项伟, 柳景华, 贾海梁, 黄伟. 2016: 长江某水电站坝基剪切带发育规律与抗滑稳定研究. 工程地质学报, 24(5): 788-797. DOI: 10.13544/j.cnki.jeg.2016.05.008
    引用本文: 项伟, 柳景华, 贾海梁, 黄伟. 2016: 长江某水电站坝基剪切带发育规律与抗滑稳定研究. 工程地质学报, 24(5): 788-797. DOI: 10.13544/j.cnki.jeg.2016.05.008
    XIANG Wei, LIU Jinghua, JIA Hailiang, HUANG Wei. 2016: DEVELOPMENT MECHANISM OF SHEAR ZONES AND STABILITY OF DAM FOUNDATION OF A HYDROPOWER STATION LOCATED IN YANGTZE RIVER. JOURNAL OF ENGINEERING GEOLOGY, 24(5): 788-797. DOI: 10.13544/j.cnki.jeg.2016.05.008
    Citation: XIANG Wei, LIU Jinghua, JIA Hailiang, HUANG Wei. 2016: DEVELOPMENT MECHANISM OF SHEAR ZONES AND STABILITY OF DAM FOUNDATION OF A HYDROPOWER STATION LOCATED IN YANGTZE RIVER. JOURNAL OF ENGINEERING GEOLOGY, 24(5): 788-797. DOI: 10.13544/j.cnki.jeg.2016.05.008

    长江某水电站坝基剪切带发育规律与抗滑稳定研究

    DEVELOPMENT MECHANISM OF SHEAR ZONES AND STABILITY OF DAM FOUNDATION OF A HYDROPOWER STATION LOCATED IN YANGTZE RIVER

    • 摘要: 坝基剪切带是水利水电工程建设中经常遇到的重大工程地质问题,常对坝基岩体稳定性有着直接影响;研究剪切带的工程地质特征特别是空间发育与分布特征,对红层地区水利水电工程建设具有重要意义。本文以长江某水电站为例,从坝基红层沉积环境与沉积相分析入手,通过对坝基岩性组合、矿物组成、结构和粒度标志、沉积构造等的综合分析,恢复坝基古沉积环境,进一步确定原生软弱夹层的沉积微相;结合区域地质构造背景,分析剪切带发育规律与空间分布特征,进而开展坝基抗滑稳定研究。研究结果表明:层间剪切带的发育及空间分布特征主要受红层沉积环境与沉积相控制;坝基层间剪切带大多发育在半韵律层的顶部,即发育在软硬岩层接触面及厚层软岩内;由于岩相变化快,所以同一剪切带的空间分布常不连续,在不同空间位置的类型也不尽相同;剪切带是具多种黏土矿物成分且含量不同的高分散体系,其具有不同的工程地质特征及强度参数;剪切带空间分布特征与性状的不连续性,对坝基岩体稳定性有着重要影响,常直接关系到工程的建设工期与造价。因此,以沉积环境和沉积相分析为切入点,能够清晰的认识剪切带的空间发育分布规律,可用于指导红层地区工程地质条件评价与坝基岩体稳定性分析。

       

      Abstract: Shear zone has direct influence on stability of dam foundation, which is an important engineering geological issue, and is very common in the construction of hydroelectric project. Studying the engineering geological characteristics especially development and distribution characteristics of shear zones has significant and positive influence on the process of construction. In this paper, the sedimentary environment and facies in the dam area are investigated by the result of lithology, mineral composition, mineral formation, grain size parameters, sedimentary structure and so on. Development mechanism and distribution characteristics of shear zone then are studied based on the regional geological structure and the results of palaeosedimentary environment and sedimentary microfacies of protosomatic weak intercalation. Taking the distribution characteristics of shear zones into account, stability of dam foundation further is analyzed and evaluated. The results display that development and distribution of shear zones are determined by sedimentary environment and facies. It arises at the top of hemicyclothem frequently. Due to the multiple lithofacies, uncontinuity of spatial distribution of shear zones is very common. The types of the same shear zone in different position are also various. In addition, XRD and XRF results show that shear zones are highly dispersed system which is composed of various clay minerals, which demonstrates different engineering geological characteristics and strength parameters. Furthermore, FLAC3D states that the uncontinuity of spatial distribution and behaviors of shear zones have great influence on the stability of dam foundation, concerning to the project duration and cost directly. Consequently, studying the shear zones from the perspective of sedimentary environment and facies is available to have a clear understanding about development and distribution characteristics of shear zones, having significant influence on the evaluation of engineering geological condition and stability analysis of dam foundation.

       

    /

    返回文章
    返回