荆江陈家湾—突起洲分汊段河道演变与趋势分析

廖宇昂, 刘瑜

长江科学院院报 ›› 2024, Vol. 41 ›› Issue (7) : 196-202.

PDF(31486 KB)
PDF(31486 KB)
长江科学院院报 ›› 2024, Vol. 41 ›› Issue (7) : 196-202. DOI: 10.11988/ckyyb.20231368
长江治理与保护创新发展暨三峡工程蓄水运用20周年学术研讨会专栏

荆江陈家湾—突起洲分汊段河道演变与趋势分析

  • 廖宇昂, 刘瑜
作者信息 +

Channel Evolution and Trend of Chenjiawan-Tuqi Sandbar Braided Reach in the Jingjiang River

  • LIAO Yu-ang, LIU Yu
Author information +
文章历史 +

摘要

三峡工程的运行极大减轻了荆江的防洪压力,同时改变了河段水沙条件,导致荆江持续发生剧烈冲淤变化。荆江陈家湾—突起洲段为典型微弯分汊河型,滩槽格局调整、主支汊易位将直接影响航道运行和防洪安排。基于三峡工程运行前后长系列水文与河道原型观测资料,揭示河段水沙变化与河床冲淤响应特征,分析河道形态尺度年际变化过程,总结河道演变规律及趋势。结果表明:三峡工程运行后,沙市站平均年输沙量下降85%,河床冲刷3.1亿m3。以太平口—三八滩汊道段滩槽变化最为剧烈,主流走势由北转南。2011年后,三八滩与腊林洲边滩守护工程基本遏制了“太平口心滩南槽南靠、三八滩南汊北提”趋势,但该段河床随即再次调整,近期又表现出“南槽北扩、南汊南扩”的新情势。同时,由于三八滩南汊发育、北汊分流比降低,北汊长江大桥下的通航问题日益突显,如何解决碍航问题,仍需进一步开展研究。

Abstract

The operation of the Three Gorges Project has significantly alleviated flood control pressures on the Jingjiang River and altered water and sediment dynamics along its course, leading to continuous and substantial erosion and sedimentation changes in the river. The Chenjiawan-Tuqi sandbar reach in the Jingjiang River represents a prototypical gently curved braided channel, where adjustments to the beach and primary branch patterns directly impact channel operations and flood mitigation measures. By analyzing long-term hydrological data and channel topography prototype observations before and after Three Gorges Project operation, we revealed the variations in water and sediment transport within the reach and the riverbed’s responses to erosion and sediment deposition. Furthermore, we examined the interannual morphological changes and scales of the channel,and summarized its evolving regularities and trends. Results indicated an 85% reduction in average annual sediment transport at Shashi Station after Three Gorges Project operation, with an erosion of 310 million cubic meters of riverbed material. The most pronounced beach changes occurred from Taiping estuary sandbar to Sanba sandbar braided reach, prompting a shift in the main flow direction from north to south. Subsequent to the 2011 implementation of the Sanba sandbar and Lalin sandbar beach protection project, the trend of “southward movement of Taiping Estuary sandbar south of the main channel and northward movement of Sanba sandbar south branch” has been largely mitigated. However, ongoing adjustments in this river section have resulted in a new pattern characterized by “northward expansion of the south deep trough and southward expansion of the south branch”. The increasing development along the south branch of the Sanba sandbar and reduced diversion ratio on the north branch have raised navigation concerns near the Yangtze River Bridge. Further investigations are necessary to address the navigation obstruction effectively.

关键词

河道演变 / 冲淤分析 / 三峡工程 / 分汊河段 / 荆江

Key words

channel evolution / deposition-scouring analysis / Three Gorges Project / braided reach / Jingjiang River

引用本文

导出引用
廖宇昂, 刘瑜. 荆江陈家湾—突起洲分汊段河道演变与趋势分析[J]. 长江科学院院报. 2024, 41(7): 196-202 https://doi.org/10.11988/ckyyb.20231368
LIAO Yu-ang, LIU Yu. Channel Evolution and Trend of Chenjiawan-Tuqi Sandbar Braided Reach in the Jingjiang River[J]. Journal of Changjiang River Scientific Research Institute. 2024, 41(7): 196-202 https://doi.org/10.11988/ckyyb.20231368
中图分类号: TV147   

参考文献

[1] 胡春宏, 方春明. 三峡工程泥沙问题解决途径与运行效果研究[J]. 中国科学: 技术科学, 2017, 47(8): 832-844. (HU Chun-hong, FANG Chun-ming. Research on Sediment Problem Solutions for the Three Gorges Project and it Operational Effects[J]. Scientia Sinica (Technologica), 2017, 47(8): 832-844.(in Chinese))
[2] 郭振英.三峡工程建设运行效益的研究及评价[J].长江技术经济,2019,3(4):4-9.(GUO Zhen-ying.Research and Evaluation of the Construction and Operation Benefits of the Three Gorges Project[J]. Technology and Economy of Changjiang,2019,3(4):4-9.(in Chinese))
[3] 许全喜,童 辉.近50年来长江水沙变化规律研究[J].水文,2012,32(5):38-47,76.(XU Quan-xi, TONG Hui. Characteristics of Flow and Sediment Change in Yangtze River in Recent 50 Years[J]. Journal of China Hydrology, 2012, 32(5): 38-47, 76.(in Chinese))
[4] 许全喜.三峡工程蓄水运用前后长江中下游干流河道冲淤规律研究[J].水力发电学报,2013,32(2):146-154.(XU Quan-xi.Study of Sediment Deposition and Erosion Patterns in the Middle and Downstream Changjiang Mainstream after Impoundment of TGR[J]. Journal of Hydroelectric Engineering,2013,32(2):146-154.(in Chinese))
[5] 董炳江,许全喜,袁 晶,等.近年来三峡水库坝下游河道强烈冲刷机理分析[J].泥沙研究,2019,44(5):42-47.(DONG Bing-jiang, XU Quan-xi, YUAN Jing, et al. Mechanism of Serious Scour along the Downstream of Three Gorges Reservoir in Recent Years[J]. Journal of Sediment Research, 2019, 44(5): 42-47.(in Chinese))
[6] 朱玲玲,许全喜,陈子寒.新水沙条件下荆江河段强冲刷响应研究[J].应用基础与工程科学学报,2018,26(1):85-97.(ZHU Ling-ling, XU Quan-xi, CHEN Zi-han. Extraordinary Scour of Jingjiang Reach Downstream from Three Gorges Project[J]. Journal of Basic Science and Engineering, 2018, 26(1): 85-97.(in Chinese))
[7] 张明进. 新水沙条件下荆江河段航道整治工程适应性及原则研究[D]. 天津: 天津大学, 2014. (ZHANG Ming-jin. Research on Principles for Channel Regulation of the Jingjiang River Channel Improvement under New Conditions of Water and Sediment[D].Tianjin: Tianjin University, 2014. (in Chinese))
[8] 周美蓉, 夏军强, 邓珊珊, 等. 三峡工程运用后长江中游河床调整沿程变化特点[J]. 湖泊科学, 2023, 35(2): 642-650. (ZHOU Mei-rong, XIA Jun-qiang, DENG Shan-shan,et al. Longitudinal Variation of Channel Evolution along the Middle Yangtze River after the Operation of the Three Gorges Project[J]. Journal of Lake Sciences, 2023, 35(2): 642-650.(in Chinese))
[9] 朱勇辉,黄 莉,郭小虎,等.三峡工程运用后长江中游沙市河段演变与治理思路[J].泥沙研究,2016(3):31-37.(ZHU Yong-hui, HUANG Li, GUO Xiao-hu, et al. Analysis of Processes and Regulation of Shashi River Reach in the Middel Reach of Yangtze River after the TGP Operation[J]. Journal of Sediment Research, 2016(3): 31-37.(in Chinese))
[10]彭严波,段光磊.长江荆江河段沙市三八滩演变机理分析[J].人民长江,2006,37(9):82-83.(PENG Yan-bo,DUAN Guang-lei.Evolution Mechanism Analysis of Sanba Beach in Shashi,Jingjiang Reach of the Yangtze River[J]. Yangtze River, 2006, 37(9): 82-83.(in Chinese))
[11]李溢汶,夏军强,邓珊珊,等.三峡工程运用前后沙市段河床形态调整特点[J].长江科学院院报,2019,36(2):13-19.(LI Yi-wen,XIA Jun-qiang,DENG Shan-shan,et al. Riverbed Geomorphic Adjustments in the Shashi Reach before and after the Operation of Three Gorges Project[J]. Journal of Yangtze River Scientific Research Institute, 2019, 36(2): 13-19.(in Chinese))
[12]杨云平,李 明,刘万利,等.长江荆江河段滩槽演变与航道水深资源提升关系[J].水科学进展,2022,33(2):240-252.(YANG Yun-ping, LI Ming, LIU Wan-li, et al. Study on the Relationship between Beach Trough Evolution and Navigation Obstruction Characteristics in Jingjiang Reach of the Yangtze River[J]. Advances in Water Science, 2022, 33(2): 240-252.(in Chinese))
[13]陈思含. 荆江河段平滩河槽形态对水沙条件响应研究[D]. 武汉: 长江科学院, 2021. (CHEN Si-han. Study on the Response of Bankfull Channel Geometry to Water and Sediment Conditions in the Jingjiang Reach[D].Wuhan: Changjiang River Scientific Research Institute, 2021. (in Chinese))
[14]汪 飞, 贾建伟, 邴建平. 沙市河段河道演变趋势的预测研究[C]//中国水利学会2021学术年会论文集第五分册. 北京:中国水利学会, 2021: 249-260.(WANG Fei, JIA Jian-wei, BING Jian-ping. Prediction of Channel Evolution of Shashi River Course[C]//Proceedings of 2021 Annual Conference of Chinese Hydraulic Engineering Society. Beijing: Chinese Hydraulic Engineering Society, 2021: 249-260. (in Chinese))
[15]张 红, 刘启航. 上荆江瓦口子至马家咀河段河床演变趋势预测研究[J]. 人民珠江, 2021, 42(9): 77-85. (ZHANG Hong, LIU Qi-hang. Study of Bed Deformation Trend of Wakouzi-Majiazui Section in the Upper Jingjiang Reach of Yangtze River[J]. Pearl River, 2021, 42(9): 77-85.(in Chinese))
[16]董耀华, 卢金友, 范北林, 等. 三峡水库运用后荆江典型河段冲淤变化计算分析[J]. 长江科学院院报, 2005, 22(2): 9-12. (DONG Yao-hua, LU Jin-you, FAN Bei-lin, et al. Research on Variations of Typical Lower Jingjiang River Reach after Three Gorges Project Operation[J]. Journal of Yangtze River Scientific Research Institute, 2005, 22(2): 9-12.(in Chinese))
[17]孙启航, 夏军强, 邓珊珊, 等. 基于圆弧与平面滑动模式的上荆江崩岸过程模拟对比分析[J]. 应用基础与工程科学学报, 2023, 31(1): 38-51. (SUN Qi-hang, XIA Jun-qiang, DENG Shan-shan,et al. Comparison of Simulated Bank Erosion Processes in the Upper Jingjiang Reach Using the Circular and Planar Sliding Modes[J]. Journal of Basic Science and Engineering, 2023, 31(1): 38-51.(in Chinese))
[18]刘昭希, 王 军, 周银军, 等. 长江荆江段二元结构河岸土体力学性能及崩塌试验[J]. 长江科学院院报, 2023, 40(2): 7-13, 26. (LIU Zhao-xi, WANG Jun, ZHOU Yin-jun, et al. Mechanical Properties and Collapse Test of Composite Riverbanks in Jingjiang Reach of Changjiang River[J]. Journal of Changjiang River Scientific Research Institute, 2023, 40(2): 7-13, 26.(in Chinese))
[19]张 翼, 夏军强, 邓珊珊, 等. 上荆江典型断面河床纵横向变形过程的概化模拟[J]. 长江科学院院报, 2016, 33(7): 6-11, 22. (ZHANG Yi, XIA Jun-qiang, DENG Shan-shan, et al. Generalized Simulation of the Longitudinal and Lateral Channel Evolution of Typical Section in the Upper Jingjiang Reach[J]. Journal of Yangtze River Scientific Research Institute, 2016, 33(7): 6-11, 22.(in Chinese))
[20]刘昭希, 王 军, 宗全利, 等. 含水率变化对荆江河岸黏性土体力学特性的影响[J]. 长江科学院院报, 2019, 36(4): 32-38. (LIU Zhao-xi, WANG Jun, ZONG Quan-li, et al. Influence of Water Content Variation on Mechanical Properties of Riverbank Cohesive Soil of Jingjiang River Reach[J]. Journal of Yangtze River Scientific Research Institute, 2019, 36(4): 32-38.(in Chinese))

基金

国家重点研发计划项目(2022YFC3201801,2022YFC3201804)

PDF(31486 KB)

Accesses

Citation

Detail

段落导航
相关文章

/