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contributor authorTokuo Yamamoto
contributor authorShigeo Takahashi
date accessioned2017-05-08T21:08:48Z
date available2017-05-08T21:08:48Z
date copyrightJanuary 1985
date issued1985
identifier other%28asce%290733-950x%281985%29111%3A1%2862%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/40423
description abstractWave damping by wave‐soil interactions is examined quantitatively. The dispersion relation is obtained explicitly. It is found that the Coulomb friction between soil grains is by far the most important wave damping mechanism in soft soil beds, e.g., clays and silts. This mechanism is highly nonlinear owing to the dynamic softening behavior of soils. Large waves damp much quicker than small waves. Simple formulas and charts are presented for estimation of the wave damping by soil motion. Wave lengths are also modified by the bed motion by up to
publisherAmerican Society of Civil Engineers
titleWave Damping by Soil Motion
typeJournal Paper
journal volume111
journal issue1
journal titleJournal of Waterway, Port, Coastal, and Ocean Engineering
identifier doi10.1061/(ASCE)0733-950X(1985)111:1(62)
treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;1985:;Volume ( 111 ):;issue: 001
contenttypeFulltext


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