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Open AccessJournal ArticleDOI

Theoretical Analysis of Model Seabed Behavior under Water Wave Excitation

Andrzej Sawicki, +2 more
- 01 Jun 2015 - 
- Vol. 37, Iss: 2, pp 33-37
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TLDR
Theoretical analysis of the behavior of a model seabed subjected to water wave excitation is presented in this article, which is based on the classical soil mechanics, including the Biot type approach.
Abstract
Abstract Theoretical analysis of the behavior of a model seabed subjected to water wave excitation is presented. The experiments were performed in the wave flume at the Danish Technological University in Lyngby. Such experiments are unique in engineering sciences and therefore provide unique empirical data for testing various models of the seabed. A controversial explanation of the experiments is presented in the literature. The goal of this research was to study pore pressure changes caused by water waves and the subsequent liquefaction of the seabed. The authors of the present contribution offer their own theoretical explanation of the wave flume experiments and discuss errors found in the literature cited. The analysis is based on the classical soil mechanics, including the Biot type approach

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References
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Book

The mechanics of scour in the marine environment

TL;DR: Scour Below Pipelines Scour around a single slender pile Scour Around a Group of Slender Piles Examples of More Complex Configurations ScourAround Large Piles Scouraround Breakwaters Scour at Seawalls Ship-Propeller Scour Impact of Liquefaction
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On the response of a poro-elastic bed to water waves

TL;DR: In this article, the problem of the response of a porous elastic bed to water waves is treated analytically on the basis of the three-dimensional consolidation theory of Biot (1941).
Journal ArticleDOI

Residual liquefaction of seabed under standing waves

TL;DR: In this article, the results of an experimental study of the seabed liquefaction under standing waves were presented, and the experimental results imply that this transport is caused by a diffusion mechanism with a diffusion coefficient equal to the coefficient of consolidation.
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