Critical threshold of periodic point bar scour and sediment body transport path in tidal reaches: A case study of Fujiangsha reach, Yangtze River

被引:2
作者
Wang, Jianjun [1 ]
Yang, Yunping [2 ]
Zhang, Mingjin [2 ]
Zhu, Lingling [3 ]
Li, Shaowu [1 ]
Wen, Yuncheng [4 ]
机构
[1] Tianjin Univ, State Key Lab Hydraul Engn Simulat & Safety, Tianjin 300072, Peoples R China
[2] Minist Transport, Tianjin Res Inst Water Transport Engn, Key Lab Engn Sediment, Tianjin 300456, Peoples R China
[3] Bur Hydrol Changjiang Water Resources Commiss, Wuhan 430010, Peoples R China
[4] Natl Energy Adm, Minist Water Resources, Minist Transport, Nanjing Hydraul Res Inst, Nanjing 210024, Peoples R China
基金
中国国家自然科学基金;
关键词
periodic scouring; critical dynamic conditions; critical morphological characteristics; Jingjiang bank; Fujiangsha reach; EVOLUTION; ESTUARY; DEPOSITION; MECHANISM; IMPACTS; EROSION; CLIMATE; TRENDS; DATONG; LOAD;
D O I
10.1007/s11442-023-2132-8
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The evolution of point bars in changing sections of a downstream tidal current limit is periodic. Accordingly, assessing the critical morphology and hydrodynamic characteristics of point bar scour and the sediment transport process of scour sediment bodies can support river regulation and waterway maintenance. The frequent scour of point bars in changing sections of tidal current limits within the Yangtze River directly restricts waterway stability. This study examined the Fujiangsha reach of the Yangtze River, hydrological data on sediment transport, and riverbed topography from 1950. The Jingjiang bank tail exhibited an evolutionary cycle (siltation>scour>siltation), with a primary period ranging from 3-6 years. Additionally, certain morphological and dynamic conditions were necessary for scour. The Datong station flow (Q) ranged from 20,000-40,000 m(3)& BULL;s(-1) for & GT;180 days & BULL;yr(-1), enabling the bank silt layers to widen. Scour occurred during flooding and was concentrated in areas 5.0-7.5 km downstream from Ebizui. When Q & GT;40,000 m(3)& BULL;s(-1) scouring occurred in the bank middle and lower reaches, whereas Q & GT;50,000 m(3)& BULL;s(-1) for >50 consecutive days, scour occurred at the tail as well. Moreover, the volume of the scour shoals increased with the number of high-flow days (& GT;60,000 m(3)& BULL;s(-1)). Bottom sand transport mainly occurred in the low-bank zone. Before the project's second phase, the longitudinal transport of the scouring sand bodies occurred as follows: Jingjiang bank > low bank on the north side of Shuangjiansha > Fubei anabranch. During the second phase, the longitudinal transport route changed to Jingjiang bank > Fubei anabranch. The Jingjiang bank volume was also reduced; thus, its development was controlled. Owing to changes in the longitudinal transport routes, dredging should be conducted in areas where scouring sand bodies are separately transported from the tail, thereby reducing the load of dredging and maintenance for the Fubei anabranch during dry years.
引用
收藏
页码:1334 / 1358
页数:25
相关论文
共 64 条
[1]  
Chen X., 2014, PORT WATERWAY ENG, V489, P1
[2]   Dynamic analysis of riverbed evolution: Chengtong Reach of Yangtze Estuary [J].
Chen, Yongping ;
Li, Jiangxia ;
Wu, Zhigang ;
Pan, Shunqi .
JOURNAL OF COASTAL RESEARCH, 2016, :203-207
[3]  
[陈云 Chen Yun], 2022, [海洋科学进展, Advances in Marine Science], V40, P247
[4]   A thirteen-year record of bathymetric changes in the North Passage, Changjiang (Yangtze) estuary [J].
Dai, Zhijun ;
Liu, James T. ;
Fu, Gui ;
Xie, Hualiang .
GEOMORPHOLOGY, 2013, 187 :101-107
[5]   Morphologic and facies trends through the fluvial-marine transition in tide-dominated depositional systems: A schematic framework for environmental and sequence-stratigraphic interpretation [J].
Dalrymple, Robert W. ;
Choi, Kyungsik .
EARTH-SCIENCE REVIEWS, 2007, 81 (3-4) :135-174
[6]  
Du D., 2021, PORT WATERWAY ENG, V581, P75
[7]   Changjiang Delta in the Anthropocene: Multi-scale hydro-morphodynamics and management challenges [J].
Guo, Leicheng ;
Zhu, Chunyan ;
Xie, Weiming ;
Xu, Fan ;
Wu, Hui ;
Wan, Yuanyang ;
Wang, Zhanghua ;
Zhang, Weiguo ;
Shen, Jian ;
Wang, Zheng Bing ;
He, Qing .
EARTH-SCIENCE REVIEWS, 2021, 223
[8]   From the headwater to the delta: A synthesis of the basin-scale sediment load regime in the Changjiang River [J].
Guo, Leicheng ;
Su, Ni ;
Townend, Ian ;
Wang, Zheng Bing ;
Zhu, Chunyan ;
Wang, Xianye ;
Zhang, Yuning ;
He, Qing .
EARTH-SCIENCE REVIEWS, 2019, 197
[9]   Revisited sediment budget with latest bathymetric data in the highly altered Yangtze (Changjiang) Estuary [J].
Guo, Xingjie ;
Fan, Daidu ;
Zheng, Shuwei ;
Wang, Hanmei ;
Zhao, Baocheng ;
Qin, Changjie .
GEOMORPHOLOGY, 2021, 391
[10]   Channel evolution under changing hydrological regimes in anabranching reaches downstream of the Three Gorges Dam [J].
Han, Jianqiao ;
Zhang, Wei ;
Yuan, Jing ;
Fan, Yongyang .
FRONTIERS OF EARTH SCIENCE, 2018, 12 (03) :640-648