A single-sided homogeneous Green's function representation for holographic imaging, inverse scattering, time-reversal acoustics and interferometric Green's function retrieval

Journal Article (2016)
Author(s)

K. Wapenaar (TU Delft - Applied Geophysics and Petrophysics)

J. Thorbecke (TU Delft - Applied Geophysics and Petrophysics)

Joost Van Der Neut (TU Delft - Applied Geophysics and Petrophysics)

Research Group
Applied Geophysics and Petrophysics
Copyright
© 2016 C.P.A. Wapenaar, J.W. Thorbecke, J.R. van der Neut
DOI related publication
https://doi.org/10.1093/gji/ggw023
More Info
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Publication Year
2016
Language
English
Copyright
© 2016 C.P.A. Wapenaar, J.W. Thorbecke, J.R. van der Neut
Research Group
Applied Geophysics and Petrophysics
Issue number
1
Volume number
205
Pages (from-to)
531-535
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Abstract

Green's theorem plays a fundamental role in a diverse range of wavefield imaging applications, such as holographic imaging, inverse scattering, time-reversal acoustics and interferometric Green's function retrieval. In many of those applications, the homogeneous Green's function (i.e. the Green's function of the wave equation without a singularity on the right-hand side) is represented by a closed boundary integral. In practical applications, sources and/or receivers are usually present only on an open surface, which implies that a significant part of the closed boundary integral is by necessity ignored. Here we derive a homogeneous Green's function representation for the common situation that sources and/or receivers are present on an open surface only. We modify the integrand in such a way that it vanishes on the part of the boundary where no sources and receivers are present. As a consequence, the remaining integral along the open surface is an accurate single-sided representation of the homogeneous Green's function. This single-sided representation accounts for all orders of multiple scattering. The new representation significantly improves the aforementioned wavefield imaging applications, particularly in situations where the first-order scattering approximation breaks down.