Finite element and distinct element analysis of the stability of a large underground hydropower machine hall in the Himalayas

被引:9
|
作者
Bhasin, Rajinder [1 ]
Pabst, Thomas [1 ]
机构
[1] Norwegian Geotech Inst, N-0806 Oslo, Norway
关键词
rock support system; Q-system; high stress; UDEC; phase; JOINTED ROCK;
D O I
10.1007/s12205-013-1351-4
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Numerical simulations have been performed to assess the stability of a large underground powerhouse in the Himalayas, using both finite element and distinct element approaches. Large convergences (around 250-300 mm) along the 45 m high wall of the Machine Hall have been measured by total station measurements during construction and up to 60 mm in the post construction and operational phase. Displacements are continuing at a reduced rate of about 3 to 6 mm per year. A large number of rock bolts have failed in the powerhouse and the shotcrete liner presents cracks and failure marks, thus questioning the long-term integrity and stability of the existing rock support system. The purpose of the numerical analysis was to back-calculate the prevailing rock mass conditions surrounding the machine hall, thereby gaining a better understanding of the mechanisms responsible for the instability in the cavern. The results from the analysis indicate that there was possibly an underestimation of the rock support requirements needed for the cavern, coupled with a not so good installation (incomplete grouting of the bolts). Both the length and the capacity of the rock bolts were underestimated presumably due to the existence of a high stress regime in the area, which may not have been taken into consideration in the design of rock support. The effect of a possible earthquake, frequent in this area, has also been studied and proves to induce a significant increase of the displacements and the support failure.
引用
收藏
页码:725 / 732
页数:8
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