摘要
Hillslope rill/interrill erosion has been investigated from the perspective of runoff transport of sediment.Recent advances in terrestrial laser scanning can provide high-resolution elevation data up to centimeter levels,and temporal digital elevation models(DEMs)enabled the detection and quantification of sediment redistribution.Erosion and deposition are spatially heterogeneous across hillslopes,and the choice of resolution is critical when using a DEM to study the spatial pattern of the processes.This study investigates the influence of grid size on the sediment change calculation and rill network delineation based on two surveys using a terrestrial laser scanner on a hillslope with well-developed rills in 2014 and 2015.Temporal DEMs were used to quantify elevation changes and used to delineate rill networks.We produced DEM pairs of incremental grid sizes(1-cm,2-cm,5-cm,8-cm,10-cm,15-cm,20-cm,and 30-cm)for DEM difference and rill network delineation.We used the 1-cm DEM as the reference to compare the results produced from other DEMs.Our results suggest that erosion mainly occurs on the rill sidewalls,and deposition on the rill floors,with patches of erosion/deposition within the interrill areas.Both the area and volume of detectable change decrease as the grid size increases,while the area and volume of erosion are less sensitive compared to those of deposition.The total length and number of rills decrease with the increased grid size,whereas the average length of rills increases.The mean offset between delineated rill network and the reference increases with larger grid sizes.In contrast to the erosion and deposition detected within rills,minor changes are detected on the interrill areas,indicating that either no topographic changes occurred or the changes were too small to be detected on the interill areas by our finest 1-cm DEMs.We recommend to use the finest possible grid size that can be achieved for future studies.
