Sediment Continuity
Sediment Continuity is a theoretical construct in river hydraulics that represents the principle governing the spatial and temporal conservation of sediment mass within a fluvial system, distinguishing it from other hydraulic continuity models by its specific focus on sediment transport rates and storage dynamics.
82
Publications
5.9K
Citations
208
Authors
100
Institutions
Publications per year
2017–2026
7
Parents
82
1–5 of 82
208
8
h-index
6
h-index
Norwegian University of Science and Technology, Norway
3 publications · 82 citations
3
h-index
3
h-index
3
h-index
1–5 of 208
100

University of Twente
Enschede, The Netherlands
5 h-index
9 publications
594 citations

University of Minnesota
Minneapolis, United States
4 h-index
8 publications
1.4K citations

Tarbiat Modares University
Tehran, Iran
4 h-index
7 publications
555 citations
University of Illinois Urbana-Champaign
Urbana, United States
3 h-index
3 publications
105 citations

Delft University of Technology
Delft, The Netherlands
3 h-index
5 publications
379 citations
Norwegian University of Science and Technology
Trondheim, Norway
3 h-index
5 publications
144 citations
Saint Anthony College of Nursing
Rockford, United States
3 h-index
6 publications
933 citations
University of South Carolina
Columbia, United States
3 h-index
6 publications
801 citations
1–8 of 100
19 publications · 1.9K citations
16
h-index
7 publications · 681 citations
7
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JGR · 7 publications · 530 citations
7
h-index
6 publications · 390 citations
6
h-index
5 publications · 218 citations
5
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1–5