Abstract
In deep hard rock excavation,stress plays a pivotal role in inducing stress-controlled failure.While the impact of excavation-induced stress disturbance on rock failure and tunnel stability has undergone com-prehensive examination through laboratory tests and numerical simulations,its validation through in-situ stress tests remains unexplored.This study analyzes the three-dimensional stress changes in the sur-rounding rock at various depths,monitored during the excavation of B2 Lab in China Jinping Underground Laboratory Phase Ⅱ(CJPL-Ⅱ).The investigation delves into the three-dimensional stress variation characteristics in deep hard rock,encompassing stress components and principal stress.The results indicate changes in both the magnitude and direction of the principal stress during tunnel exca-vation.To quantitatively describe the degree of stress disturbance,a series of stress evaluation indexes are established based on the distances between stress tensors,including the stress disturbance index(SDI),the principal stress magnitude disturbance index(SDIm),and the principal stress direction distur-bance index(SDId).The SDI indicates the greatest stress disturbance in the surrounding rock is 4.5 m from the tunnel wall in B2 Lab.SDIm shows that the principal stress magnitude disturbance peaks at 2.5 m from the tunnel wall.SDId reveals that the largest change in principal stress direction does not nec-essarily occur near the tunnel wall but at a specific depth from it.The established relationship between SDI and the depth of the excavation damaged zone(EDZ)can serve as a criterion for determining the depth of the EDZ in deep hard rock engineering.Additionally,it provides a reference for future construc-tion and support considerations.
基金项目
国家自然科学基金(42202320)
国家自然科学基金(42102266)
Open Project of Engineering Research Center of Phosphorus Resources Development and Utilization of Ministry of Education(LKF201901)
Yalong River Hydropower Development Co.,Ltd()
万方数据