Measurable quantities of Cs-137 were found in soil samples from profil
es on a toposequence in southwest Niger. Erosional and depositional si
tes were identified by comparing Cs-137 inventories with a reference s
ite, although, because of the addition of dust, the identification of
such a site was difficult. A first approximation of the reference inve
ntory (2066 +/- 125 Bq m(-2)) was achieved by modelling. Marked dispar
ities between the Cs-137 profiles and the reference profile at some si
tes may be due to the eluviation of Cs-137 fixed to clay, where soils
have been exposed to cycles of wetting and drying. This hypothesis is
supported by principal components analysis and non-hierarchical multiv
ariate classification. Other divergences from the reference profile we
re interpreted as the results of the redeposition of material with sma
ll Cs-137 content, derived from subsoil and gully walls. These complic
ations created the need for additional modelling to estimate the net s
oil flux. At some sites the net soil flux was calculated using models
that related Cs-137 movement to soil redistribution. It appears that a
vegetation canopy protects accumulated dust from water erosion on ste
ep slopes and from wind erosion on gentle slopes. The net soil flux wa
s found to be -16 +/- 2 t ha(-1) yr(-1). (C) 1998 Elsevier Science B.V
.