Formation of a sandy near-bed transport layer from a fine-grained bed under oscillatory flow

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Formation of a sandy near-bed transport layer from a fine-grained bed under oscillatory flow

[1] Bed surface coarsening was found to be an important effect for the formation of ripples and the dynamics of the boundary layer above a predominantly silt-sized sediment bed (median particle size equal to 26 mm; 20% fine sand, 70% silt, 10% clay) under oscillatory flow (with orbital velocities of 0.32–0.52 m/s) in a laboratory wave duct. Following bed liquefaction, substantial winnowing of t...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2007

ISSN: 0148-0227

DOI: 10.1029/2006jc003635