Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications

Low-angle lee-side slopes of dunes are commonly developed on the world’s riverbeds, and dune migration associated with sediment transport exert a major influence on riverine processes. However, the catenary-bead dune has been identified in the Yangtze River (YR) Estuary, featuring a higher lee-side...

Full description

Bibliographic Details
Main Authors: Shuwei Zheng, Xinmeng Yuan, Suxian Yang, Heqin Cheng, Xingjie Guo, Yurong Cui, Enfeng Liu, Zijun Li
Format: Article
Language:English
Published: MDPI AG 2022-06-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/10/7/886
_version_ 1797446090979540992
author Shuwei Zheng
Xinmeng Yuan
Suxian Yang
Heqin Cheng
Xingjie Guo
Yurong Cui
Enfeng Liu
Zijun Li
author_facet Shuwei Zheng
Xinmeng Yuan
Suxian Yang
Heqin Cheng
Xingjie Guo
Yurong Cui
Enfeng Liu
Zijun Li
author_sort Shuwei Zheng
collection DOAJ
description Low-angle lee-side slopes of dunes are commonly developed on the world’s riverbeds, and dune migration associated with sediment transport exert a major influence on riverine processes. However, the catenary-bead dune has been identified in the Yangtze River (YR) Estuary, featuring a higher lee-side angle. To date, the morphological variation and formation reasons of catenary-bead dunes in the YR Estuary remain uncharacterized. In this study, we used a multibeam echo system (MBES) to investigate the bedforms of the YR estuary during 2014–2015, as well as to discuss the seasonal variation of catenary-bead dunes. The results indicate that the catenary-bead dunes of the YR Estuary are characterized by growth during the flood season and extinction during the dry season. The lee-side angle is typically ~16.7°, which is larger than that of other dune types (3.7–8°) in the estuary; moreover, the catenary-bead dunes are higher than other dune types of the same length in the YR Estuary. The relationship between the dune height (<i>H</i>) and length (<i>L</i>) was found to be <i>H</i> = 0.1667<i>L</i><sup>0.603</sup> (<i>R</i><sup>2</sup> = 0.38), while the other dune types yielded the relationship of <i>H</i> = 0.0845<i>L</i><sup>0.758</sup> (<i>R</i><sup>2</sup> = 0.52). Strong runoff superimposing the ebb tide led to the development of catenary-bead dunes. Furthermore, the higher coarse sediment content (69.9–72%) and lower clay content (6.3–6.7%) of the riverbed sediment are favorable for their formation, while the higher curved crest-lines are favorable for the formation of the associated elliptical pits.
first_indexed 2024-03-09T13:35:16Z
format Article
id doaj.art-a54b3864f9714fdeb199b9ceb2210893
institution Directory Open Access Journal
issn 2077-1312
language English
last_indexed 2024-03-09T13:35:16Z
publishDate 2022-06-01
publisher MDPI AG
record_format Article
series Journal of Marine Science and Engineering
spelling doaj.art-a54b3864f9714fdeb199b9ceb22108932023-11-30T21:12:58ZengMDPI AGJournal of Marine Science and Engineering2077-13122022-06-0110788610.3390/jmse10070886Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and ImplicationsShuwei Zheng0Xinmeng Yuan1Suxian Yang2Heqin Cheng3Xingjie Guo4Yurong Cui5Enfeng Liu6Zijun Li7College of Geography and Environment, Shandong Normal University, Jinan 250358, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250358, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250358, ChinaState Key Lab of Estuarine & Coastal Research, East China Normal University, Shanghai 200062, ChinaShanghai Institute of Geological Survey, Shanghai 200072, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250358, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250358, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250358, ChinaLow-angle lee-side slopes of dunes are commonly developed on the world’s riverbeds, and dune migration associated with sediment transport exert a major influence on riverine processes. However, the catenary-bead dune has been identified in the Yangtze River (YR) Estuary, featuring a higher lee-side angle. To date, the morphological variation and formation reasons of catenary-bead dunes in the YR Estuary remain uncharacterized. In this study, we used a multibeam echo system (MBES) to investigate the bedforms of the YR estuary during 2014–2015, as well as to discuss the seasonal variation of catenary-bead dunes. The results indicate that the catenary-bead dunes of the YR Estuary are characterized by growth during the flood season and extinction during the dry season. The lee-side angle is typically ~16.7°, which is larger than that of other dune types (3.7–8°) in the estuary; moreover, the catenary-bead dunes are higher than other dune types of the same length in the YR Estuary. The relationship between the dune height (<i>H</i>) and length (<i>L</i>) was found to be <i>H</i> = 0.1667<i>L</i><sup>0.603</sup> (<i>R</i><sup>2</sup> = 0.38), while the other dune types yielded the relationship of <i>H</i> = 0.0845<i>L</i><sup>0.758</sup> (<i>R</i><sup>2</sup> = 0.52). Strong runoff superimposing the ebb tide led to the development of catenary-bead dunes. Furthermore, the higher coarse sediment content (69.9–72%) and lower clay content (6.3–6.7%) of the riverbed sediment are favorable for their formation, while the higher curved crest-lines are favorable for the formation of the associated elliptical pits.https://www.mdpi.com/2077-1312/10/7/886dunessedimentary environmentmultibeam echo soundermorphological variationYangtze River Estuary
spellingShingle Shuwei Zheng
Xinmeng Yuan
Suxian Yang
Heqin Cheng
Xingjie Guo
Yurong Cui
Enfeng Liu
Zijun Li
Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications
Journal of Marine Science and Engineering
dunes
sedimentary environment
multibeam echo sounder
morphological variation
Yangtze River Estuary
title Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications
title_full Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications
title_fullStr Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications
title_full_unstemmed Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications
title_short Seasonal Variation of Catenary-Bead Dunes in the Yangtze River Estuary: Causes and Implications
title_sort seasonal variation of catenary bead dunes in the yangtze river estuary causes and implications
topic dunes
sedimentary environment
multibeam echo sounder
morphological variation
Yangtze River Estuary
url https://www.mdpi.com/2077-1312/10/7/886
work_keys_str_mv AT shuweizheng seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT xinmengyuan seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT suxianyang seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT heqincheng seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT xingjieguo seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT yurongcui seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT enfengliu seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications
AT zijunli seasonalvariationofcatenarybeaddunesintheyangtzeriverestuarycausesandimplications