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contributor authorJohn F. A. Sleath
contributor authorS. Wallbridge
date accessioned2017-05-08T21:10:24Z
date available2017-05-08T21:10:24Z
date copyrightNovember 2002
date issued2002
identifier other%28asce%290733-950x%282002%29128%3A6%28228%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/41450
description abstractMeasurements are reported of sediment pickup rates from rippled beds in an oscillatory-flow water tunnel. Two maxima in pickup rate are observed in each half-cycle: The first corresponds to the sediment entrained at flow reversal, and the second occurs close to maximum flow velocity. Additionally, fluid velocities were measured with a laser doppler anemometer in the mobile layer over both rippled and plane beds. These measurements confirm the finding of Zala Flores and Sleath that the flow in the mobile layer is quasisteady at low values of the acceleration parameter
publisherAmerican Society of Civil Engineers
titlePickup from Rippled Beds in Oscillatory Flow
typeJournal Paper
journal volume128
journal issue6
journal titleJournal of Waterway, Port, Coastal, and Ocean Engineering
identifier doi10.1061/(ASCE)0733-950X(2002)128:6(228)
treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;2002:;Volume ( 128 ):;issue: 006
contenttypeFulltext


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