Sealing, crusting and cracking of crusts of the soil surface has been
observed in many parts of the world in areas with sandy, silty and loa
my soils. Sealing and crust formation occurs under the influence of ra
in storm and drying weather, With prolonged drying, surface crusts mig
ht crack, leading to complex situations with respect to infiltration a
nd runoff generation. Cracking of crusted loamy soils appears to be a
general process. This study aims to measure the hydraulic properties o
f fully crusted and cracked-crusted areas and to evaluate the effects
of these measurements on catchment discharge and soil loss in a loess
region of the Netherlands, using the LISEM soil erosion model. Samples
with minimum infiltration rates (fully crusted) and with maximum infi
ltration rates (cracked-crusted surfaces) were taken from fields with
bare soil or winter wheat and their soil hydraulic functions were meas
ured, The results of these measurements were used as input in the LISE
M soil erosion model, Simulations of discharge and soil loss were done
for each of these two land-uses and for two rain events, Additionally
, simulated discharge and soil loss under actual recorded land-use wer
e calculated. In all cases, soils with no surface cracks produced high
er figures for discharge and soil loss than those where 10% of the sur
face crust was cracked, For a good interpretation of the results for s
oil loss, the spatial distribution of cracked-crusted areas and fully
crusted areas has to be investigated in detail. To deal with cracked-c
rusted and fully crusted areas in simulation modelling, care has to be
taken to accurately measure the soil physical functions representing
the maximum and minimum infiltration rates. An assignment of these fun
ctions to calculation grids has to be made. As the LISEM model is capa
ble of assigning different soil physical functions to each calculation
grid, an improved prediction of the soil physical behaviour of the ca
tchment can be simulated.