Ground Stress Characteristics of Underground Caverns in Yebatan Hydropower Station

ce/papers Pub Date : 2025-03-18 DOI:10.1002/cepa.3152
Chong Zhang, Jianhua He, Xiuli Ding, Shuling Huang, Peiyang Yu
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Abstract

Ground stress is the primary load acting on the support structures of large underground engineering projects, directly affecting the stability of the cavern's surrounding rock. Therefore, determining the characteristics of ground stress is the main issue to be resolved in the design of underground engineering. To investigate the ground stress characteristics of underground caverns in Yebatan hydropower station, the aperture deforming method is adopted to measure the ground stress. The results show that the magnitude of maximum principal stress (i.e. σ1) is 16.51 - 37.57 MPa. And its orientation ranges from N82°E to N54°W, which is close to the direction of the regional tectonic principal compressive stress. Meanwhile, ground stress field of underground caverns is mainly horizontal tectonic stress. Furthermore, the formation of disk-shaped rock cores can be found in the drilling holes of PD08 exploratory adit, indicating that the underground caverns are located in high ground stress area. Finally, the location of spalling is concentrated in upstream spandrel, providing significant validation for the ground stress characteristics within the underground caverns of Yebatan hydropower station.

叶巴滩水电站地下洞室地应力特征
地应力是作用在大型地下工程支护结构上的主要荷载,直接影响到洞室围岩的稳定性。因此,地应力特征的确定是地下工程设计中需要解决的主要问题。为研究叶八滩水电站地下洞室地应力特征,采用孔径变形法对洞室地应力进行测量。结果表明:最大主应力(σ1)为16.51 ~ 37.57 MPa;其方位在N82°E ~ N54°W之间,接近区域构造主压应力方向。地下洞室地应力场以水平构造应力场为主。此外,在PD08勘探坑道钻孔中发现盘状岩心的形成,表明地下洞室位于高地应力区。最后,剥落位置集中在上游拱肩,为叶巴滩水电站地下洞室地应力特征提供了重要的验证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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