叶巴滩坝址深部破裂岩体特征及对拱坝稳定的影响

    Development characteristics of deep fracture rock mass of Yebatan high arch dam and its stability influence analysis

    • 摘要: 深部破裂在中国西部深切峡谷地区的岸坡深部岩体内广泛发育,其工程地质特性与发育分布特征对坝基岩体安全稳定具有重要影响。以叶巴滩坝址区岩体内深部破裂为研究对象,通过分析拱坝附近岩体深部破裂发育基本特征与工程地质特性,对深部破裂成因进行探讨。在此基础上,采用投影统计实测法分析了深部破裂发育程度与岩体连通率的相互关系,揭示了深部破裂带位置岩体节理裂隙形成的新潜在滑移面的特征;基于JRC-JCS模型与Mohr-Coulomb强度准则,推导了一种考虑结构面起伏、节理裂隙和岩桥强度参数以及作用在岩体剪切面上的压应力等因素的非贯通性滑面参数取值方法。以2 760 m拱圈高程附近典型中等与强烈深部破裂为例,采用工程地质稳定评价方法与有限元法分析了中等与强烈深部破裂对拱坝稳定的影响。研究表明:深部破裂节理裂隙优势产状方向大致与河流走向一致,其倾角以中陡倾为主,当强烈或中等深部破裂带穿过不稳定块体时,可与构成滑移面的断层等结构面共同形成新的不稳定滑移体;不同类型深部破裂带中节理裂隙对岩体连通率及其岩体力学指标具有显著不同影响;深部破裂对岩体内的应力传递具有削弱或阻隔作用;左岸2 760 m高程抗力体内的强烈与中等深部破裂对该处不稳定体内的局部变形影响较大,建议采用灌浆加固或置换处理。

       

      Abstract: Deep fracture is widely developed in deep rock mass of bank slopes in the deep canyon areas of western China, its engineering geological characteristics and development distribution have an important influence on the safety and stability of dam foundation rock mass.Taking the deep fracture of rock mass in the Yebatan arch dam site as the research object, we discuss causes of deep fracture by analyzing the basic characteristics of deep fracture development and engineering geological characteristics of rock mass near the arch dam.On this basis, the relationship between the development degree of deep fracture and connectivity rate of rock mass is analyzed by using the projection statistical measurement method, and the characteristics of new potential slip plane produced by rock mass joint fissure at the deep fracture zone are revealed.Based on the JRC-JCS model and the Mohr-Coulomb strength criterion, a parameter value determining method of non-penetrating sliding surface is derived, which takes into account the feature of structural plane, the strength parameters of joint fissure and rock bridge, and the compressive stress acting on the shear plane of rock mass.Finally, the typical moderate and strong deep fractures near2760m arch circle elevation are taken as an example.The influence of moderate and strong deep fractures on the stability of Yebatan arch dam is analyzed by using engineering geological stability evaluation method and finite element method.The results show that the dominant direction of deep fracture joint is roughly the same as the river trend, and its dip angle is mainly medium and steep.When the strong or medium deep fracture zone passes through unstable blocks, it can form new unstable slip body together with the structural planes such as the fault forming and sliding planes.Joint fissures in deep fracture zones with different degrees of development have significantly different effects on connectivity and mechanical indexes of rock mass.Deep fracture can weaken or block the stress transfer in rock mass.The strong and medium deep fractures in the left bank2760m elevation resistance abutment has a great influence on local deformation of the unstable body, so it is recommended to adopt grouting reinforcement or replacement treatment.

       

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