Vertical Accretion
Vertical Accretion is the process of sediment deposition that occurs incrementally upward on a floodplain surface during overbank flow events, distinguishing it from lateral accretion by involving vertical build-up of alluvial material perpendicular to the flow direction rather than lateral migration of channel-derived deposits.
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501
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230
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2017–2026
51
181
Marsh vertical accretion via vegetative growth
John A. Nyman, Russel J. Walters, Ronald D. DeLaune et al. · Estuarine Coastal and Shelf Science · 2006 · 420 citations
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United States Geological Survey
Reston, United States
21 h-index
56 publications
7.1K citations
Louisiana State University
Baton Rouge, United States
14 h-index
33 publications
4.6K citations

University of Wollongong
Wollongong, Australia
5 h-index
6 publications
458 citations
Duke University
Durham, United States
5 h-index
9 publications
452 citations

University of Padua
Padua, Italy
5 h-index
21 publications
497 citations

Macquarie University
Sydney, Australia
5 h-index
7 publications
369 citations
William & Mary
Williamsburg, United States
4 h-index
7 publications
878 citations
Indiana University Bloomington
Bloomington, United States
4 h-index
6 publications
599 citations
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11 publications · 717 citations
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JCR · 10 publications · 697 citations
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10 publications · 1.2K citations
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JSR · 7 publications · 732 citations
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7 publications · 1K citations
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