【摘要】 岩体裂隙面是粗糙不平的,具有分形特征。裂隙本身可以看成由上下两裂隙面叠合而成的,可以应用分形几何理论来模拟粗糙裂隙面和裂隙张开度的分布情况。在用分形理论模拟裂隙面及裂隙张开度的基础上,用特征有限元方法对粗糙裂隙中的溶质运移进行了模拟。模拟结果显示,考虑裂隙面的粗糙度,模拟其中的溶质运移更符合实际情况。与平均张开度下光滑裂隙中的溶质运移相比,粗糙裂隙中的浓度锋面更落后,而且存在不均匀性和各向异性的特点。更多还原

【Abstract】 Rough fracture surface is of characteristics of fractal and can be considered as congruence of the upper and lower fracture surfaces. The rough fracture surface and the distribution of fracture apertures can be simulated by fractal theory. The simulation is made on solute transport in rough fractures by characteristic FEM based on the fracture face and fracture apertures simulated by using fractal theory. The result of simulation shows that it is more actual to simulate solute transport in fractures with its roughness considered. In contrast with the solute transport in smooth fractures with average aperture,the frontal surface of concentration in a rough fracture is more behindhand and is of characteristics of nonuniformity and anisotropy.更多还原