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

检波器 地质学 垂直地震剖面 质点速度 钻孔 反演(地质) 合成数据 地震学 分布式声传感 大地测量学 声学 算法 光纤传感器 计算机科学 岩土工程 电信 物理 光纤 构造学
作者
Anton Egorov,Julia Correa,Andrej Bóna,Roman Pevzner,Konstantin Tertyshnikov,Stanislav Glubokovskikh,Vladimir Puzyrev,Boris Gurevich
出处
期刊:Geophysics [Society of Exploration Geophysicists]
卷期号:83 (3): R273-R281 被引量:53
标识
DOI:10.1190/geo2017-0718.1
摘要

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.
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