考虑循环应力比空间分布特征的库岸老滑坡地震稳定性分析
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上海大学力学与科学工程学院

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TU411

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Seismic Stability Analysis of Reservoir Bank Slope Considering Spatial Distribution Characteristics of Cyclic Stress Ratio
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School of Mechanics and Engineering Science,Shanghai University

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    摘要:

    在强降雨和地震的联合作用下,忽略边坡土动力参数的空间分布特征,以潜在滑动面的安全系数作为评价指标,将无法准确评估再次发生滑坡的风险。以三峡库区中石榴树包老滑坡为研究对象,在降雨与水位变化的联合作用下,边坡仍处于稳定状态,但缺乏地震评估信息。为了准确分析老滑坡的地震稳定性,采用仿真地震波模型,并通过研究边坡土循环应力比(Cyclic Stress Ratio, CSR)的空间分布特征,修正边坡土的动力参数,基于Newmark滑块位移法,优化计算库岸边坡的永久位移。首先,基于等效线性分析理论,结合循环荷载的动三轴剪切试验,在不同CSR的循环荷载条件下,获得边坡土超孔隙水压力和动剪切模量的变化规律;然后,考虑三峡库区地震的微频特点,采用随机地震动模型,生成石榴树包老滑坡的仿真地震波,作为数值分析的动荷载。最后,利用GeoStudio中QUAKE/W子程序,输入随机地震动荷载和边坡土动力参数,获取CSR的空间分布特征,计算库岸边坡的永久位移,评估库岸边坡的地震稳定性。结论表明:石榴树包老滑坡浅层的崩积粉质黏土,难以出现液化现象。且在强降雨最不利工况的同期,如遭遇了三峡库区的设防地震,石榴树包老滑坡的永久位移将小于临界永久位移,表明不会再次失稳。

    Abstract:

    Under the combined action of heavy rainfall and earthquake, ignoring the spatial distribution characteristics of the geodynamic parameters of the slope, and using the safety factor of the potential sliding surface as the evaluation index will inaccurately assess the stability. The Shiliushubao old landslide in the Three Gorges Reservoir area is taken as the research object. Under the combined action of rainfall and reservoir water level change, the slope remains stable, but lacks seismically evaluation. To accurately analyze the seismic stability of old landslide, the artificial seismic wave model is used. By studying the spatial distribution characteristics of Cyclic Stress Ratio (CSR) of the slope soil, the dynamic parameters of the slope soil were adjusted. Based on the Newmark sliding displacement method, the permanent displacement of the reservoir bank slope was optimized. Firstly, based on the equivalent linear analysis theory, combined with the dynamic triaxial shear test of cyclic load, the variation of excess pore water pressure and dynamic shear modulus of slope soil will be obtained under the different CSR conditions. Then, considering the characteristics of frequent earthquakes in the Three Gorges reservoir area, the stochastic ground motion model is adopted which generates the artificially seismic wave for the Shiliushubao old landslide. Finally, the QUAKE/W module of GeoStudio 2018 is used to calculate the random ground motion and the dynamic parameters of the slope is obtained by the spatial distribution of CSR. The seismic stability of the reservoir bank slope is evaluated by calculating the permanent displacement. The conclusion shows that the shallow colluvial silty clay of the Shiliushubao old landslide is not prone to liquefaction. And under the heavy rainfall and the most unfavorable reservoir water level change, if the fortified earthquake is encountered in the reservoir area, the permanent displacement of the reservoir bank slope is less than the critical permanent displacement, which indicates that the Shiliushubao old landslide will not slide again.

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李天虎,王长虹,胡世韬,等. 考虑循环应力比空间分布特征的库岸老滑坡地震稳定性分析[J]. 科学技术与工程, , ():

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  • 收稿日期:2025-03-17
  • 最后修改日期:2025-04-22
  • 录用日期:2025-05-04
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