A Laboratory Experimentation on the Interactions Between Water Waves and Soft Clay Beds
- 1 December 1984
- journal article
- research article
- Published by Taylor & Francis in Coastal Engineering in Japan
- Vol. 27 (1) , 279-291
- https://doi.org/10.1080/05785634.1984.11924393
Abstract
Wave tank experiments are conducted to measure the wave damping of water waves propagating in a constant water overlaying an underconsolidated clay bed. It is found that water waves attenuate at a maximum rate when the bottom pressure steepness is about twice the vertical gradient of shear strength of the clay bed. The wave length is also affected by the motion of the clay bed. The phenomena of soil mass transport in soft clay bed during the passage of nonlinear water waves are observed and quantified in a laboratory soil-wave tank for the first time. Also shear strength profiles and soil particle motions for several bed conditions are measured.Keywords
This publication has 16 references indexed in Scilit:
- Inverted Shear Modulus from Wave‐induced Soil MotionJournal of Geotechnical Engineering, 1985
- Numerical integration method for seabed response to water wavesInternational Journal of Soil Dynamics and Earthquake Engineering, 1983
- Physical Modeling of Sea‐Seabed InteractionsJournal of Engineering Mechanics, 1983
- On the response of a Coulomb‐damped poroelastic bed to water wavesMarine Geotechnology, 1983
- Non-linear mechanics of ocean wave interactions with sediment bedsApplied Ocean Research, 1982
- Interaction of Ocean Waves with a Soft BottomJournal of Physical Oceanography, 1980
- On the response of a poro-elastic bed to water wavesJournal of Fluid Mechanics, 1978
- Surface waves and bottom sediment responseMarine Geotechnology, 1977
- Boundary dissipation of oscillatory wavesJournal of Fluid Mechanics, 1966
- The dissipation of wave energy by bottom frictionEOS, Transactions American Geophysical Union, 1949