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The single-porosity and dual-permeability models in HYDRUS-1D (&amp;Scaron;imůnek et al. 1998, 2003) were used to simulate variably-saturated water movement in clay soils with and without macropores. Numerical simulations of water flow for several scenarios of probable macropore compositions show a considerable impact of preferential flow on water infiltration in such soils. Preferential flow must be considered to predict water recharge in clay soils.

Numerical Study of Macropore Impact on Ponded Infiltration in Clay Soils