首页 | 本学科首页   官方微博 | 高级检索  
     

平面二维水流泥沙数学模型有限元分析
引用本文:张云鹏,黄久林.平面二维水流泥沙数学模型有限元分析[J].山东大学学报(工学版),2002,32(4):342-345.
作者姓名:张云鹏  黄久林
作者单位:250061,山东省,济南市山东大学土建与水利学院
摘    要:建立了水流泥沙平面二维数学模型 讨论了动边界处理方法及定解条件 在利用有限元方法建立了离散的常微分方程组后 ,采用了选择系数质量矩阵集中法求解 ,从而避免了大量方程组的联解 ,极大限度地节省了计算存贮量 ,缩短了计算时间 通过实例验证 ,该模型适用于短河段、沉沙区、放淤区、引航道及边界条件较复杂的水工建筑物附近动床河段的冲淤数值模拟 ,并有较高精度

关 键 词:河床  河道淤积  有限元分析
文章编号:1000-5323(2002)04-0342-04
修稿时间:2002年4月10日

FINITE ELEMENT METHOD FOR TWO-DIMENSIONAL MATHEM ATIC MODEL IN RIVER FLOW AND SEDIMENT TRANSPORT
ZHANG Yun peng,HUANG Jiu lin.FINITE ELEMENT METHOD FOR TWO-DIMENSIONAL MATHEM ATIC MODEL IN RIVER FLOW AND SEDIMENT TRANSPORT[J].Journal of Shandong University of Technology,2002,32(4):342-345.
Authors:ZHANG Yun peng  HUANG Jiu lin
Abstract:A two dimensional model in horizontal planes for the river flow and sediment transport is presented. The methods dealing with movable boundary and the conditions determining the answer are discussed. In order to adapt the complicated topography and boundary condition, the finite element method in numerical simulation is adopted. Appling the "Selective Lumping Scheme", a procedure to solve an algebraic simultaneous equation system can be avoided. It makes the storage reduced extremely. This mathematic model can be used in short reach, sedimentary region, approach channel, and the adjacent area of hydraulic structures that have complicated boundary conditions. The calculating results agree experimental values reasonably well.
Keywords:River beds  River channel sedimentation  Finite element analysis
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号