Flow-sediment Connectivity
Flow-Sediment Connectivity is a hydrological construct that characterizes the degree to which surface water flow regimes facilitate the entrainment, transport, and deposition of sediment within fluvial systems, thereby maintaining geomorphological continuity and process linkages across river corridors.
151
Publications
12K
Citations
561
Authors
288
Institutions
Publications per year
2017–2026
84
151
1–5 of 151
561
Research Institute for Geo-Hydrological Protection, Italy
8 publications · 1.8K citations
8
h-index
6
h-index
4
h-index
Research Institute for Geo-Hydrological Protection, Italy
4 publications · 540 citations
4
h-index
3
h-index
1–5 of 561
288

Chinese Academy of Sciences
Beijing, China
9 h-index
30 publications
1.4K citations
Research Institute for Geo-Hydrological Protection
Perugia, Italy
9 h-index
17 publications
6K citations
University of Chinese Academy of Sciences
Beijing, China
7 h-index
13 publications
478 citations

Macquarie University
Sydney, Australia
6 h-index
11 publications
2K citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
18 publications
913 citations
Institute of Geographic Sciences and Natural Resources Research
Beijing, China
6 h-index
11 publications
481 citations

Beijing Normal University
Beijing, China
6 h-index
22 publications
720 citations
National Research Council
Rome, Italy
6 h-index
11 publications
2.5K citations
1–8 of 288
22 publications · 2.6K citations
19
h-index
12 publications · 796 citations
12
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13 publications · 2.2K citations
12
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9 publications · 491 citations
10
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4 publications · 210 citations
5
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1–5