Sediment export by water from an agricultural catchment in the Loam Belt of central Belgium

An agricultural drainage basin of 250 ha was selected in the Belgian Loam B elt to evaluate sediment export by water. Water discharge was continuously measured at the outlet of the catchment and suspended sediment samples were taken proportional with discharge during rainfall events. From these sampl es supended sediment concentration and grain-size distribution were determi ned, Within the catchment, regular surveys were conducted in order to obtai n detailed data on vegetation cover, soil surface parameters and erosion an d sedimentation features. Important variations in sediment yield were detec ted at various time-scales, ranging from a year, over a season to one event . These variations could be linked with processes occurring within the catc hment. Due to the development of a vegetation cover, the suspended sediment concentrations were lower during the summer period than during the winter period for the same discharge. The evolution in both suspended sediment con centration and grain-size distribution during the winter period is explaine d by variations in the soil surface state of the fields as well as the deve lopment of a rill and gully network. The positive hysteresis observed withi n a single event is explained by taking into account the distance between t he sediment source and the catchment outlet and not by sediment flushing. O ur analysis shows that the role of the main factors controlling the geomorp hic response of such a catchment can be identified only if measurements at the outlet are complemented by detailed data on the conditions within the c atchment. Catchment model calibration and validation are therefore impossib le if this information is lacking. (C) 2000 Elsevier Science B.V. All right s reserved.