Spatial patterns of sediment delivery to valley floors: sensitivity to sediment transport capacity and hillslope hydrology relations

There is considerable interest in large-scale spatial patterns of sediment transport in catchments, and this topic is often approached. using terrain-based modelling. In such models topography influences the discharge of overland now and its sediment transport capacity. The sediment transport capacity of overland flow is commonly expressed as a power function of slope and discharge (i.e, q(s) = k(1)q(beta)S(gamma)). The relationship between discharge and contributing area can also be expressed as a power function. Several reviews reveal a limited range of values for the two exponents beta and gamma. In this paper we examine the sensitivity of catchment-scale patterns of sediment delivery to valley Boors to a range of sediment transport capacity and hillslope hydrology parameterizations, using two catchments on the southern tablelands of New South Wales. The results indicate that, over the limited range of beta and gamma identified within the literature, sediment deliveries to valley floors across the two catchments al e similar for all but one of five sediment transport capacity relationships. The patterns are dominated by the trend in slope through each catchment. The sensitivity to hillslope hydrology of predicted sediment delivery patterns is strong in the catchment with systematic variation in unit hillslope area, and weak in the catchment for which there are no systematic trends in unit hillslope area. We believe there is less experimental evidence to restrict choice of hillslope hydrology parameters than there is for sediment transport capacity. Copyright (C) 2001 John Wiley & Sons, Ltd.