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According to the robustness of solutions and the coverage of fluctuation range of infiltration rate, SHIP model can be integrated into hydrologic models to simulate SHR infiltration process and benefit the flood forecast.
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They are calculated for a range of infiltration rates and compared with those obtained by assuming the upper fringe boundary to be horizontal.
According to this classification each soil hydrological group is assigned a range of values of infiltration rates in mm/h.
Infiltration tests were carried out within the field in order to deal with the spatial variability of infiltration rate.
The non-conserved land demonstrated the lowest mean value of infiltration rate.
The effect of composite density and fiber type on the alteration of infiltration rate is discussed.
It is suggested that d1 and δ0 be chosen based on experimental measurements of infiltration rate and temperature excursion during silicon infiltration.
Numerous infiltration models are in use for estimation of infiltration rates.
Spatial variation of infiltration rates makes the management of surface irrigation systems a very complex process.
The effects of seasonal temperatures could result in five times difference of infiltration rates.
Variation of infiltration rates with landscape position influences the amount, distribution, and routing of overland flow.
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