve wat...
Until recently, it had been thought that humid catchment woody plants transpired primarily mobile so...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceStable isotopes of water (O-18 and ...
Partitioning evapotranspiration (ET) into soil evaporation E and plant transpiration T is important,...