周创兵, 熊文林. 1996: 论岩体的渗透特性. 工程地质学报, 4(2): 69-74.
    引用本文: 周创兵, 熊文林. 1996: 论岩体的渗透特性. 工程地质学报, 4(2): 69-74.
    Zhou Chuangbin, Xiong Wenlin. 1996: ON PERMEABILITY CHARACTERISTICS OF ROCK MASS. JOURNAL OF ENGINEERING GEOLOGY, 4(2): 69-74.
    Citation: Zhou Chuangbin, Xiong Wenlin. 1996: ON PERMEABILITY CHARACTERISTICS OF ROCK MASS. JOURNAL OF ENGINEERING GEOLOGY, 4(2): 69-74.

    论岩体的渗透特性

    ON PERMEABILITY CHARACTERISTICS OF ROCK MASS

    • 摘要: 从岩体结构的控渗作用出发, 可将岩体的渗流介质划分为多孔介质、准多孔介质、面状流不连续介质及脉状流不连续介质四类;论述了岩体复杂的渗透特性, 包括渗流的不均匀性、各向异性、非饱和性及渗流与变形的耦合等问题。文中还对岩体渗流分析的技术思路进行了讨论。

       

      Abstract: Based on the controlling effect of rock mass structure on the permeability of rock mass, the percolation media of rock mass are divided into four types, i. e. porous,quasi-porous, planar flow discontinuous and vein flow discontinuous media. The complicated permeability of rock mass I involving inhomogeneous, anisotropic. unsaturated behaviour as well as the coupling between hydraulic conductivity and deformation are discussed. The technical routines for the percolation analysis of rock mass are alsohere.

       

    /

    返回文章
    返回