abstract |
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Artificial rainfall and tracer experiments were conducted on two hillslope sites to
identify runoff processes and to test a double porosity physically based numerical hillslope
model (QSOIL). The results show good agreement between the measured and the predicted runoff
components, matric potential and water content. The spatial and temporal behaviour of the
different runoff generation processes was determined. A distinct vertical macropore system,
resulting in bypass flow, and as the major contributing region for surface flow a highly
permeable structured A horizon were attributed to one hillslope site. In contrast, the soil
of the other site showed a bimodal pore size distribution, assumed to be a combination of
mesopores and micropores developed by plant roots, and resulting in a higher subsurface flow
response. |