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基于最小可用能耗率原理的河流水沙数学模型
引用本文:陈绪坚,胡春宏.基于最小可用能耗率原理的河流水沙数学模型[J].水利学报,2004,35(8):0038-0045.
作者姓名:陈绪坚  胡春宏
作者单位:中国水利水电科学研究院,泥沙研究所,北京,100044
基金项目:国家自然科学基金重点项目(50239040),水利部创新项目(SCX2003 01)
摘    要:本文把河流视为具有能量紊动黏性热耗散结构的开放系统,根据耗散结构的熵和能耗理论,提出了保持冲积河流稳定的最小可用能耗率原理和公式。该原理全面地反映了河道输水输沙的能耗特性,在数学上完整地表达了冲积河流河床演变的基本原理——自动调整作用原理。应用该原理的公式封闭河床演变方程组,建立了冲积河流河道输水输沙优化的数学模型,根据该模型的计算结果分析了黄河下游河道输水输沙的规律,并解释了河床演变的各种现象。应用该模型计算了黄河下游各河段输水输沙优化的临界指标,并提出了有利于改善小浪底水库调水调沙运用的建议,为小浪底水库调水调沙提供参考。

关 键 词:河床演变  熵和能耗  最小可用能耗率原理  数学模型  输水输沙优化  黄河下游
文章编号:0559-9350(2004)08-0038-08
修稿时间:2004年4月9日

Mathematical model for flow and sediment in alluvial river based on minimum rate of available energy dissipation principle
CHEN Xu-jian.Mathematical model for flow and sediment in alluvial river based on minimum rate of available energy dissipation principle[J].Journal of Hydraulic Engineering,2004,35(8):0038-0045.
Authors:CHEN Xu-jian
Affiliation:China Institute of Water Resources and Hydropower Research, Beijing 100044, China
Abstract:The river is regarded as an open system with structure of thermal energy dissipation due to turbulence and viscosity. On this basis, the theory of dissipation structure is applied to deduce the principle of minimum rate of available energy dissipation for maintaining the stability of the alluvial river. According to this principle, the energy dissipation characteristics of flow and sediment transport can be comprehensively described and the basic principle of riverbed evolution i.e. automatic regulation principle is fully expressed. The formula deduced is applied to close the equations describing the evolution of riverbed and establish the mathematical model expressing the optimized transport of water and sediment in alluvial river. The model is applied to calculate the critical indexes of optimized transport of water and sediment in the lower reaches of Yellow River and a recommendation on improving the dispatch of water and sediment in Xiaolangdi Reservoir is suggested accordingly.
Keywords:riverbed evolution  entropy and energy dissipation  minimum rate of available energy dissipation  mathematical model  optimized transport of water and sediment  lower reaches of Yellow River
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