【24h】

STUDY ON TWO DIMENSIONAL SEDIMENT MATHEMATICAL MODEL OF PLANE IN THE LOWER YELLOW RIVER

机译:黄河下游二维平面泥沙数学模型研究

获取原文
获取原文并翻译 | 示例

摘要

Based on the fitting method of boundary coordinate, the solution by dispersion for flow continuity equation and flow motion equation is worked out with ADI method on alternative grids. The solution by dispersion for sediment continuity equation is worked out with the method on control volume. The basic frame of model is set up by the newest research results of sediment continuity equation, bed deformation equation, capacity of sediment-laden flow and bed roughness etc introduced. This model is verified by 1982's flood. It is shown from the results that the process of peak propagation, the process of water level variation and the process of sediment concentration calculated by the model tally with measured results well. The velocity field, flooded depth and range, and sediment concentration field etc are identical with the fact.
机译:在边界坐标拟合的基础上,用ADI方法在替代网格上求解了流动连续性方程和流动运动方程的色散解。利用控制量法,求出了泥沙连续性方程的分散解。该模型的基本框架是通过引入沉积物连续性方程,床变形方程,含沙流量和床糙度等最新研究结果来建立的。 1982年的洪水验证了该模型。结果表明,利用模型计算出的峰值传播过程,水位变化过程和泥沙浓度过程均与实测结果吻合较好。速度场,淹没深度和范围,泥沙浓度场等与事实相同。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号