Seepage Characteristics and Stability Analysis of Transmission Line Tower Bank Slope Under the Action of Reservoir Water

Rongquan Fan, Yifei Jiao, Feng Tian, Wenhui Zeng, Bin Dong
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Abstract

Based on the saturated unsaturated seepage theory and Geo-studio software (SEEP/W and SLOPE/W modules), this article calculates the seepage feature and stability coefficient of the reservoir bank slope of a 220kV transmission line N47 tower in Western Sichuan, it shows that the slope stability and seepage field are affected by the rising and falling speed of reservoir level. The analysis results explain that with the increase of the rising rate of reservoir level, the pore water pressure increases rapidly, the slower the rise of a phreatic line is, and the more obvious the depression is. The faster the drawdown rate of reservoir water level is, the faster the decrease of pore water pressure is, the slower the decline of saturation line is, and the more obvious the upward convex is. During the rise of reservoir level, it is beneficial to landslide stability, but with end of the rise, this favorable trend gradually weakens or even develops in the opposite direction; The dropping of reservoir level is unfavorable to landslide stability. After the descent, this unfavorable trend gradually weakens and develops in the opposite direction.
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水库水作用下输电线路塔岸边坡渗流特性及稳定性分析
基于饱和非饱和渗流理论和Geo-studio软件(SEEP/W和SLOPE/W模块),对川西220kV输电线路N47塔库岸边坡的渗流特征和稳定系数进行了计算,得出了库位升降速度对边坡稳定性和渗流场的影响。分析结果表明,随着储层水位上升速率的增大,孔隙水压力迅速增大,潜水线上升速度越慢,凹陷越明显。水库水位下降速度越快,孔隙水压力下降越快,饱和线下降越慢,上凸越明显。在水库水位上升期间,有利于滑坡稳定,但随着水位上升的结束,这种有利趋势逐渐减弱,甚至向相反方向发展;水库水位的下降不利于滑坡的稳定。下降后,这种不利趋势逐渐减弱,并向相反方向发展。
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