Field infiltration tests using portable rainfall infiltrometers were c
onducted in the Wangjiagou experimental basin in the hilly loess regio
n of north China. Based on data collected at 27 sites, a topographic z
onation of infiltration characteristics was observed. The average stea
dy infiltration rate and the average pending time decreased from the h
illtop to the hillslope and further decreased to the gully wall. Such
a zonation is closely related to the variations of topography, soil an
d land use conditions in the study area. A general infiltration model
is proposed. Collected field data are used to establish the applicabil
ity of the proposed model in the study area.