丁桂伶, 王连俊, 刘升传. 2007: 齐岳山隧道岩溶发育特征与破坏区范围内安全深度的预测. 工程地质学报, 15(S1): 333-337.
    引用本文: 丁桂伶, 王连俊, 刘升传. 2007: 齐岳山隧道岩溶发育特征与破坏区范围内安全深度的预测. 工程地质学报, 15(S1): 333-337.
    DING Guiling, WANG Lianjun, LIU Shengchuan. 2007: CHARACTERISTICS OF KARST DEVELOPMENT IN QIYUESHAN TUNNEL AND SAFETY DEPTH PREDICTION IN DAMAGED AREA. JOURNAL OF ENGINEERING GEOLOGY, 15(S1): 333-337.
    Citation: DING Guiling, WANG Lianjun, LIU Shengchuan. 2007: CHARACTERISTICS OF KARST DEVELOPMENT IN QIYUESHAN TUNNEL AND SAFETY DEPTH PREDICTION IN DAMAGED AREA. JOURNAL OF ENGINEERING GEOLOGY, 15(S1): 333-337.

    齐岳山隧道岩溶发育特征与破坏区范围内安全深度的预测

    CHARACTERISTICS OF KARST DEVELOPMENT IN QIYUESHAN TUNNEL AND SAFETY DEPTH PREDICTION IN DAMAGED AREA

    • 摘要: 本文首先介绍了齐岳山隧道构造岩溶地貌的基本情况及其地貌类型分类,本区地表岩溶溶洞分布具有多层性,规模不等,形态多样;其次介绍了得胜场槽谷岩溶洞穴系统的特点,包括太平洞和五同庙凉风洞的发育条件和发育特征,并给出了得胜场槽谷的岩溶发育的垂向分带特征,在竖向上体现出自地表向下的垂直分带性,依次可分为:岩溶强烈发育带、岩溶中等发育带、岩溶弱发育带。然后,文中详细分析了测区岩溶发育规律,包括岩溶沿顺层发育特征、沿构造裂隙发育特征、沿断层发育特征及溶崩角砾岩岩溶较不发育;最后应用有限元方法对在一定破坏区范围内的安全深度进行了预测,认为安全深度应该在距地面22.25m以下。

       

      Abstract: Firstly, the basic information and physiognomy style of Karst Physiognomy of QiYueshan tunnel are introduced in this paper. There are multilayers in the surface karst cave of this area which have different scales and shapes. Secondly, it describes the characteristic of karst cave system of Deshengchang trough valley,including the development characteristics and conditions of Taiping cave and Wutongmiao cave. It also introduces the vertical zoning characteristics of karst cave system of Deshengchang trough valley including karst strongly developed strip, karst middling developed strip and karst weakly developed strip. Then the karst development rules of the area are introduced including karst development characteristics in the same direction, cranny and faultage area. At last the safety depth in given damaged area is predicted through FE method and the result is considered to be beneath 22.25m.

       

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