RESEARCH ON TRANSFUSION STRESS COUPLING MECHANISM OF CREVASSE ROCK MASS
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摘要: 隧洞开挖前,岩体中的地下水与围岩应力处于一种相对平衡状态,由于隧洞的开挖,一方面使地下水排泄有了新的通道,加速了水循环,破坏了原有的补给运移排泄系统的平衡;另一方面,造成围岩应力重分布,部分结构面由于增压而闭合,部分岩体卸荷松弛或产生剪切滑移,人为破坏了原有的地下水渗流条件,使得隧洞自身成为地下水向外排泄的地下廊道,导致突水灾害。采用Monte-Carlo方法建立二维离散裂隙网络,并将其导入UDEC软件中的岩体结构离散裂隙网络介质模型(DFN),依据此模型,采用离散单元法对裂隙岩体渗流特性、裂隙岩体洞室开挖力学特性以及裂隙岩体渗流应力耦合机制进行研究。结合具体实例,对不考虑水力耦合和考虑水力耦合情况下在裂隙岩体中开挖洞室的洞周围岩的力学特性做了对比。Abstract: Before a tunnel excavation, the groundwater in the rock and the surrounding rock stress are in a state of relative balance, because the excavation makes tunnel groundwater drain has a new channel, thus accelerating the water cycle, which destroyed balance of the original supplies-migration-the drainage system;On the other hand, the surrounding rock stress was redistributed and part of structural surface was closed due to pressurization, part of unloading rock mass produced shear slippage, which vandalized the original groundwater seepage condition, thus making tunnel itself become an underground corridor to discharge water in different forms, resulting in bursting water disasters.Monte Carlo method was used to establish 2-d discrete-fracture network, which was input rock mass structure discrete fissure network medium model(DFN), according to the model of the discrete element method in fractured rock mass seepage characteristics, fracture rock cavern excavation mechanical characteristics and seepage stress coupling mechanism of fractured rock mass.Combined with concrete examples, a comparison was done for cases of excavating caverns in fractured rocks with and without consideration of hydraulic coupling.
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Key words:
- the crevasse rock mass /
- seepage field /
- stress field /
- coupling
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[2] Esaki J. Shear-Flow Coupling Test on Rock Joints[C]//Proc .7 th?Int . Conf. ISRM:1992. Tsang Y W, Witherspoon P A. Hydromechnical Behavior of a?Deformable Rock Fracture Subject to Normal Stress[J]. J. Geophys?Researd.1981,86(B10):9187-9198. [3] 耿克勤.岩体裂隙渗流水力特性的实验研究[J].清华大学学报,1996,36(1):102-106. [4] 件彦卿,张倬元.岩体水力学导论[M].成都:西南交通大学出版社,1995. [5] Ohnishi U, Ohtsu H. Coupled Stress Flow Analysis of?Discontinuous Media by Finite Elements[J]. Proc Jpn Soc Civ?Eng,1982,322:111-120. [6] 王媛,徐志英,速宝玉.裂隙岩体渗流与应力耦合分析的四自由度全耦合法[J].水利学报,1998(7):55-59. [7] 朱珍德,徐卫亚.裂隙岩体渗流场与损伤场耦合模型研究[J].河海大学学报:自然科学版,2003,31(2):156-160.
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