F
F. Schuurman
Researcher at Utrecht University
Publications - 17
Citations - 732
F. Schuurman is an academic researcher from Utrecht University. The author has contributed to research in topics: Meander & Beach morphodynamics. The author has an hindex of 10, co-authored 17 publications receiving 593 citations. Previous affiliations of F. Schuurman include Royal HaskoningDHV.
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Physics‐based modeling of large braided sand‐bed rivers: Bar pattern formation, dynamics, and sensitivity
TL;DR: In this paper, a physics-based morphological model for sand-bed braided rivers has been proposed to reproduce morphology and dynamics characteristic of braided river and determine the model sensitivity to generally used constitutive relations for flow and sediment transport.
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Experimental and numerical findings on the long‐term evolution of migrating alternate bars in alluvial channels
Alessandra Crosato,Alessandra Crosato,Frehiwot Beidmariam Desta,John Cornelisse,F. Schuurman,Wim S. J. Uijttewaal +5 more
TL;DR: In this paper, the authors studied the long-term evolution of alternate bars by performing two independent long-duration laboratory experiments and some numerical tests with a physics-based depth-averaged model.
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Bifurcation instability and chute cutoff development in meandering gravel-bed rivers
TL;DR: In this paper, a morphodynamic 3D model and a one-dimensional (1D) model with nodal-point relation with field observations of chute cutoffs in a meandering gravel-bed river were compared.
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Meandering channel dynamics in highly cohesive sediment on an intertidal mud flat in the Westerschelde estuary, the Netherlands
TL;DR: In this article, the effect of highly cohesive bed and bank sediment on channel inception and meander geometry and dynamics is investigated in small meandering channels of about 1 m wide on an intertidal mudflat in the Westerschelde estuary the Netherlands.
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Bar dynamics and bifurcation evolution in a modelled braided sand-bed river
TL;DR: The study shows that bar dissection due to local transverse water surface gradients is the dominant bifurcation initiation mechanism, although conversion of unit bars into compound bars dominates in the initial stage of a braided river.