Lisem: A Single‐event Physically Based Hydrological and Soil Erosion Model for Drainage Basins. I: Theory, Input and Output

Effect of natural restoration time of abandoned farmland on soil detachment by overland flow in the Loess Plateau of China

“…Soil detachment by overland flow decreased with soil cohesion (De Roo et al, 1996;Torri et al, 1998;Zhang et al, 2008), which increased with root density Du et al, 2010). Nevertheless, no significant correlation was found between soil cohesion and soil detachment capacity in this study.…”

Spatio-temporal characteristics of soil protection efforts of the Grain for Green Project in northern Shaanxi Province

“…(3) Previous research on soil erosion in northern Shaanxi has largely been on small watershed (Morgan, 1994;Wang et al, 1994;De et al, 1996), and the accuracy of the models used in such research can be verified via runoff volumes of basin hydrological stations. This study, however, simulates the soil erosion for the whole of the northern Shaanxi region, so verification cannot be done only by comparing data from a certain hydrological station.…”

Evolution of overland flow connectivity in bare agricultural plots

“…In order to use these results and the RSCf in hydrological models a possible approach could be to implement the subgrid variability of overland flow in a similar manner as for instance the Probability Density Model (PDM; Moore, ), which implements the subgrid variability of the ‘soil absorption capacity’ as a probability density curve. Alternatively, one may use the parameters defining the RSCf as a means to implement the progressive non‐linear nature of overland flow generation, similar to the openLISEM model (De Roo et al , , De Roo et al ,). This model takes into account the runoff that takes place before the excess rainfall reaches the maximum depression storage and reflects the gradual nature of overland flow generation.…”