留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH

陈宝冲

陈宝冲. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. 中国地理科学, 1994, 4(3): 242-251.
引用本文: 陈宝冲. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. 中国地理科学, 1994, 4(3): 242-251.
Chen Baochong. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. Chinese Geographical Science, 1994, 4(3): 242-251.
Citation: Chen Baochong. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. Chinese Geographical Science, 1994, 4(3): 242-251.

THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH

THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH

计量
  • 文章访问数:  702
  • HTML全文浏览量:  23
  • PDF下载量:  888
  • 被引次数: 0
出版历程
  • 刊出日期:  1994-09-20

THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH

摘要: The general form of the north-branch of the Changjiang River mouth has changed much as a result of the change of the main stream lines of the Nantong reach of the Changjiang River and the influence of human activities since 1915. By the 1930s, the main stream lines of the Nantong reach of the Changjiang River has shifted to the Tongzhou Bar west channel. The north-branch at the Changjiang River mouth has become atrophic because of Tongzhou Bar east channel's deposition. After 1958, Toughal Bar and Jiangxin Bar were exploited. And in 1970, the north channel of Jiangxin Bar was blocked up. All these things make the water of the north-branch more difficult to pass through. It leads to the decline of the total discharge percentage of the north-branch. And it causes the rising tide to go back to the south-branch. However, since 1978, with the development of Tongzhou Bar east channel and its left bank being scoured, the water amount of the north-branch has been increasing. And the water, load and salt of going back to the south-branch has been becoming less.

English Abstract

陈宝冲. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. 中国地理科学, 1994, 4(3): 242-251.
引用本文: 陈宝冲. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. 中国地理科学, 1994, 4(3): 242-251.
Chen Baochong. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. Chinese Geographical Science, 1994, 4(3): 242-251.
Citation: Chen Baochong. THE CHANGE OF THE GENERAL FORM AND THE TRANSPORT OF THE WATER, LOAD AND SALT ABOUT THE NORTH-BRANCH OF THE CHANGJIANG RIVER MOUTH[J]. Chinese Geographical Science, 1994, 4(3): 242-251.

目录

    /

    返回文章
    返回