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    中国百强科技报刊

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    中国高校百佳科技期刊

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    Volume 48 Issue 9
    Sep.  2023
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    Article Contents
    Lü Liqun, Zhou Guanyu, Ma Chao, Huang Feng, Gao Ziqi, 2023. Coupling Process of Debris Flow Erosion and Wavy Flow Caused by Incision on Paleosedimentary Basin. Earth Science, 48(9): 3389-3401. doi: 10.3799/dqkx.2022.329
    Citation: Lü Liqun, Zhou Guanyu, Ma Chao, Huang Feng, Gao Ziqi, 2023. Coupling Process of Debris Flow Erosion and Wavy Flow Caused by Incision on Paleosedimentary Basin. Earth Science, 48(9): 3389-3401. doi: 10.3799/dqkx.2022.329

    Coupling Process of Debris Flow Erosion and Wavy Flow Caused by Incision on Paleosedimentary Basin

    doi: 10.3799/dqkx.2022.329
    • Received Date: 2022-04-21
      Available Online: 2023-10-07
    • Publish Date: 2023-09-25
    • Uplift of the Qinghai-Tibet Plateau result in accelerating fluvial incision of the Yellow River. The incision of the Yellow River makes Daheba River, one of the tributaries of the Yellow River, incise quickly on the flat and broad Tongde basin covered by deep fluvial sediments and loess. Tongde basin has changed from sedimentary area to erosion area, and debris flow are developing. The study on the mechanism of debris flow groups occurrence is of great significance to the prevention and mitigation of debris flow in paleosedimentary basins. This paper analyzed the characteristics of sediments soil mechanics, water system of Daheba River and the mechanism of erosin and motion of debris flow through field investigation and physical model. Analysis showed that the Daheba River incised on thick lacustrine sediments and the sediments composed by gravel and sand, good sorting, were beneficial to the formation of debris flow. Under the condition of uplift of Qinghai-Tibet Plateau and rapid incisions of Yellow River, the headward erosion of Daheba River had made the river energy gradually extend upstream. Therefore, different distribution and development characteristics were at different river sections of Daheba River. The thickness and incision depth of pebble sand sediment layer determine the erosion intensity and development trend of debris flow. The intermittent energy source of debris flow head is caused by the process of water flow incision, debris flow erosion, pebble sand separation and collapse, which promotes the fluctuation of debris flow movement.

       

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