基于非连续裂隙介质网络流的线素法模型研究
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Research of the line element method model based on discontinuous fracture media network flow
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    摘要:

    为了准确描述出基岩裂隙网络流的流场状态,基于非连续裂隙介质渗流理论,以流体力学为基础,把裂隙的交叉点作为节点,节点之间的裂隙作为线元,各线元流向共同节点的流量等于贮存的变化量。依次建立各节点的渗流方程式,构建地下水裂隙介质网络流的渗流模型。利用该方法对模拟区域进行计算并与经典数值解法的计算结果进行对比,结果表明线素法模型能够准确的表征出裂隙含水介质的构造特征,并能够准确反映出地下水的实际流动方向。

    Abstract:

    In order to accurately describe the rock fracture network flow field condition,the fracture of the intersection was taken as a node and the node between the fracture line was taken as line element by basing on the discontinuous fracture media seepage theory and fluid mechanics; the line element flow to the common node of each wire flow amount was equal to the change in storage. And then the seepage equations were established and the groundwater seepage flow model of fracture network flow media was built. And the simulation domain was calculated by using this method,and then the results with the classical numerical method were compared. The results show that the line element method model can accurately characterize the structural characteristics of fractured aqueous medium,and which is able to accurately reflect the actual groundwater flow direction.

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李树文,高轲,王若男.基于非连续裂隙介质网络流的线素法模型研究[J].河北工程大学自然版,2013,30(4):73-77

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  • 收稿日期:2013-05-27
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  • 在线发布日期: 2015-01-12
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