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珠江口门枯季动力过程及盐度分布特征
引用本文:范中亚,林澍,曾凡棠,汪中洋,萧洁儿.珠江口门枯季动力过程及盐度分布特征[J].热带地理,2013,33(4):400-406.
作者姓名:范中亚  林澍  曾凡棠  汪中洋  萧洁儿
作者单位:(环境保护部华南环境科学研究所 水环境模拟与污染控制研究中心,广州 510655)
基金项目:国家重大科技专项水污染控制与治理资助项目(2014ZX07211-005);中央级公益性科研院所科研业务专项
摘    要:2011年2月在珠江口八口门进行了同时段综合水文测验,对测验期间资料进行分析,结果表明:(1)八口门分流比从大至小依次为:磨刀门、虎门、洪奇门、蕉门、崖门、虎跳门、鸡啼门和横门;(2)外海潮波传入河口,磨刀门、鸡啼门高潮位首先出现,而虎门和蕉门最后出现,其时差约为1~2 h;磨刀门属于强径流弱潮流河口,相比其他口门涨潮流速偏小,落潮流速偏大;(3)八口门潮周期盐度平均值从大至小依次为:虎门、崖门、磨刀门、虎跳门、横门、蕉门、洪奇门、鸡啼门;(4)虎门、崖门和鸡啼门盐度属于强混合型;磨刀门大潮属于强混合型,小潮处于高度层化型河口;其他4个口门属于中等强度混合类型,其特点为下层盐度大,上层盐度小,大潮时混合强一些,小潮时混合弱一些。

关 键 词:珠江口门  动力过程  盐度  枯季  

Characteristics of Hydrodynamics and Salinity in the Estuaries of the Pearl River in Dry Season
FAN Zhongya , LIN Shu , ZENG Fantang , WANG Zhongyang , XIAO Jie’er.Characteristics of Hydrodynamics and Salinity in the Estuaries of the Pearl River in Dry Season[J].Tropical Geography,2013,33(4):400-406.
Authors:FAN Zhongya  LIN Shu  ZENG Fantang  WANG Zhongyang  XIAO Jie’er
Abstract:Large scale hydrological observations in the eight estuaries of the Pearl River were simultaneously carried out in February, 2011. Analysis of the field data showed that: (1) the eight estuaries in descendant order of runoff were: Modaomen, Humen, Hongqimen, Jiaomen, Yamen, Hutiaomen, Jitimen and Hengmen; (2) during tide waves going into the estuaries, Modaomen and Jitimen reached their top water level first, Humen and Jiaomen the last, and their time difference about 1 to 2 hours; the runoff was strong and tide was weak in Modaomen; the flood velocity in Modaomen was smaller than those in other estuaries, but ebb velocity the contrary; (3) the eight estuaries in descendant order of average salinity were: Humen, Yamen, Modaomen, Hutiaomen, Hengmen, Jiaomen, Hongqimen and Jitimen; (4) Humen, Yamen and Jitimen were of strong salinity mixing type; Modaomen belonged to strong salinity mixing type during spring tide, but high-degree stratification type during neap tide. other four estuaries belonged to moderate-degree mixing type, which were characterized by high salinity at bottom layer and low at surface layer, strong mixing during spring tide and weak mixing during neap tide.
Keywords:the estuaries of the Pearl River  hydrodynamics  salinity  dry season
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