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    川西高原工程扰动区松散土坡植被抗侵蚀作用机制

    Mechanism of erosion resistance of vegetation on loose soil slopes in engineering-disturbed areas of the western Sichuan Plateau

    • 摘要: 背景为揭示植被对松散边坡坡表颗粒冲刷启动的影响规律,依托四川省盐源县白草坡光伏发电场工程,开展室内水槽冲刷模型试验。方法采用均匀圆柱形钢条模拟刚性植被,构建不同坡度(5°、10°、15°)的松散颗粒边坡模型,系统设置植被高度、植被密度及颗粒粒径等工况,模拟降雨径流条件下的坡面冲刷过程。通过高速摄像机监测坡表颗粒运动状态,获取颗粒发生明显位移时的临界径流水深。结果试验结果表明:坡度增大使颗粒冲刷启动的临界径流水深显著降低,且呈非线性变化特征。植被高度的增加可提高颗粒冲刷启动所需的临界径流水深,但其增效随坡度增大而减弱:当坡度为5°时,植被高度由3 cm增至5 cm对应的临界径流水深增量为0.022 m;坡度为10°和15°时,该增量分别为0.012 m和0.010 m。颗粒粒径对临界径流水深的影响相对有限,在同一坡度条件下,4.5 mm与7.5 mm颗粒对应的临界径流水深差值均不超过0.006 cm,表明在粒径较小条件下,颗粒稳定性接近启动阈值。随着植被密度增大,径流能量耗散增强,颗粒冲刷启动所需的临界径流水深整体提高。结论坡度是控制松散边坡颗粒冲刷启动的主导因素,其增大会削弱植被及颗粒粒径的防护效应。研究成果可为刚性植被覆盖条件下非黏性边坡的水土保持与坡面冲刷防治提供试验依据。

       

      Abstract: Background To elucidate the influence of vegetation on the initiation of particle scouring on loose slopes, laboratory flume scour model tests were conducted based on the Baicaopo Photovoltaic Power Station project in Yanyuan County, Sichuan Province. Methods Uniform cylindrical steel rods were employed to simulate rigid vegetation. Loose granular slope models with varying inclines (5°, 10°, 15°) were constructed. Conditions including vegetation height, density, and particle size were systematically varied to simulate slope scouring processes under rainfall runoff conditions. High-speed cameras monitored particle movement on the slope surface to determine the critical runoff depth at which particles exhibited significant displacement. Results Experimental findings indicate that increasing slope gradient significantly reduces the critical runoff depth required to initiate particle scouring, exhibiting a non-linear relationship. Elevating vegetation height increases this critical depth, though this effect diminishes with steeper slopes: at 5° gradient, raising vegetation height from 3 cm to 5 cm increases the critical depth by 0.022 m; while at 10° and 15° slopes, this increment was 0.012 m and 0.010 m respectively. Particle size exerted relatively limited influence on critical flow depth; at identical slopes, the difference in critical flow depth between 4.5 mm and 7.5 mm particles did not exceed 0.006 cm, indicating particle stability approached the initiation threshold under smaller grain sizes. As vegetation density increases, runoff energy dissipation intensifies, leading to an overall rise in the critical runoff depth required to initiate particle scouring. Conclusions Slope gradient is the dominant factor controlling particle scour initiation on loose slopes; its increase diminishes the protective effects of vegetation and particle size. These findings provide experimental evidence for soil conservation and slope scour prevention on non-cohesive slopes under rigid vegetation cover conditions.

       

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