Motion at surface of a gassy ocean sediment layer induced by obliquely incident P waves-Reference-Cited by-同舟云学术

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Motion at surface of a gassy ocean sediment layer induced by obliquely incident P waves

Published:2018-02 Issue: Volume:149 Page:95-105
ISSN:0029-8018
Container-title:Ocean Engineering
language:en
Short-container-title:Ocean Engineering

Author:

Chen Wei-Yun,Jeng Dong-Sheng,Zhao Hong-Yi,Chen Guo-Xing,Li Xiao-Jun

Funder

National Natural Science Foundation of China

Natural Science Foundation of Jiangsu Province

State Key Program of National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Ocean Engineering,Environmental Engineering

Reference32 articles.

1. Reflection transmission coefficients for a layered fluid sediment overlying a uniform solid substrate;Ainslie;J. Acoust. Soc. Am.,1996

2. A comparison between wave propagation in water-saturated and air-saturated porous materials;Albert;Appl. Phys. Lett.,1993

3. A model for wave propagation in gassy sediments;Bedford;J. Acoust. Soc. Am.,1983

4. Bulk elastic wave propagation in partially saturated porous solids;Berryman;J. Acoust. Soc. Am.,1988

5. Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range;Biot;J. Acoust. Soc. Am.,1956

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