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DEPARTMENT OF MECHANICAL ENGINEERING COLUMBIA UNIVERSITY, NEW YORK, N. Y. 10027
Abstract
It is shown that the presence of a liquid in the pores of a plate causes a decrease in the phase velocity of both flexural and compressional motions, the effect being greatest for long waves. At the same time the motion is attenuated: the attenuation is larger in flexure than in compression, and increases with decreasing plate thickness.
Footnotes
* Currently Visiting Professor, Department of Mechanics, TechnionIsrael Institute of Technology, Haifa, and Department of Mechanical Engineering, The Ben-Gurion University of the Negev, Beersheva, Israel.
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S. HAJRA and A. MUKHOPADHYAY Reflection and refraction of seismic waves incident obliquely at the boundary of a liquid-saturated porous solid Bulletin of the Seismological Society of America, October 1, 1982; 72(5): 1509 - 1533. [Abstract] [PDF] |
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