Hyperconcentrated Flow
Hyperconcentrated Flow is a type of sediment-laden fluid flow distinguished from other fluvial flows by its exceptionally high sediment concentration, typically ranging between 20% and 60% by volume, which significantly alters its rheological behavior and transport mechanisms compared to conventional turbulent suspension or bedload transport.
52
Publications
2.5K
Citations
126
Authors
78
Institutions
Publications per year
2017–2026
10
Parents
52
Rheology of Hyperconcentrations
Pierre Y. Juliën, Yongqiang Lan · Journal of Hydraulic Engineering · 1991 · 166 citations
Erosion caused by hyperconcentrated flow on the Loess Plateau of China
Jiongxin Xu · CATENA · 1999 · 147 citations
Hyperpycnal (over density) flows and deposits
Carlos Zavala · Journal of Palaeogeography · 2020 · 135 citations · Full text
1–5 of 52
126
7
h-index
2
h-index
2
h-index
2
h-index
2
h-index
1–5 of 126
78

Chinese Academy of Sciences
Beijing, China
11 h-index
16 publications
607 citations
Institute of Geographic Sciences and Natural Resources Research
Beijing, China
6 h-index
11 publications
239 citations
Tsinghua University
Beijing, China
5 h-index
6 publications
164 citations

Beijing Normal University
Beijing, China
3 h-index
6 publications
152 citations
Wolters Kluwer (Netherlands)
Alphen aan den Rijn, The Netherlands
2 h-index
2 publications
129 citations
Institute of Soil and Water Conservation
Yangling, China
2 h-index
3 publications
184 citations
Colorado State University
Fort Collins, United States
2 h-index
4 publications
382 citations

Delft University of Technology
Delft, The Netherlands
2 h-index
2 publications
129 citations
1–8 of 78
6 publications · 215 citations
6
h-index
6 publications · 372 citations
6
h-index
4 publications · 89 citations
5
h-index
4 publications · 304 citations
4
h-index
JSR · 2 publications · 111 citations
2
h-index
1–5