Mid-channel Bars
Mid-Channel Bars is a fluvial landform characterized as a longitudinal, elongated deposit of sediment within the river channel, distinguished by its central or near-central position relative to the thalweg and its formation through flow separation and sediment deposition in response to channel width variations or bedform interactions.
36
Publications
1.5K
Citations
108
Authors
64
Institutions
Publications per year
2017–2026
16
36
1–5 of 36
108
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Chongqing Institute of Green and Intelligent Technology, China
2 publications · 61 citations
2
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2
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1–5 of 108
64

Chinese Academy of Sciences
Beijing, China
3 h-index
7 publications
175 citations

University of Liverpool
Liverpool, United Kingdom
2 h-index
2 publications
120 citations

University of Bradford
Bradford, United Kingdom
2 h-index
2 publications
28 citations
National Institute of Technology Warangal
Warangal, India
2 h-index
2 publications
28 citations
Indian Institute of Technology Guwahati
Guwahati, India
2 h-index
7 publications
115 citations
Chongqing Institute of Green and Intelligent Technology
Chongqing, China
2 h-index
8 publications
234 citations

University of Leeds
Leeds, United Kingdom
2 h-index
3 publications
353 citations

East China Normal University
Shanghai, China
2 h-index
9 publications
277 citations
1–8 of 64
6 publications · 469 citations
6
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4 publications · 186 citations
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JSR · 3 publications · 105 citations
3
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2 publications · 29 citations
2
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2 publications · 31 citations
2
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1–5