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三峡建坝后长江宜昌—汉口河段水沙与河床的应变

袁文昊 李茂田 陈中原 尹道卫 韦桃源

袁文昊, 李茂田, 陈中原, 尹道卫, 韦桃源. 三峡建坝后长江宜昌—汉口河段水沙与河床的应变[J]. 华东师范大学学报(自然科学版), 2016, (2): 90-100. doi: 10.3969/j.issn.1000-5641.2016.02.012
引用本文: 袁文昊, 李茂田, 陈中原, 尹道卫, 韦桃源. 三峡建坝后长江宜昌—汉口河段水沙与河床的应变[J]. 华东师范大学学报(自然科学版), 2016, (2): 90-100. doi: 10.3969/j.issn.1000-5641.2016.02.012
YUAN Wen-Hao, LI Mao-Tian, CHEN Zhong-Yuan, YIN Dao-Wei, WEI Tao-Yuan. Responses of runoffsediment flux and bedform in the Middle Yangtze River to the completion of the Three Gorges Dam[J]. Journal of East China Normal University (Natural Sciences), 2016, (2): 90-100. doi: 10.3969/j.issn.1000-5641.2016.02.012
Citation: YUAN Wen-Hao, LI Mao-Tian, CHEN Zhong-Yuan, YIN Dao-Wei, WEI Tao-Yuan. Responses of runoffsediment flux and bedform in the Middle Yangtze River to the completion of the Three Gorges Dam[J]. Journal of East China Normal University (Natural Sciences), 2016, (2): 90-100. doi: 10.3969/j.issn.1000-5641.2016.02.012

三峡建坝后长江宜昌—汉口河段水沙与河床的应变

doi: 10.3969/j.issn.1000-5641.2016.02.012
基金项目: 

长江中下游典型大坝水库泥沙淤积过程中溶解硅滞留行为探究(41271520)

详细信息
    通讯作者:

    李茂田,男,副教授,研究方向为河流动力地貌学.

  • 中图分类号: P47

Responses of runoffsediment flux and bedform in the Middle Yangtze River to the completion of the Three Gorges Dam

  • 摘要: 通过三峡建坝前后19502013年的水文、泥沙与2003年和2011年的实测河床底形资料对比,试图讨论长江中游宜昌汉口河段水沙及河床地形等应变量对三峡建坝的响应,为人们理解河流水沙及河床冲淤对超大型水库应变的幅度提供具体案例. 三峡建坝后,宜昌站和汉口站年均流量由建坝前的13 850 m3/s和22 650 m3/s(19502002)减少到建坝后的12 450 m3/s和21 000 m3/s(20032013),分别减少10.1%和7.2%;年均输沙量由5.56亿t和4.02亿t(19502002)锐减至0.6亿t和1.5亿t(20032013),分别减少89.5%和62.2%;年均悬沙中值粒径则由35 \mm(19502002)和25 \mm(19551975)减少至4 \mm和15 \mm(20032010). 同时,水流挟沙不饱和能力的增加,引起了河床的沿程冲刷及泥沙粗化,宜枝河段、荆江河段和城汉河段深泓处分别平均冲刷了3.7 m、1.5 m 和 0.4 m,在主槽刷深的同时,河道浅滩有不同程度的萎缩. 三峡建坝已导致中游水沙及冲淤条件发生了巨大改变. 
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出版历程
  • 收稿日期:  2015-03-02
  • 刊出日期:  2016-03-25

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