岩质滑坡涌浪对三峡库区岸坡的冲刷模型试验
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TV139.2+5

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国家自然科学基金(51479015);西部交通建设科技项目(20113288141160)


Experimental study on erosion of bank slopes induced by rock landslide surges in the Three Gorges Reservoir Region
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    摘要:

    为了解岩质滑坡涌浪对三峡库区岸坡的冲刷破坏情况,以万州港为原型,设计岩体滑坡涌浪物理模型试验,分析了不同滑坡体体积和滑面倾角情况下滑坡涌浪对库区3种不同粒径岸坡的冲刷深度和静水面上下15 m岸坡整体的冲刷特性。试验结果表明:岸坡最大冲刷深度与滑坡体宽度及厚度呈正相关关系;滑坡体体积较大时,岸坡冲刷深度在滑坡体滑面倾角为40°时最大,滑坡体体积较小时,岸坡冲刷深度在滑坡体滑面倾角为60°时最大;岸坡需防护范围为静水面上下7 m,在静水面和岸坡接触的部位需重点防护。根据试验数据,给出了计算岸坡最大冲刷深度的经验公式。

    Abstract:

    In order to study the landslide failure of rock slopes induced by rock landslide surges in the Three Gorges Reservoir Region, physical model tests of rock landslide in Wanzhou port have been designed as the prototype. The influences of landslide volumes, inclination angles of the slip surface and three different slope soil particle diameters were studied in the experiment. The scouring depthsand the overallerosion characteristics of slopesin the range of 15 m below and above static water level have been analyzed. The results show that the maximum scouring depths are in positive correlation with the width and thickness of the landslide mass. For large volume of landslide mass, the scouring depth can reach its maxima if the inclination angle of the slip face is 40° while for relatively smaller volume of landslide mass, the inclination angle is 60°. The suggested scope for bank protection is in the range of 7 m below and above static water level. The empirical formula for the maximum erosion depth of bank slope was obtained based on experimental data.

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胡杰龙,王平义,喻涛,等.岩质滑坡涌浪对三峡库区岸坡的冲刷模型试验[J].水利水电科技进展,2018,38(1):88-94.(HU Jielong, WANG Pingyi, YU Tao, et al. Experimental study on erosion of bank slopes induced by rock landslide surges in the Three Gorges Reservoir Region[J]. Advances in Science and Technology of Water Resources,2018,38(1):88-94.(in Chinese))

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  • 收稿日期:2016-12-22
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  • 在线发布日期: 2018-02-02
  • 出版日期: 2018-01-10