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KONG Ya-zhen, HE Song-lin, DING Ping-xing, HU Ke-lin. Characteristics of temporal and spatial variation of salinity and their indicating significance in the Changjiang Estuary[J]. Haiyang Xuebao, 2004, 26(4): 9-18.
Citation: KONG Ya-zhen, HE Song-lin, DING Ping-xing, HU Ke-lin. Characteristics of temporal and spatial variation of salinity and their indicating significance in the Changjiang Estuary[J]. Haiyang Xuebao, 2004, 26(4): 9-18.

Characteristics of temporal and spatial variation of salinity and their indicating significance in the Changjiang Estuary

  • Received Date: 2003-12-01
  • Rev Recd Date: 2004-04-30
  • Large scale hydrological observations in the Changjiang Estuary have been respectively carried out in February and July,2003.The survey range extends from Jiangyin to -20 m iso depth out of the mouth,and the measuring stations distribute in four outlets.Field observations show that:(1) temporal and spatial variation of salinity is mainly controlled run off discharge,flow distribution ratio of the outlets,tidal range and geomorphologic situation;(2) the order from high to low for the distribution of salinity is the North Branch,South Passage,North Passage,and the North Channel;(3) the saltwater flows backwards from the North Branch to the South Branch during the dry season,but more than half section of the North Branch is still held by freshwater during the flood season;the mouth sector of the North Channel,where tidal variation of salinity is major and seasonal variation is minor,has stratified interface between saltwater and freshwater;the South Passage,where tidal variation of salinity is minor and seasonal variation is major,is characteristic of mid strongly mixed type;and the situation of the North Passage is between situations of the North Channel and the South Passage;(4) the temporal and spatial variation of salinity reflects that flow distribution ratio to the North Branch,the North Channel and the South Passage increases to a certain extent in the flood season.
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  • 王盼成,贺松林.长江大通站水沙过程的基本特征.I.径流过程分析[J].华东师范大学学报(自然科学版),2004,(2):72-82.
    沈焕庭,茅志昌,陈吉余.南水北调对长江口咸水入侵影响预测及对策[A].陈吉余.南水北调(东线)对长江口生态环境影响及其对策[M].上海:华东师范大学出版社,2003.79-86.
    吴守培,顾玉亮.北支盐水入侵对长江口水源地的影响[A].陈吉余.南水北调(东线)对长江口生态环境影响及其对策[M].上海:华东师范大学出版社,2003.108-131.
    陈吉余,沈焕庭,徐海根,等.三峡工程对长江河口盐水入侵和侵蚀堆积过程影响的初步分析[A].中国科学院三峡工程生态与环境科研项目领导小组.长江三峡工程对生态与环境景响及其对策研究论文集[C].北京:科学出版社,1987.350-368.
    沈焕庭,茅志昌,谷国传,等.南水北调对长江河口盐水入侵的影响[A].陈吉余,等.长江河口动力地貌和沉积过程[M].上海:上海科学技术出版社,1988.145-150.
    韩乃斌,顾玉亮,徐建益.南水北调对长江口盐水入侵影响分析[A].陈吉余.南水北调(东线)对长江口生态环境影响及其对策[M].上海:华东师范大学出版社,2003.87-99.
    沈焕庭,郭成涛,朱慧芳,等.长江河口最大浑浊带的变化规律及其成因探讨[A].陈吉余,等.长江河口动力地貌和沉积过程[M].上海:上海科学技术出版社,1988.216-228.
    贺松林,孙介民.长江河口最大浑浊带悬沙输移特征[J].海洋与湖沼,1996,27(1):60-66.
    沈焕庭,胡辉.长江口门附近的水流与混合[A].陈吉余,等.长江河口动力地貌和沉积过程[M].上海:上海科学技术出版社,1988.131-144.
    潘定安,胡方西,周月琴,等.长江河口夏季的盐淡水混合[A].陈吉余,等.长江河口动力地貌和沉积过程[M].上海:上海科学技术出版社,1988.151-165.
    胡方西,胡辉,谷国传,等.长江口锋面研究[M].上海:华东师范大学出版社,2002.16-21.
    沈焕庭.长江河口物质通量[M].北京:海洋出版社,2001.91-92.
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