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广州水道咸潮影响因素分析
引用本文:莫思平,李越,卢素兰.广州水道咸潮影响因素分析[J].水利水运工程学报,2007,0(4):36-42.
作者姓名:莫思平  李越  卢素兰
作者单位:1. 南京水利科学研究院,水文水资源与水利工程科学国家重点实验室,江苏,南京,210029
2. 珠江水利科学研究院,广东,广州,510610
摘    要:根据实测资料分析了广州水道的成潮变化规律及其主要影响因素.根据盐度数学模型计算了地形、海平面、风况和流量分配方式4种因素对咸潮的影响程度,结果表明,年内流量分配方式对成界的影响最明显,其次是地形和风况的变化,海平面抬升对成潮影响相对较小.

关 键 词:咸潮    地形    海平面抬升    风况    径流    盐度数学模型    广州水道
文章编号:1009-640X(2007)04-0036-07
收稿时间:2007-05-08
修稿时间:2007年5月8日

Analysis of factors affecting saline water intrusion in Guangzhou waterway
MO Si-ping,LI Yue,LU Su-lan.Analysis of factors affecting saline water intrusion in Guangzhou waterway[J].Hydro-Science and Engineering,2007,0(4):36-42.
Authors:MO Si-ping  LI Yue  LU Su-lan
Abstract:Based on field data, this paper analyzes the impact of saline water intrusion on Guangzhou waterway and identifies the dominant factors determining the variation of saline water tide. Furthermore, by the use of salinity mathematical model, the degree of effects of four factors, i. e. , terrain, sea level, wind regime and flow rate distribution on saline water tide variation, is presented respectively. Among these factors, flow rate distribution has significant effects on the saline water boundary, terrain and wind regime have less significant effects on it, and the sea level can affect the saline water tide weakly.
Keywords:saline water intrusion  terrain  sea level  wind regime  runoff  salinity mathematical model  Guangzhou waterway
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