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2012 Proceedings - International Tissue Elasticity Conference

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085 SUB–WAVELENGTH RESOLUTION IN SHEAR WAVE IMAGING: THE TIME REVERSAL<br />

APPROACH.<br />

Stefan Catheline 1 , Rémi Souchon 1 , Jean–Yves Chapelon 1 .<br />

1 INSERM U1032, University of Lyon, Lyon, France.<br />

Background: When a wave field is measured within the propagative medium, for instance in seismology,<br />

magnetic resonance elastography (MRE) or ultrasound (US) based elastography, it is known that, the<br />

resolution is ultimately limited by the measuring point density and not the wavelength [1]. Indeed, in<br />

contrast with far field conventional imaging systems, in situ measurement enables the retrieval of the<br />

near field details needed for super resolution. From a time reversal interpretation point of view, because<br />

of diffraction, even if the source is point–like, the wave refocuses on a spot size that cannot be smaller<br />

than half a wavelength except in the presence of an acoustic sink. The acoustic sink plays the inverse<br />

role of a source: it absorbs the energy of an incoming wave. Thus surpassing the diffraction limit for<br />

imaging implies that the acoustic sink can be recreated.<br />

Aims: Here we report numerical and experimental results obtained with a passive acoustic sink where a<br />

focal spot size only depends on the spatial sampling of the field.<br />

Methods: The experiment is as follows: in the first step, a diffuse wave field is created inside the sample<br />

by random finger impacts given from the surface for 10 seconds. The 2D displacement field is then<br />

measured inside the soft solid using speckle tracking algorithms developed in elastography. It involves a<br />

64 channel array working at 5MHz with a repetition frequency of 2000Hz. In the second step, the<br />

displacement at one point chosen as a virtual source is correlated to the other points of the image in<br />

order to compute a time reversal field in the computer. In the third and last step, the decomposition of<br />

the time reversal field into the causal and anticausal Green’s function is computed from a spatial Fourier<br />

transform. Thus, these functions imply the existence of a source and a sink respectively that both<br />

overcome the diffraction limit.<br />

Results: The refocusing spots issued from the Green' s function retrieval are compared to time reversal,<br />

Figure 1. The effect of the windowing inherent to the imaging technique of elastography on the Fourier<br />

transform will be discussed. Although no new information is brought by this approach, it is shown that<br />

imaging with an evanescent wave is possible and that it conserves the symmetry properties of the source.<br />

Conclusions: So the conclusion is that, in the absence of noise in the data, the tomography resolution of<br />

the in situ imaging technique depends only on the spatial sampling of the field inside the medium of<br />

propagation; in MRE it depends on the MR image, in US elastography on the sonogram and in seismology<br />

on the distance between geophones and not on the shear and Rayleigh wavelength, respectively.<br />

Figure 1: Focus spots along x and z directions are obtained from time reversal. They are compared to the anticausal<br />

Green's function (TR+passive sink). The size of the focus spot depends only on the spatial sampling of the<br />

field.<br />

Reference:<br />

[1] Tanter et al.: Médecine Nucléaire, 31 , pp. 132–141, 2007.<br />

indicates Presenter 103

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