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均质各向异性土层中轴对称渗流问题的分析
引用本文:吴世余,李宏. 均质各向异性土层中轴对称渗流问题的分析[J]. 岩土工程学报, 2008, 30(4): 581-583
作者姓名:吴世余  李宏
作者单位:安徽省水利部淮河水利委员会水利科学研究院;安徽省水利部淮河水利委员会水利科学研究院 安徽蚌埠233000;安徽蚌埠233000;
摘    要:对于均质各向异性土层中的轴对称渗流问题,也同平面问题一样,可取缩放渗流场比尺的方法解题,但其结果不同于平面问题。按研究结果:如缩小径向尺度,则缩小后渗流场的等效渗透系数为横向渗透系数kh;如放大轴向尺度,则放大后渗流场的等效渗透系数为平均渗透系数√khkv。

关 键 词:各向异性  轴对称  渗流  
文章编号:1000-4548(2008)04-0581-03
修稿时间:2007-07-20

Analysis for axisymmetric seepage flows in homogeneous and anisotropic strata
WU Shi-yu,LI Hong. Analysis for axisymmetric seepage flows in homogeneous and anisotropic strata[J]. Chinese Journal of Geotechnical Engineering, 2008, 30(4): 581-583
Authors:WU Shi-yu  LI Hong
Affiliation:Anhui and River Water Resources Research Institute 233000 China
Abstract:The axisymmetric flows in anisotropic porous medium could be solved by the same method used in plan flows,that was,reducing the horizontal dimension or enlarging the vertical dimension of the field.But the results were different from those of the plan problems.According to the research results,if the radial dimension was reduced,the equivalent permeability coefficient of the reduced field was the horizontal permeability coefficient kh;and if the axial dimension was enlarged,the equivalent permeability coefficient of enlarged field was the mean permeability coefficient √kh kv.
Keywords:anisotropy  axial symmetry  seepage flow
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