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When the soil zone becomes saturated, water percolates downward.
Precipitation infiltrates below the ground surface into the soil zone.
Plants absorb water through their roots, so concentrating irrigation in the soil zone is crucial.
With constant reinforcement length, the reinforced soil zone could be treated as a deep beam.
The unsaturated soil zone had a significant effect on removing NH4 and NO3 infiltrated from the surface water.
The SVE technique is used to remove volatile chlorinated hydrocarbons (VCHC) from the water-unsaturated soil zone.
In contrast, reinforcement length to a very large extent determined the lateral displacement at the back of reinforced soil zone.
Particularly in groundwater, additional oxygen sources from the soil zone may be quantified with new oxygen isotope signals that were influenced by diffusion.
The effects of soil type on measured loads at the connections and peak tensile loads located within the reinforced soil zone are identified.
Hydrologic balance means the relationship between the quality and quantity of water inflow to, water outflow from, and water storage in a hydrologic unit such as a drainage basin, aquifer, soil zone, lake, or reservoir.
The potential effect of rainfall and evapotranspiration on contaminant migration in the unsaturated soil zone was studied using a deterministic dynamic modeling approach.
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CEO of Professional Science Editing for Scientists @ prosciediting.com