For the determination of groundwater recharge processes in arid environments, vadose zone water fluxes and water storage should be considered. To better understand and quantify vadose zone processes influencing groundwater recharge, a soil column experimental setup has been developed that mimics arid atmospheric conditions and measures water and temperature fluxes in high temporal and spatial resolution. The focus of the experiment was on the determination of water infiltration, redistribution, evaporation and percolation under non-isothermal conditions. TDR rod sensors and a specific TDR "Taupe" cable sensor were used for water content measurements and allowed the infiltration fronts to be traced over the whole column length. Applying sing...
Water deficit and salt accumulation in soil are serious problems in crop fields in semi-arid regions...
Tracer methods are commonly used for estimation of soil water and groundwater recharge flux especial...
Unsaturated zone processes play a key role in groundwater recharge as the thickness of the unsaturat...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
Vadose zone water fluxes in arid settings are investigated regarding their sensitivity to hydraulic ...
The two primary objectives of this research project were to determine quantitative estimates for soi...
The two primary objectives of this research project were to determine quantitative estimates for soi...
The two primary objectives of this research project were to determine quantitative estimates for soi...
International audienceFor monitoring the vadose zone, different strategies can be chosen, depending ...
International audienceFor monitoring the vadose zone, different strategies can be chosen, depending ...
Water deficit and salt accumulation in soil are serious problems in crop fields in semi-arid regions...
Tracer methods are commonly used for estimation of soil water and groundwater recharge flux especial...
Unsaturated zone processes play a key role in groundwater recharge as the thickness of the unsaturat...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
The quantification of vadose zone water fluxes in arid regions poses many difficulties due to low wa...
Vadose zone water fluxes in arid settings are investigated regarding their sensitivity to hydraulic ...
The two primary objectives of this research project were to determine quantitative estimates for soi...
The two primary objectives of this research project were to determine quantitative estimates for soi...
The two primary objectives of this research project were to determine quantitative estimates for soi...
International audienceFor monitoring the vadose zone, different strategies can be chosen, depending ...
International audienceFor monitoring the vadose zone, different strategies can be chosen, depending ...
Water deficit and salt accumulation in soil are serious problems in crop fields in semi-arid regions...
Tracer methods are commonly used for estimation of soil water and groundwater recharge flux especial...
Unsaturated zone processes play a key role in groundwater recharge as the thickness of the unsaturat...