Philippe Roux

Dr. Philippe Roux

The Institute of Earth Sciences (ISTerre), Grenoble Alpes University, 38000 Grenoble, France
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Research Focus & Metrics

Academic Career Length

33Years (1994-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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3 November 2000 in Reports on Progress in Physics
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MFMathias Fink
Mathias Fink
DCDidier Cassereau
Didier Cassereau
ADArnaud Derode
Arnaud Derode
CPClaire Prada
Claire Prada
Philippe RouxPhilippe Roux
Philippe Roux
FWFrançois Wu
François Wu

26 July 2005 in Geophysical Research Letters
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KSKarim G. Sabra
Karim G. Sabra
PGPeter Gerstoft
Peter Gerstoft
Philippe RouxPhilippe Roux
Philippe Roux
WKW. A. Kuperman
W. A. Kuperman
MFMichael C. Fehler
Michael C. Fehler

15 February 2005 in Geophysical Research Letters
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Journal Article
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KSKarim G. Sabra
Karim G. Sabra
PGPeter Gerstoft
Peter Gerstoft
Philippe RouxPhilippe Roux
Philippe Roux
WKW. A. Kuperman
W. A. Kuperman
MFMichael C. Fehler
Michael C. Fehler

10 June 2016 in Scientific Reports
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ACAndrea Colombi
Andrea Colombi
DCDaniel Colquitt
Daniel Colquitt
Philippe RouxPhilippe Roux
Philippe Roux
SGSebastien Guenneau
Sebastien Guenneau
RCRichard V. Craster
Richard V. Craster
Critical concepts from three different fields, elasticity, plasmonics and metamaterials, are brought together to design a metasurface at the geophysical scale, the resonant metawedge, to control seismic Rayleigh waves. Made of spatially graded vertical subwavelength resonators on an elastic substrate, the metawedge can either mode convert incident surface Rayleigh waves into bulk elastic shear waves or reflect the Rayleigh waves creating a “seismic rainbow” effect analogous to the optical rainbow for electromagnetic metasurfaces. Time-domain spectral element simulations demonstrate the broadband efficacy of the metawedge in mode conversion while an analytical model is developed to accurately describe and predict the seismic rainbow effect; allowing the metawedge to be designed without the need for extensive parametric studies and simulations. The efficiency of the resonant metawedge shows that large-scale mechanical metamaterials are feasible, will have application and that the time is ripe for considering many optical devices in the seismic and geophysical context.

11 January 2016 in Scientific Reports
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ACAndrea Colombi
Andrea Colombi
Philippe RouxPhilippe Roux
Philippe Roux
SGSebastien Guenneau
Sebastien Guenneau
PGPhilippe Gueguen
Philippe Gueguen
RCRichard V. Craster
Richard V. Craster
We explore the thesis that resonances in trees result in forests acting as locally resonant metamaterials for Rayleigh surface waves in the geophysics context. A geophysical experiment demonstrates that a Rayleigh wave, propagating in soft sedimentary soil at frequencies lower than 150 Hz, experiences strong attenuation, when interacting with a forest, over two separate large frequency bands. This experiment is interpreted using finite element simulations that demonstrate the observed attenuation is due to bandgaps when the trees are arranged at the sub-wavelength scale with respect to the incident Rayleigh wave. The repetitive bandgaps are generated by the coupling of the successive longitudinal resonances of trees with the vertical component of the Rayleigh wave. For wavelengths down to 5 meters, the resulting bandgaps are remarkably large and strongly attenuating when the acoustic impedance of the trees matches the impedance of the soil. Since longitudinal resonances of a vertical resonator are inversely proportional to its length, a man-made engineered array of resonators that attenuates Rayleigh waves at frequency ≤10 Hz could be designed starting from vertical pillars coupled to the ground with longitudinal resonance ≤10 Hz.

4 December 1995 in Physical Review Letters
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ADArnaud Derode
Arnaud Derode
Philippe RouxPhilippe Roux
Philippe Roux
MFMathias Fink
Mathias Fink
We report the first experiments showing the reversibility of transient acoustic waves through high-order multiple scattering by means of an acoustic time-reversal mirror. A point source generates a pulse which scatters through 2000 steel rods immersed in water. The time-reversed waves are found to converge to their source and recover their original wave form, despite the high order of multiple scattering involved and the usual sensitivity to initial conditions of time-reversal processes. Surprisingly, the observed resolution was one-sixth of the theoretical limit for the mirror's aperture.