Elastic full-waveform inversion of vertical seismic profile data acquired with distributed acoustic sensors

Author:

Egorov Anton1ORCID,Correa Julia2ORCID,Bóna Andrej2,Pevzner Roman2ORCID,Tertyshnikov Konstantin2,Glubokovskikh Stanislav2ORCID,Puzyrev Vladimir3ORCID,Gurevich Boris4ORCID

Affiliation:

1. Curtin University, GPO Box U1987, Perth, Australia, CO2CRC, PO Box 1182, Carlton, Australia, and Lomonosov Moscow State University, ul. Leninskiye Gory, 1, Moscow 119991, Russia..

2. Curtin University, GPO Box U1987, Perth, Australia and CO2CRC, PO Box 1182, Carlton, Australia..

3. Curtin University, GPO Box U1987, Perth, Australia..

4. Curtin University, GPO Box U1987, Perth, Australia, CO2CRC, PO Box 1182, Carlton, Australia, and CSIRO, Australian Resources Research Centre, 26 Dick Perry Avenue, Kensington, Australia..

Abstract

Distributed acoustic sensing (DAS) is a rapidly developing technology particularly useful for the acquisition of vertical seismic profile (VSP) surveys. DAS data are increasingly used for seismic imaging, but not for estimating rock properties. We have developed a workflow for estimating elastic properties of the subsurface using full-waveform inversion (FWI) of DAS VSP data. Whereas conventional borehole geophones usually measure three components of particle velocity, DAS measures a single quantity, which is an approximation of the strain or strain rate along the fiber. Standard FWI algorithms are developed for particle velocity data, and hence their application to DAS data requires conversion of these data to particle velocity along the fiber. This conversion can be accomplished by a specially designed filter. Field measurements show that the conversion result is close to vertical particle velocity as measured by geophones. Elastic time-domain FWI of a synthetic multioffset VSP data set for a vertical well shows that the inversion of the vertical component alone is sufficient to recover elastic properties of the subsurface. Application of the proposed workflow to a multioffset DAS data set acquired at the CO2CRC Otway Project site in Victoria, Australia, reveals salient subhorizontal layering consistent with the known geology of the site. The inverted [Formula: see text] model at the well location matches the upscaled [Formula: see text] log with a correlation coefficient of 0.85.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference29 articles.

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