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三门峡库区一维非恒定非均匀泥沙输移数学模型
引用本文:陈前海,方红卫,王光谦.三门峡库区一维非恒定非均匀泥沙输移数学模型[J].水科学进展,2004,15(2):160-164.
作者姓名:陈前海  方红卫  王光谦
作者单位:清华大学水利水电工程系, 北京, 100084
基金项目:国家重点基础研究发展规划(973)资助项目(G1999043607)~~
摘    要:黄河是高含沙河流,含沙量季节差异显著。因此研究黄河干流的非恒定水沙输移规律以及库区泥沙的淤积问题极为重要。应用圣维南方程组以及非恒定泥沙连续方程建立了非恒定非均匀泥沙含沙量计算公式,并根据沙量平衡方程推求出三门峡库区河底高程的变化规律。使用已有的资料对模型进行的验证表明:模型计算与实测资料符合良好,该模型具有较好的应用前景。

关 键 词:非恒定流    非均匀输沙    数学模型    三门峡库区    黄河
文章编号:1001-6791(2004)02-0160-05
收稿时间:2002-12-26
修稿时间:2002年12月26

1-D numerical simulation of unsteady flow and non-uniform sediment transport at the Sanmenxia reservoir in the Yellow River
CHEN Qian-hai,FANG Hong-wei,WANG Guang-qian.1-D numerical simulation of unsteady flow and non-uniform sediment transport at the Sanmenxia reservoir in the Yellow River[J].Advances in Water Science,2004,15(2):160-164.
Authors:CHEN Qian-hai  FANG Hong-wei  WANG Guang-qian
Affiliation:Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China
Abstract:Flow in the Yellow River carries sediment in high concentration, and most of sediment transport occurs during the summer time. As the result the calculation of unsteady sediment transport is one of the most important tasks in the Yellow River. This paper presents the unsteady sediment concentration formula accounted for realistically in a model that has predictive power. Applications of the model to Sanmenxia reservoir are shown and compared with field measurement whenever possible.
Keywords:unsteady flow  non-uniform sediment transport  mathematical model  Sanmenxia reservoir  Yellow River
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