梁晓丹, 赵坚, 宋宏伟. 2012: 围岩自调节成拱特性的实验与数值分析. 工程地质学报, 20(1): 96-102.
    引用本文: 梁晓丹, 赵坚, 宋宏伟. 2012: 围岩自调节成拱特性的实验与数值分析. 工程地质学报, 20(1): 96-102.
    LIANG Xiaodan, ZHAO Jian, SONG Hongwei. 2012: EXPERIMENTAL AND NUMERICAL ANALYSIS ON THE ARCHING ACTION FROM STRESS ADJUSTING IN SURROUNDING ROCKS. JOURNAL OF ENGINEERING GEOLOGY, 20(1): 96-102.
    Citation: LIANG Xiaodan, ZHAO Jian, SONG Hongwei. 2012: EXPERIMENTAL AND NUMERICAL ANALYSIS ON THE ARCHING ACTION FROM STRESS ADJUSTING IN SURROUNDING ROCKS. JOURNAL OF ENGINEERING GEOLOGY, 20(1): 96-102.

    围岩自调节成拱特性的实验与数值分析

    EXPERIMENTAL AND NUMERICAL ANALYSIS ON THE ARCHING ACTION FROM STRESS ADJUSTING IN SURROUNDING ROCKS

    • 摘要: 本文在围岩应力分析的基础上,通过物理实验模拟和数值计算,分析了由于隧道开挖后应力变化引起的围岩自调节成拱的特性及相关影响因素作用下的压力拱成拱规律。在本文中,将压力拱内边界距洞口的距离和拱体厚度作为判定压力拱成拱和评价围岩稳定的参数。当内边界靠近隧道洞口,围岩基本稳定; 压力拱的厚度小意味着需要较少的岩体来承担拱体自身和其上岩体的荷载。在此基础上,运用平面应变相似模拟实验模拟隧道开挖过程,对开挖过程中洞口周围应力升高区进行了观察和分析,明确了压力拱的成拱,以及随着距离洞口越近变形增加的幅度越大等现象。运用数值分析发现,随着节理的间距的减小,压力拱内边界靠近洞口,压力拱厚度增大; 在2组节理围岩中,节理倾角分别为30和60时,成拱最不利; 而节理的黏结强度对压力拱成拱的影响程度与节理摩擦角的大小相关联,摩擦角大于20时,节理黏结强度对压力拱成拱影响甚微。

       

      Abstract: In this paper,after the stress analysis of surrounding rocks,excavation simulated experiments and numerical calculation are applied to study the characteristics of arching action under conditions of different rock properties.Firstly,inner boundary and thickness are used to define an arch in surrounding rocks and to evaluate the stability of underground openings.When the inner boundary is near openings,the surrounding rocks are stable.The thickness of arching action indicates the extent to which the surrounding rocks are influenced by excavation.Less thickness means fewer rocks are used to sustain their own weight and that of rocks above.Then,the arching action is defined in the excavation simulated experiment.In this experiment,it is observed and analyzed that the increase of tangential stresses occurs and an arch is formed around an opening.Data from the experiment show that the increase of displacements is greater near the opening.In numerical analysis,it is found that joints have great influence on the formation of an arch.The position of inner boundary of pressure arch is far away from an opening and thickness is greater with the decrease of joint space.And,in rock mass containing two sets of joint,when a joint incline angle is 30 degree or 60 degree respectively,it is disadvantageous for an arch formation.In addition,the influence degree of joint cohesion on arching action is related to joint friction angle.When the joint friction angle is more than 20 degree,the joint cohesion influence is negligible.

       

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