To calculate soil erosion based on landunit in a catchment is a new and important method for estimation of soil and water conservation measuresTo achieve such a process based calculation in a catchment or a basin, soil erosion model with both landform factors and up and down stream relations in a catchment need to be developedMeanwhile, the runoff flow networks among landunits, which indicate the relations of runoff flow paths between landunits, are necessaryThe flow networks must be connected with soil erosion models to fit the model principlesIn this paper, the traditional technology of grid based flow network was improved according to loess soil erosion rolesA landunit based runoff and sediment flow network model was developed for simulating the flow process in whole basin, from top of basin to its outletThe flow network among landunit was calculated and three important parameters for soil erosion model were afforded: water and sediment flow order among landunits; the spatial distribution of the conflux amount among landunits; and the slope length of the runoff and sediment passing through each landunitThe soil erosion model was developed according to field observation of natural rainfall and artificial rainfalls with different slope, various land cover and different soil conditionsThe model was divided into three models according to landform positions: flat slope model for areas where the slope of landunit is less than 5 degree; slope model for simulation in whole slope; and gully bottom model for calculation of sediments transfer to the outletThese three models were connected with the landunit flow networks, and the parameters for each landunit such as soil type, slope, elevation, vegetation coverage, cultivating measures, landform position, slope length, etc, were automatically transferred from landunit file to the soil erosion model.
LIU Gao huan, CAI Qiang guo, ZHU Hui yi, TANG Zheng hong
. Simulation of Runoff and Sediment Flow in a Catchment Based on Landunit Flow Networks[J]. PROGRESS IN GEOGRAPHY, 2003
, 22(1)
: 71
-78
.
DOI: 10.11820/dlkxjz.2003.01.009