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天然河道水沙平面二维数学模型研究
引用本文:李永强 陈红中. 天然河道水沙平面二维数学模型研究[J]. 华北水利水电学院学报, 1999, 20(1): 10-13
作者姓名:李永强 陈红中
作者单位:[1]河南黄河勘测设计研究院 [2]郑州水利学校
摘    要:针对天然河道中常出现水位随流量变化并导致流动区域发生变化的这种现象,利用ADI(AlternatingDirectionImplicitMethod)法,融入迎风有限差分格式离散基本方程,利用迭代法求解差分方程组,并采用大清河实测水文资料,对模型进行了验证.证明了该模型能成功地求解出天然河道平面流场的形态以及河道的冲淤状况.

关 键 词:二维;数学模型;迭代;ADI

The study and the application of two-dimension water flow and sediment mathematical model in the river
LI Yong-qiang ,CHEN Hong-zhong ,SHI Shou-liang. The study and the application of two-dimension water flow and sediment mathematical model in the river[J]. Journal of North China Institute of Water Conservancy and Hydroelectric Power, 1999, 20(1): 10-13
Authors:LI Yong-qiang   CHEN Hong-zhong   SHI Shou-liang
Affiliation:LI Yong-qiang 1,CHEN Hong-zhong 2,SHI Shou-liang 3
Abstract:The flow guautity vaviation leads to the change of water level in the river. so the area that water covers too. The condition the authors utilize the method of ADI(Alternating Direction Implicit Method)and finite difference to solve the basic equation. The mathematical model is verified by the hydrology test data of Daqinghe in Hebei province.The status of the fluid and the erosion or silt in the river are solved by the above methe matical model.
Keywords:two-dimension  mathematical model  iterative method  ADI(Alternating Direction Implicit Method)  
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