摘要
对等效离散的机制进行了理论分析，通过水槽试验和对珠江典型河段的天然观测，说明潮流断面平均流速和平均浓度相对于潮平均值的波动是引起等效离散的主要原因，提出了计算等效离散系数的实用方法，并对负离散问题进行了讨论。
The mechanism of equivalent dispersion is analyzed in this paper. Based on experimental study and observational results of typical reach in the Pearl River, it is expressed that the fluctuations between sectional averaged values and tidal averaged value of velocity and concentration are the main reason which causes equivalent dispersion. The practical calculation method of equivalent dispersion coefficient is developed and the phenomenon of negative dispersion is discussed.
出处
《清华大学学报（自然科学版）》
EI
CAS
CSCD
北大核心
1997年第11期57-60,共4页
Journal of Tsinghua University(Science and Technology)
基金
国家自然科学基金
关键词
潮汐流动
等效离散
计算方法
珠江
水污染
tidal flow
equivalent dispersion
calculation method
negative dispersion
the Pearl River.
