Multi-attribute parameterization modelling to assess response of microtopographic variation to rainfall-seepage coupled erosion

Abstract

Slope microtopography redistribution caused by the process of surface–subsurface hydrology results in the randomness and nonlinearity of erosion behavior. However, the erosion effects of various microtopographic features under the rainfall-seepage coupled impact remain inadequately explored. In this work, a specialized parameterization framework was employed, coupling numerical attribute, shape, and structure with the spatial pattern of microtopography, specifically to quantify changes in microtopography and to clarify their response mechanisms to rainfall-seepage erosion on purple soil slopes. The continuous rainfall-seepage simulation experiments were conducted on a 15° tilled-slopes differing in microreliefs (conventional tillage, CT; artificial digging, AD; ridge tillage, RT) with constant rainfall intensity of 1.0 mm min−1 coupling three seepage rates of 2, 4 and 8 L/min, respectively. Results revealed that the elevation decay occurred in the stage of transition from sheet erosion to rill erosion for CT, AD and RT slopes, representing a “erosion > deposition” feature. The numeric roughness and multifractal pattern of microtopography showed RT > AD > CT slope during the rainfall-seepage erosion. The spatial change of microtopography was attributed to structural-oriented factors because the nugget ratio with less than 25 % accounted for 73.33 %. Synchronously, the runoff, sediment yields and concentrations increased with the increase of rainfall-seepage intensity. It was found that the response of roughness index on soil erosion was more obvious for smooth surface with relatively contribution rate of 81 %, while the change of microstructure (H) and multifractal shape (ΔD) were more sensitive to erosion process on AD and RT slopes respectively. The results reported in this study have important implications for an in-depth apprehending of microtopography erosion effects in saturation-excess dominated slope cropland.