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复杂河道边界对滑坡涌浪周期的影响
引用本文:王梅力,祖福兴,徐绩清,王平义,韩林峰.复杂河道边界对滑坡涌浪周期的影响[J].水利水运工程学报,2020,0(5):33-39.
作者姓名:王梅力  祖福兴  徐绩清  王平义  韩林峰
作者单位:重庆交通大学 国家内河航道整治工程技术研究中心,重庆 400074;重庆交通大学 建筑与城市规划学院,重庆 400074;重庆市交通规划勘察设计院,重庆 400074;重庆交通大学 国家内河航道整治工程技术研究中心,重庆 400074
基金项目:国家自然科学基金资助项目(51479015);山区公路水运交通地质减灾重庆市高校重点实验室开放基金项目(kfxm2018-15)
摘    要:滑坡涌浪对涌浪生成和传播区域可能造成巨大影响。河道型水库滑坡涌浪受河道边界的作用会产生波浪叠加。为研究河道边界对滑坡涌浪周期的影响规律,借助长江三峡库区万州某河段与原型一致的物理模型,基于FLOW-3D计算流体力学软件建立三维滑坡涌浪数值模型,给出了数值求解、网格划分和边界条件设置方法,并经物理模型试验对建立的三维数学模型进行一致性较好的验证。按照滑坡体入水点位于河道直线段、弯道凸岸顶点、弯道凹岸顶点3种工况,模拟分析复杂河道边界对滑坡涌浪周期的影响规律,绘制波谱强度与频率关系图,得出不同岸坡坡度、弯道凹岸平面曲率、凹岸圆弧角度、凸岸圆弧角度对涌浪周期的影响规律。

关 键 词:滑坡涌浪  复杂河道边界  反射波周期  数值模拟  FLOW-3D
收稿时间:2019-07-31

Effect of complicated river boundaries on the cycle of landslide surge
Affiliation:1.National Engineering Technology Research Center for Inland Waterway Regulation, Chongqing Jiaotong University, Chongqing 400074, China2.College of Architecture and Urban Planning, Chongqing Jiaotong University, Chongqing 400074, China3.Chongqing Traffic Planning Survey and Design Institute, Chongqing 400074, China
Abstract:Landslide surge can cause huge damage to the area of surge generation and propagation. The effect of the river boundary on the landslide surge in a river-type reservoir will result in wave superposition. In order to study the effect of river boundary on the surge period of landslide, a 3-d numerical model of landslide surge is established based on the FLOW-3D computational fluid dynamics software, using a physical model which is identical to the prototype of a river section in Wanzhou in Three Gorges Reservoir area. The methods of numerical solution, mesh generation and boundary condition setting are given, and the consistency of the three-dimensional mathematical model is verified by physical model test results. According to the three working conditions that the water entry point of the landslide body is located in the straight section of the river channel, at the crest of the convex bank and at the crest of the concave bank of the curved channel, the relation graphs of spectrum intensity and frequency are drawn. The influence law of the complicated river boundary on the surge period of the landslide is analyzed, and the effects of different bank slopes, curvature of curved concave bank, arc angle of concave bank and arc angle of convex bank on swell period are obtained.
Keywords:
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