大型嵌岩封闭地连墙的水平静载试验研究

    The laterally static loading test of the closed rock-socketed diaphragm walls

    • 摘要: 封闭地下连续墙作为长期基础使用时有着出色的水平承载能力,依托深圳某项目,在现场进行了嵌岩封闭地连墙的水平静载试验,并通过预先埋设和布置的元件监测了加载过程中的墙顶位移、墙身变形及墙侧岩土抗力。试验过程中最大加载量达到80500kN,为目前世界上最大加载量的水平静载试验。试验结果表明:嵌岩封闭地连墙的荷载位移曲线为缓变型非线性曲线,墙体在加载过程中同时产生水平转动和竖向转动,墙体水平转动主要由现场岩石分布不均匀导致;墙侧岩土压力沿深度先增大后减小,最大土压力位于0.23倍墙深处,墙侧岩土抗力分布受竖向转动的旋转点位置影响较大,试验墙旋转点位于岩层较浅位置处;墙内土体不产生抗力,岩体抗力相较墙外有所折减,墙内中风化花岗岩的岩石抗力约为墙外岩体的0.73倍,墙内微风化花岗岩的岩石抗力约为墙外的0.63倍。

       

      Abstract: Closed diaphragm walls, when used as long-term foundations, demonstrate exceptional lateral bearing capacity. Relying on a specific project in Shenzhen, a lateral static loading test was conducted on rock-socketed enclosed diaphragm walls. The test monitored the displacements at the wall top and lateral geotechnical resistance using pre-installed instruments. During the experiment, the maximum applied load reached 80500 kN, representing the largest lateral static loading test conducted worldwide to date. The experimental results reveal that the load-displacement curve of the rock-socketed closed diaphragm wall exhibits a gradual and nonlinear characteristic. Throughout the loading process, the wall experienced both horizontal and vertical rotations, with horizontal rotation primarily caused by the uneven distribution of rock layers on-site. The lateral geotechnical pressure along the depth showed a trend of initially increasing and subsequently decreasing, with the maximum pressure observed at a depth of 0.28 times the wall depth. The distribution of lateral geotechnical pressure was significantly influenced by the position of the vertical rotation point, which was located in a relatively shallow rock layer. Furthermore, no resistance was provided by the enclosed soil, and the enclosed rock resistance was notably reduced compared to the surrounding rock resistance. Specifically, the enclosed rock resistance of moderately weathered granite was approximately 0.73 times that of the surrounding rock, while the enclosed rock resistance of slightly weathered granite was approximately 0.63 times that of the surrounding rock.

       

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