Abstract:
Gully erosion is one of the main causes of soil loss in dry lands. Understanding the dominant mechanisms
of erosion is important to achieve effective erosion control, thus in this study our main objective was to \ quantify the mechanisms involved in gully bank retreat as a result of three processes, falling of entire soil aggregates, transport of soil material by splash and by water running along gully banks (runoff), during rainfall events. The study was conducted in the sloping lands of the KwaZulu-Natal province, a region that is highly affected by gully erosion. Artificial rain was applied at 60 mmh−1 for 45min at the vertical wall of a gully bank typical to the area. The splash material was collected by using a network of 0.045 m2 buckets. The sediments in the running water were assessed by sampling the runoff
collected from a microplot inserted within the base of the bank, and collecting the fallen aggregates after
the rainfall simulation was complete. Results indicated that the overall erosion for the simulation was 721gm−2 h−1. Runoff erosion proved to be the dominant mechanism and amounted to 450gm−2 h−1, followed by
splash and fall down of aggregate (about 170 gm−2 h−1). Gully bank retreat occurred at a
rate of 0.55 mmh−1 and assuming that the soil bulk density is 1.3gcm−3, this corresponds to a retreat of
8.8 mmy−1. Extra polations to the watershed level, where about 500 m2 of gully bank are observed per
hectare, would lead to an erosion rate of 4.8 tha−1 y−1. These limited results based on a simulated storm show that the three main mechanisms (runoff, splash and fall down of aggregates) are responsible for
the retreat of gully banks and that to mitigate gully erosion, appropriate measures are required to control all three mechanisms. Further research studies are needed to confirm and to scale up, both in time and space, as the sedata are obtained at one location and from a single artificial storm.
