A stochastic model governing the downslope transport of a sediment par
ticle during an erosion event is described. Particles alternate betwee
n resting on the soil bed and being transported by the overland flow.
Probability densities and moments are constructed for the distribution
of a particle's position at a given time, and also for time of passag
e to a given location. We show that a suitable averaging of the stocha
stic particle motions in our model gives rise to the deterministic ero
sion differential of Hairsine and Rose (Hairsine, P., Rose, C., 1991.
Soil Sci. Sec. Am. J. 55 (2), 320-324). The model generalized H. Einst
ein's stochastic model (Der Geschiebebetrieb als Wahrscheinlichkeitspr
oblem, Verlag Rascher, Zurich, 1937) for bedload transport in streams.
(C) 1998 Published by Elsevier Science B.V.