Title: Inverse problem in air-saturated porous media via reflected waves
Authors: Fellah, Zine El Abidine ×
Berger, S
Lauriks, Walter
Depollier, C
Chapelon, JY #
Issue Date: May-2003
Publisher: Amer inst physics
Series Title: Review of scientific instruments vol:74 issue:5 pages:2871-2879
Abstract: Direct and inverse scattering problem in air filled porous materials is solved. A simple ultrasonic reflectivity method is proposed for measuring the porosity of porous materials having a rigid frame. The proposed method is based on a temporal model of the direct and inverse scattering problem for the propagation of transient ultrasonic waves in a homogeneous isotropic slab of porous material having a rigid frame. This time domain model of wave propagation was initially introduced by the authors [Z. E. A. Fellah and C. Depollier, J. Acoust. Soc. Am. 107, 683 (2000)]. The viscous and thermal losses of the medium are described by the model devised by Johnson [D. L. Johnson, J. Koplik, and R. Dashen, J. Fluid. Mech. 176, 379 (1987)] and J. F. Allard (Chapman and Hall, London, 1993)] modified by a fractional calculus-based method applied in the time domain. The reflected acoustic wave by air filled porous media can be approximated by the reflected wave at the first interface. The expression of the reflection coefficient is reduced to a simple expression depending on porosity, tortuosity, and incidence angle. An expression of the porosity function of the tortuosity and incidence angle is obtained by solving the inverse problem. Experimental and numerical validation results of this method are presented. This method has the advantage of being rapid and efficient. (C) 2003 American Institute of Physics.
ISSN: 0034-6748
Publication status: published
KU Leuven publication type: IT
Appears in Collections:Soft Matter and Biophysics
× corresponding author
# (joint) last author

Files in This Item:

There are no files associated with this item.

Request a copy


All items in Lirias are protected by copyright, with all rights reserved.

© Web of science