Fundamental study on the effects of the keystone height and structure on sediment deposition in a high‐gradient channel
Autor: | Rei Itsukushima, Yuki Masago |
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Rok vydání: | 2019 |
Předmět: |
0106 biological sciences
geography Fundamental study geography.geographical_feature_category 010604 marine biology & hydrobiology 0208 environmental biotechnology Flow (psychology) Sediment 02 engineering and technology 01 natural sciences 020801 environmental engineering Short distance Head (geology) Antidune Flow velocity Environmental Chemistry Geomorphology Channel (geography) Geology General Environmental Science Water Science and Technology |
Zdroj: | River Research and Applications. 35:1443-1453 |
ISSN: | 1535-1467 1535-1459 |
DOI: | 10.1002/rra.3524 |
Popis: | Step–pool structures are among the most important structures in riverbed morphology that can contribute to the stabilization of riverbeds and riverbanks, energy dissipation during floods, and head reduction function. Two concepts have been suggested regarding step–pool formation: the development of antidunes (antidune concept) and keystone concept. The latter suggests that a large boulder (keystone) incidentally left in a river channel can trap pebbles and build a step–pool structure. The ultimate goal of this study is to reveal the step–pool formation process and establish a design method based on the keystone concept. This paper describes the experimental results of the effects of the keystone arrangement on sediment deposition. Step–pool formation based on the keystone concept has previously been focused on the process of sediment deposition a short distance from a keystone. However, this study reveals that the obstruction of sediment supply due to the decreased flow velocity in the main river course is an important factor. When the arrangement interval of keystones is small, the amount of sediment supply downstream decreases because the flow velocity at the main flow channel between the keystones does not increase. In contrast, the flow velocity at the main river course increases between the keystones, and supplied sediment is transported to the most downstream section if the keystone arrangement interval is large enough to join the flow from the bank side of the keystones. |
Databáze: | OpenAIRE |
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