1146 articles – 4004 references  [version française]
HAL: hal-00563872, version 1

Short view  Export this paper
Locating a weak change using diffuse waves: Theoretical approach and inversion procedure
Rossetto V., Margerin L., Planès T., Larose E.
Journal of Applied Physics 109, 3 (2011) 034903 - http://hal.archives-ouvertes.fr/hal-00563872
Article in peer-reviewed journal
Physics/Mechanics/Acoustics
Engineering Sciences/Acoustics
Physics/Mechanics/Materials and structures in mechanics
Engineering Sciences/Mechanics/Materials and structures in mechanics
Physics/Physics/General Physics
Locating a weak change using diffuse waves: Theoretical approach and inversion procedure
Vincent Rossetto 1, Ludovic Margerin 2, Thomas Planès 3, Eric Larose 3
1:  Laboratoire de physique et modélisation des milieux condensés (LPMMC)
http://lpmmc.grenoble.cnrs.fr/
CNRS : UMR5493 – Université Joseph Fourier - Grenoble I
Maison des Magistères/CNRS 25 Av des martyrs - BP 166 38042 GRENOBLE CEDEX 9
France
2:  Institut de recherche en astrophysique et planétologie (IRAP)
CNRS : UMR5277 – Université Paul Sabatier [UPS] - Toulouse III – Observatoire Midi-Pyrénées
France
3:  Institut des sciences de la Terre (ISTerre)
http://isterre.fr/
CNRS : UMR5275 – IFSTTAR – Université de Savoie – Université Joseph Fourier - Grenoble I – INSU – OSUG – Institut de recherche pour le développement [IRD] : UR219
BP 53 38041 Grenoble cedex 9
France
Ondes et structures
We describe a time-resolved monitoring technique for heterogeneous media. Our approach is based on the spatial variations of the cross-coherence of diffuse waves acquired at fixed positions but at different dates. The technique applies to all kind of waves, provided that waveforms can be acquired with a sampling frequency much larger than the wave frequency. To locate and characterize a weak change that occurred between successive acquisitions, we use a maximum likelihood approach combined with a diffusive propagation model. We characterize this technique, locating a weak change using diffuse waves, called LOCADIFF, with the aid of numerical simulations. In several illustrative examples, we show that the change can be located with a precision of a few wavelengths and that its effective scattering cross-section can be retrieved. We investigate how the accuracy and precision of the method depends on the number of source-receiver pairs, on the time window used to compute the cross-correlation and on the errors in the propagation model. Applications can be found in nondestructive testing, seismology, radar, and sonar location.
English
2010-08-23

Journal of Applied Physics (J. Appl. Phys.)
Publisher American Institute of Physics (AIP)
ISSN 0021-8979 
international
2011-02-03
109
3
034903

acoustic wave propagation – maximum likelihood estimation – numerical analysis
43.25.Cb Macrosonic propagation, finite amplitude sound; shock waves

Project Id ANR-08-JCJC-0066 SISDIF
Attached file list to this document: 
TEX
locadiff.tex(65.4 KB)
accuracy3d-D.eps(10.4 KB)
accuracy3d-N.eps(10.7 KB)
accuracy3d-sigma.eps(10.3 KB)
accuracy3d-time-N.eps(27.3 KB)
Bayes.eps(106.1 KB)
boundary.eps(14 KB)
boundaryQ.eps(17.8 KB)
circle.eps(5.4 KB)
errorT.eps(34.1 KB)
exp1-pm3d.eps(412.5 KB)
f.eps(17.2 KB)
g.eps(17.2 KB)
Le2.eps(18.5 KB)
Le.eps(15 KB)
L.eps(14.2 KB)
logQ_-1,3_-2,2_-3,5_50.eps(3.6 MB)
logQ.eps(342.6 KB)
sensitivity.eps(189.1 KB)
simu2d_carte.eps(30.6 KB)
simu2d_waveforms.eps(99.9 KB)
PS
locadiff.ps(1.4 MB)
PDF
locadiff.pdf(692.9 KB)