Abstract
Surface waves and cohesive sediments are part of a coupled system in which the components interact to produce extreme rates of wave attenuation and rapid resuspension of bottom sediments. A review of published literature, together with examination of new and archived data sets from Louisiana and Surinam, indicates that these interactions are of practical significance in that they 1) may govern areas of present and future erosion and accretion in open-coast environments, 2) can lead to extraordinarily high rates of sediment transport, even under relatively weak currents, and 3) result in cohesive sediment storage facilities that display both temporary and transitory characteristics.
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Wells, J.T., Kemp, G.P. (1986). Interaction of Surface Waves and Cohesive Sediments: Field Observations and Geologic Significance. In: Mehta, A.J. (eds) Estuarine Cohesive Sediment Dynamics. Lecture Notes on Coastal and Estuarine Studies, vol 14. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-4936-8_3
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DOI: https://doi.org/10.1007/978-1-4612-4936-8_3
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