Flume studies were conducted in order to evaluate the influence of:slope, s
ediment size, discharge and inflow sediment concentration on sediment depos
ition by overland flow. Additionally, experiments were carried out to measu
re transport capacity of overland flow at low slopes, using a wide range of
discharges. The experimental data show that the hydraulic conditions where
net deposition occurs can be divided into two domains. The first domain is
characterized by hydraulic conditions where transport capacity is not sign
ificant. In the second domain net deposition still occurs but transport cap
acity is significant. The size of the latter domain is dependent on the sed
iment size distribution, on the hydraulic roughness and on the inflow sedim
ent concentration. The experiments clearly indicate the necessity of incorp
orating a threshold value in any deposition equation, These experiments dem
onstrate that shear stress is a valuable threshold for deposition modelling
. Copyright (C) 1999 John Wiley & Sons, Ltd.