芦山抽水蓄能电站库区复杂堆积体成因研究

    Study on multi-stage genesis of complex deposits in reservoir area of Lushan Pumped Storage Power Station

    • 摘要: 堆积体形成原因不同,其结构和物理力学性质各有差异,对堆积体稳定性评价存在较大影响。芦山抽水蓄能电站下库库区成因不明的边坡堆积体可能对水电站的施工安全和长期运行安全构成威胁。为确保堆积体稳定性评价的准确性,基于详细的野外调查,采用无人机倾斜摄影、LiDAR航摄、钻探等技术手段,对芦山抽水蓄能电站下库库区堆积体进行了调查,并深入分析了堆积体的成因和地貌的形成演化过程。结果表明:①堆积体的主要物质来源于堆积体下游侧的陡崖;②堆积体内含有深度不一、不连续的软弱夹层,推测堆积体由下游陡崖多次崩塌所形成;③研究区至少发生过两个期次的大规模崩塌,又经历过长期的地表改造,形成现今的地貌;④基于对堆积体成因的深入探究,确认堆积体仅在基覆界面处存在贯通性的软弱界面,堆积体内部的软弱夹层深度不一且不连续,故在讨论堆积体稳定性时,应将堆积体基覆界面的结构和强度作为主要影响因素进行分析。研究成果可为类似复杂堆积体成因机制研究提供参考依据。

       

      Abstract: The formation reasons of accumulation bodies are different, with diverse structures and physical and mechanical properties, which bring about challenges on the stability evaluation of deposits.A slope accumulation body with unknown causes in the lower reservoir area of Lushan Pumped Storage Power Station may pose a threat to the construction safety and long-term operation safety of the hydropower station.In order to ensure the accuracy of the stability evaluation of the accumulation body, based on the detailed field investigation including the UAV tilt photography, LiDAR aerial photography, drilling and other technical means, the accumulation body was investigated, and the formation causes of the accumulation body and the evolution of geomorphology formation were analyzed in-depth.The results show that: ① The main material of the accumulation body originates from the steep cliff on the downstream side of the accumulation body.② The accumulation body contains soft and weak interlayers of varying depths and discontinuities, and it is assumed that the accumulation body is formed by multiple collapses of the downstream cliffs.③ It is speculated that at least two phases of large-scale landslides occurred in the study area, and the present landforms are gradually formed after a long period of surface modification.④ Based on the in-depth argument on the causes of the accumulation body, it is confirmed that the there is a through and weak interface at the base-cover interface of the accumulation body, and the depth of the weak interlayer inside the accumulation body is different and discontinuous.Therefore, the structure and strength of the base-cover interface of the accumulation body should be analyzed as the main influencing factors in exploring the stability of the accumulation body.The results can provide a reference basis for the study on genesis mechanisms of similar complex accumulation bodies.

       

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