Soil column experiments to quantify vadose zone water fluxes in arid settings
2012-03-01 ENVIRONMENTAL EARTH SCIENCES 2012 65(卷), 5(期), (1523-1533页)
JCR分区:
影响因子:
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 single irrigations of different amount and intensity showed the applicability of the experimental setup for the measurement of water movement in the unsaturated soil column.
相关推荐
- Hydrochemical and Tracer Monitoring to Assess Runoff Generation from Semi-arid Andean Headwater Catchments [2012-03-01]
- Using synoptic tracer surveys to assess runoff sources in an Andean headwater catchment in central Chile [2012-03-01]
- Use of isotopic signatures for the determination of natural recharge and chemical characterization of groundwaters: the case of Horombe plateau area, SW Madagascar [2012-03-01]
- Surface and subsurface conceptual model of an arid environment with respect to mid- and late Holocene climate changes [2012-03-01]