基于一维盐度模型的珠江河网咸潮上溯距离分析
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Saltwater intrusion lengths in the Pearl River networks based on one-dimension salinity model
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    摘要:

    建立珠江三角洲河网整体一维水动力、盐度数值计算模型,此模型涵盖了整个珠江三角洲河网区,验证结果良好。在此模型基础上,对2001年枯季和2005年枯季珠江三角洲咸潮上溯情况进行模拟计算,模拟结果表明,0.5‰盐度线在整个河网区域呈现出向右倾斜的“S”形,2005年枯季咸潮平均上溯距离达到了32.4 km,这几乎是2001年枯季的2倍。进一步利用模型模拟4种不同来水情况下的咸潮上溯距离的变化情况,对4种来水流量下的咸潮上溯距离进行分析,发现当上游来水平均流量减少将近0.5倍时,下游8大口门处咸潮上溯平均距离将增加1倍左右。

    Abstract:

    A one-dimension hydrodynamic-salinity mathematical calculation model of the Pearl River networks is established.This model covers the entire river region,and it is verified with good results.Based on this model,analysis of the characteristics of saltwater intrusion in the Pearl River Delta in dry seasons of 2001 and 2005 has been carried out.The result indicates that the simulated 0.5 parts per thousand salinity isohaline in the Pearl River networks displays a shape similar to “S” and slanting to the right.The saltwater intrusion lengths of 2005 intruded far upstream at an average length of 32.4 km,which is almost twice longer than that in 2001.Four representative upstream flows are also simulated to analysis the response of the saltwater intrusion lengths to discharges.The result implies that when upstream average flows reduce by 0.5 times,saltwater intrusion lengths at the eight outlets increase by nearly 1 time.

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官明开,蒋齐嘉,徐龑文,等.基于一维盐度模型的珠江河网咸潮上溯距离分析[J].水运工程,2016(11):66-71.

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  • 在线发布日期: 2016-11-17
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