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Numerical analysis of landslide-generated impulse waves affected by the reservoir geometry

机译:储层几何影响影响的滑坡脉冲波的数值分析

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摘要

Impulse waves generated by landslides are a potential major hazard for the operation of hydropower reservoirs, as they pose a serious threat to the dam, to residents and to properties along the shoreline. A number of experimental studies have been conducted based on generalized models to predict the wave characteristics, but using the results from these models to predict landslide-generated impulse waves may result in significant errors due to wave reflection caused by changes in the reservoir width. To investigate the effects of reservoir geometry on the characteristics of landslide-generated waves during propagation, 14 numerical experiments were performed using Tsunami Squares. The real-sized numerical models were based on statistical data from the Yangtze River and a generalized cross section of the Gongjiafang landslide located in the Three Gorges Reservoir, China. Two types of generalized reservoir geometries were investigated - namely with converging and diverging reservoir widths. It is shown that the wave amplitudes decrease with increasing reservoir width, while wave heights and troughs have a complicated dependence on changes in reservoir width. Compared to the amplitudes of the leading waves, the wavelengths and start-up time of wave amplitudes were more affected in the converging reservoir models by variations in the reservoir width.
机译:山体滑坡产生的脉冲波是水电站的运作的潜在重大危害,因为它们对大坝对居民和海岸线的性质构成严重威胁。已经基于广义模型进行了许多实验研究以预测波特性,但是使用这些模型的结果来预测滑坡产生的脉冲波可能导致由于储存器宽度的变化引起的波反射引起的显着误差。为了研究储层几何形状对传播期间山次隆起的波的特性的影响,使用海啸正方形进行了14个数值实验。实际规模的数值模型基于长江统计数据以及位于中国三峡库区的公鸡坊滑坡的广义横截面。研究了两种类型的广义储层几何形状 - 即在会聚和分歧储层宽度。结果表明,波浪幅度随着储层宽度的增加而降低,而波浪高度和槽具有对储存宽度变化的复杂依赖性。与前导波的幅度相比,通过储存器宽度的变化,在会聚储层模型中,波长的波长和启动时间更受影响。

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