Recent research has directed attention to the properties of the eroded mate
rial because of its influence in deposition phenomena and in carrying capac
ity of pollutant materials.
In this paper, the spatial distribution of the content of nitrogen, phospho
rus and total organic carbon is firstly deduced using the measurements carr
ied out in 129 soil samples well distributed over the Sicilian Sparacia Bas
in and a Kriging interpolation method. Then the load of each chemical was c
alculated at morphological unit and basin scale using the above-mentioned s
patial distributions and sediment yield values calculated by a parametric a
pproach such as the revised universal soil loss equation (RUSLE) coupled wi
th a spatial disaggregation criterion of sediment delivery processes. Final
ly, at basin scale, a new expression of the enrichment ratio of a given pol
lutant has been proposed; the enrichment ratio values were also related to
the corresponding basin sediment delivery ratio values. (C) 2000 Silsoe Res
earch Institute.