An investigation into processes influencing the morphodynamics of an intertidal mudflat, the Dollard estuary, the Netherlands: I. Hydrodynamics and suspended sediment

As part of an interdisciplinary experiment, a series of measurements have b een obtained on the mudflats of the Dollard Estuary, the Netherlands. The a im was to investigate the sediment transport and accumulation processes occ urring during the covering and uncovering of the mudflats, particularly as the area was known to be ebb current dominant. Current velocity measurement s confirmed the ebb dominance, and suspended matter concentrations measured over several tidal cycles in calm weather revealed that the highest concen trations occurred at the beginning of the flood and the end of the ebb. The resulting sediment flux, however, was flood dominant. During windy weather the balance of flux changed to ebb dominance. Measurements of flee size an d settling velocity show a major organic component produced by entrainment of a thin surface layer during the early flood tide. During a windy period settling velocities in the adjacent channel together with the concentration variations showed a phase lag with water depth and velocity. The highest s ettling velocities occurred at about slack water, and there were residual e bb fluxes of suspended sediment. It is concluded that the ebb dominance of the currents is not apparent in the sediment fluxes during calm weather, bu t in periods of high winds the flux is likely to be ebb directed, except wh en diatom productivity is high. The overall response is similar to that of flood dominated mudflats. (C) 2000 Academic Press.