Soil hydrophobicity affects the susceptibility of soils to erosion in a var
iety of ways (e.g. increased aggregate stability, reduced infiltration capa
city, enhanced overland flow), but there are problems concerning the overal
l assessment of its erosional impact. Three current problems are discussed:
(I) poor isolation of hydrophobicity from other effects; and poor understa
nding of its overall impact: (2) areally, at slope and catchment scales; an
d (3) temporally, over periods of months or years rather than on a storm ba
sis. These problems are highlighted with reference to the literature and to
research in Portugal on highly hydrophobic forest soils. A conceptual mode
l relating erosion risk to three key aspects of soil hydrophobicity (tempor
al contiguity, spatial contiguity and the thickness of any overlying hydrop
hilic soil) is presented in order to provide a framework for future researc
h into hydrophobicity-soil erosion Links. (C) 2000 Elsevier Science B.V. Al
l rights reserved.