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Henk M. Schuttelaars

Researcher at Delft University of Technology

Publications -  105
Citations -  2870

Henk M. Schuttelaars is an academic researcher from Delft University of Technology. The author has contributed to research in topics: Sediment transport & Sediment. The author has an hindex of 27, co-authored 99 publications receiving 2401 citations. Previous affiliations of Henk M. Schuttelaars include Utrecht University.

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Numerical Bifurcation Methods and their Application to Fluid Dynamics: Analysis beyond Simulation

TL;DR: Numerical bifurcation analysis of high-dimensional dynamical systems has been extensively studied in the literature as discussed by the authors, where the authors provide an overview of current techniques and typical applications of such problems in fluid dynamical problems.
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Sediment Trapping in Estuaries.

TL;DR: A transport decomposition is used to present processes that lead to convergent SPM transport, and trapping mechanisms that leading to ETMs at the landward limit of the salt intrusion, in the freshwater zone, at topographic transitions, and by lateral processes within the cross section are reviewed.
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The influence of channel deepening on estuarine turbidity levels and dynamics, as exemplified by the Ems estuary

TL;DR: In this paper, an exploratory, semi-analytical model is calibrated to simulate the equilibrium SPM distribution in the upper estuary during five time periods from 1965 to 2005, using archival bathymetric and tidal data.
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The Effect of Tidal Asymmetry and Temporal Settling Lag on Sediment Trapping in Tidal Estuaries

TL;DR: In this article, a 2DV model is developed to investigate the changes in relative roughness (friction) and mixing, resulting in fundamental changes in the char- acteristics of the horizontal (velocity) and vertical tides (sea surface elevation).
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Drivers of Residual Estuarine Circulation in Tidally Energetic Estuaries: Straight and Irrotational Channels with Parabolic Cross Section

TL;DR: In this paper, the authors examined the generation of residual circulation in a tidally energetic estuary with constant longitudinal salinity gradient and parabolic cross section by means of a two-dimensional cross-sectional numerical model, neglecting river runoff and Stokes drift.