Study of the ebb sediment diversion ratios during wet season in the South and North Passage, Changjiang Estuary

  • YANG Wan-lun ,
  • DAO Fu-hai ,
  • LUAN Hua-long ,
  • GE Jian-zhong ,
  • DING Ping-xing
Expand
  • State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China

Received date: 2017-02-23

  Online published: 2018-03-22

Abstract

This study investigates the characteristics of the ebb water and sediment diversion ratios during wet season in the North Passage, Changjiang Estuary and the reasons for the differences within neap-spring tidal cycles based on field measurements. The results of the measurements indicate that the averaged ebb flow diversion ratios of the North Passage in spring and neap tide are 41.9% and 43.1%, respectively, while the averaged ebb sediment diversion ratios of the North Passage in spring and neap tide are 35.1% and 39%,the averaged ebb sediment diversion ratios of the North Passage in spring can approximate representatively ebb sediment diversion status. The ebb sediment diversion ratio of the North Passage is dependent on the ratios of mean flow velocity, suspended sediment concentration and section areas of the North and South Passage. And these parameters show minor changes within neap-spring tidal cycles. Therefore, it can be concluded that the differences of ebb flow and sediment diversions of the North Passage within neap-spring tidal cycles are limited.

Cite this article

YANG Wan-lun , DAO Fu-hai , LUAN Hua-long , GE Jian-zhong , DING Ping-xing . Study of the ebb sediment diversion ratios during wet season in the South and North Passage, Changjiang Estuary[J]. Journal of East China Normal University(Natural Science), 2018 , 2018(2) : 170 -180 . DOI: 10.3969/j.issn.1000-5641.2018.02.018

References

[1] 陈吉余, 沈焕庭, 恽才兴. 长江河口动力过程和地貌演变[M]. 上海:上海科学技术出版社, 1988.
[2] 杨婷, 陶建峰, 张长宽, 等. 长江口整治工程对分水分沙年际变化的影响分析[J]. 人民长江, 2012(5):84-88.
[3] 谢华亮, 戴志军, 李为华, 等. 长江口南北槽分流口动力地貌过程研究[J]. 应用海洋学学报, 2014(2):151-159.
[4] 窦润青, 郭文云, 葛建忠, 等. 长江口北槽落潮分流比变化原因分析[J]. 华东师范大学学报(自然科学版), 2014(3):93-104.
[5] 童朝锋, 严以新, 孟艳秋, 等. 分汊河道分流比估算方法[J]. 水利水电科技进展, 2011(6):7-9.
[6] 杨世伦, 贺松林, 谢文辉. 长江口九段沙的形成演变及其与南北槽发育的关系[J]. 海洋工程, 1998(4):56-66.
[7] 周济福, 李家春. 鱼咀及丁坝对长江口航道分流分沙的影响[J]. 应用数学和力学, 2004(2):141-149.
[8] 高敏, 范期锦, 谈泽炜, 等. 对长江口北槽分流比的分析研究[J]. 水运工程, 2009(5):82-86.
[9] 刘杰, 陈吉余, 徐志扬. 长江口深水航道治理工程实施后南北槽分汊段河床演变[J]. 水科学进展, 2008(5):605-612.
[10] 交通运输部长江口航道管理局. 长江口12.5 m深水航道维护河势跟踪分析报告[R]. 上海:交通运输部长江口航道管理局, 2012.
[11] 丁君松, 丘凤莲. 汊道分流分沙计算[J]. 泥沙研究, 1981(1):58-64.
[12] 英晓明, 丁平兴, 胡克林, 等. 基于ADCP和OBS观测的洋山港关键断面水沙通量研究[J]. 泥沙研究, 2010(2):22-30.
[13] 冯凌旋. 长江口南北槽分流口演变及其对北槽深水航道整治工程的响应[D]. 上海:华东师范大学, 2010.
[14] 冯凌旋, 李九发, 刘新成, 等. 近期长江河口南、北槽分流口河床演变过程研究[J]. 泥沙研究, 2012(6):39-45.
Outlines

/