Experiments were conducted in the laboratory to evaluate the influence of sediment concentration, sediment grain-size distribution, bed slope and flow discharge on sediment deposition rates and patterns associated with a reduction in bed slope. The experimental data clearly indicate that sediment de
Sediment transport by overland flow over an area of net deposition
✍ Scribed by L. Beuselinck; G. Govers; A. Steegen; T. A. Quine
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 217 KB
- Volume
- 13
- Category
- Article
- ISSN
- 0885-6087
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✦ Synopsis
Flume studies were conducted in order to evaluate the in¯uence of slope, sediment size, discharge and in¯ow sediment concentration on sediment deposition by overland ¯ow. Additionally, experiments were carried out to measure transport capacity of overland ¯ow at low slopes, using a wide range of discharges. The experimental data show that the hydraulic conditions where net deposition occurs can be divided into two domains. The ®rst domain is characterized by hydraulic conditions where transport capacity is not signi®cant. In the second domain net deposition still occurs but transport capacity is signi®cant. The size of the latter domain is dependent on the sediment size distribution, on the hydraulic roughness and on the in¯ow sediment concentration. The experiments clearly indicate the necessity of incorporating a threshold value in any deposition equation. These experiments demonstrate that shear stress is a valuable threshold for deposition modelling.
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