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infiltration capacity
If inputs exceed the infiltration capacity then overland flow is produced.
      
Infiltration Factors affecting infiltration, rate, Infiltration capacity and its determination.
      
Infiltration capacity is the ability of the soil to absorb surface water.
      
In the first, surface runoff occurs when the rain rate exceeds the soil infiltration capacity.
      
In this case, design alternatives must be supported by a field investigation that establishes the infiltration capacity of the subgrade materials.
      
In summer the moderately high infiltration capacity of soil prevents runoff on the upland except during unusually intense storm events.
      
In particular, when the water-input rate is less than the corresponding soil infiltration capacity, all the rainfall infiltrates into the soil.
      
In the early spring the infiltration capacity of the soil may be very low because of ice contained within the soil.
      
JLOWintensity = rains twice the duration of high intensity rains and only slightly above the infiltration capacity of the soil.
      
Overall, these sediments probably have high infiltration capacity and a high horizontal permeability.
      
Runoff in WEPP-WTM is calculated by subtracting the infiltration capacity of the soil from the rainfall rate.
      
Runoff is limited on soils with a high infiltration capacity.
      
Sand can be assumed to have an infiltration capacity of around 200 litres per 2 per day.
      
Such organic debris also covers the soil, preventing splash erosion, and maintains infiltration capacity.
      
Set aside a portion of the site's native vegetation and areas with soils that have a high infiltration capacity.
      
Saturated hydraulic conductivity is an index of the infiltration capacity of filter media.
      
Soil infiltration capacity allows water to infiltrate at different rates.
      
This underground data is helpful to know the permeability >amp; infiltration capacity of the rocks and ground water ability to run the stream flow.
      
This limits their infiltration capacity, so that only shallow hybrid layers are formed.
      
These variables affect such other soil characteristics as cation exchange capacity, permeability, and infiltration capacity.
      
 

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