黄润秋, 肖华波. 2008: 浅埋双连拱隧道围岩边坡体系变形机理及稳定性分析. 工程地质学报, 16(5): 584-591.
    引用本文: 黄润秋, 肖华波. 2008: 浅埋双连拱隧道围岩边坡体系变形机理及稳定性分析. 工程地质学报, 16(5): 584-591.
    HUANG Runqiu, XIAO Huabo. 2008: DEFORMATION MECHANISM AND STABILITY STUDY ON SYSTEM OF SURROUNDING ROCK AND SLOPE OF SHALLOW DOUBLE - ARCH TUNNEL. JOURNAL OF ENGINEERING GEOLOGY, 16(5): 584-591.
    Citation: HUANG Runqiu, XIAO Huabo. 2008: DEFORMATION MECHANISM AND STABILITY STUDY ON SYSTEM OF SURROUNDING ROCK AND SLOPE OF SHALLOW DOUBLE - ARCH TUNNEL. JOURNAL OF ENGINEERING GEOLOGY, 16(5): 584-591.

    浅埋双连拱隧道围岩边坡体系变形机理及稳定性分析

    DEFORMATION MECHANISM AND STABILITY STUDY ON SYSTEM OF SURROUNDING ROCK AND SLOPE OF SHALLOW DOUBLE - ARCH TUNNEL

    • 摘要: 双连拱隧道是一种新的隧道形式, 由于其整体跨度大、结构复杂、施工工序繁琐, 在地形偏压、地质条件复杂的情况下修建双连拱隧道难度较高, 尤其在洞口段容易出现衬砌开裂、边坡变形等一系列工程问题。结合安徽铜黄高速公路汤屯段富溪隧道进口段工程, 采用地质条件研究与数值模拟分析相结合的研究手段, 对复杂地质条件下偏压双连拱隧道围岩① 边坡体系在施工过程中应力应变发展过程进行了研究。综合分析表明, 富溪隧道进口段处于F5断层影响带内, 岩体呈碎裂结构,同时, 受到地形偏压影响, 隧道开挖后衬砌和围岩表现为沉降变形和侧向变形, 进口边坡在隧道围岩变形的诱导下, 表现为蠕滑- 拉裂变形破裂。根据以上研究成果, 提出了富溪隧道变形治理应以控制进口段隧道拱顶的变形为主。

       

      Abstract: Double- arch tunnel is a k ind o f new tunnel form. It has a large span, complica ted structure and cock amam iew orking procedure. Therefore, it is difficult to be constructed under unsymmetrical pressure and comp lex geo log ical cond itions. E specially, a series of eng ineering problems, such as lin ing crack ing and tunne l slope de fo rmation, o ften occur in the entrance po rtal reg ion. Th is paper is based on the pro ject of Fux i tunnel and uses both geo log ical analysis and numerical simulation method. The stress- stra in processes of lining and rock mass are ex am ined systemat ically during the construction of the double- arch tunnel under unsymme trical pressure and com plex geological cond it ions. The comprehensive ana lysis show s that ow ing to the in fluence of theF5 fau l,t fragmenta l structure rockmass w as encountered in the portal reg ion. Due to poor rockmass and unsymmetrical pressure, lining and surrounding rock occurred settlem ent and lateral deform ation after tunne l excavat ion. The slope deformation mode w as creep sliding- fracturing wh ich w as is a result from surround ing rock deformat ion. Based on the above analysis, a conclusion w as drawn that control of the tunnel vau lt deformat ion is a key step to contro l the who le de fo rmation o f the entrance reg ion.

       

    /

    返回文章
    返回