| 论岩体的渗透特性 |
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| 引用本文： | 周创兵,熊文林.论岩体的渗透特性[J].力学学报,1996,4(2):69-74. |
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| 作者姓名： | 周创兵 熊文林 |
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| 作者单位： | 武汉水利电力大学,武汉430072 |
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| 基金项目： | 国家八·五攻关项目,国家自然科学基金 |
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| 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。
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| 关 键 词： | 岩体 渗流介质 渗透特性 |
| 收稿时间： | 1996-01-08 |
ON PERMEABILITY CHARACTERISTICS OF ROCK MASS |
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| Zhou Chuangbin,Xiong Wenlin.ON PERMEABILITY CHARACTERISTICS OF ROCK MASS[J].chinese journal of theoretical and applied mechanics,1996,4(2):69-74. |
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| Authors: | Zhou Chuangbin Xiong Wenlin |
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| Institution: | Wuhan University of Hydrualic and Electric Engineering, Wuhan 430072 |
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| 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. |
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| Keywords: | Rock mass Percolation media Permeability |
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