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Application of the POCS inversion method to cross‐borehole imaging

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dc.contributor Háskóli Íslands
dc.contributor University of Iceland
dc.contributor.author Bjarnason, Ingi Þorleifur
dc.contributor.author Menke, William
dc.date.accessioned 2019-03-04T13:12:20Z
dc.date.available 2019-03-04T13:12:20Z
dc.date.issued 1993-07
dc.identifier.citation Menke, W., & Bjarnason, I. T. (1993). Application of the POCS inversion method to cross-borehole imaging. Geophysics, 58(7), 941-948. doi:10.1190/1.1443485
dc.identifier.issn 0016-8033
dc.identifier.issn 1942-2156 (eISSN)
dc.identifier.uri https://hdl.handle.net/20.500.11815/1035
dc.description Publisher's version (útgefin grein)
dc.description.abstract Cross-borehole tomography suffers from a well-known problem of data incompleteness: the limited ray coverage dictated by the poor experimental geometry implies that certain features of the velocity field are not determined by the data. Construction of a tomographic image of the velocity field therefore requires the addition of prior constraints to the inversion. In the Fourier wavenumber domain (assuming straight-line rays), the process of adding prior constraints is equivalent to specifying unmeasured wavenumber coefficients. The projection onto convex sets (POCS) algorithm can impose physically plausible constraints that allow high quality tomographic images to be produced. Each constraint is viewed as defining a set (in function space) of images that satisfy that particular constraint. The POCS method finds one or more images in the intersection of the constraining sets, which is equivalent to finding an image that simultaneously satisfies a number of constraints including the observed data. The sets of images that we employ include: those that satisfy the data in the sense of having certain known wavenumber components, those that have bounded energy in certain unmeasured wavenumber components, those that have seismic velocity bounded everywhere (e.g., nonnegative), and those in which the velocity structure is confined to the region between the boreholes. An advantage of the POCS algorithm is that it allows both space-domain and wavenumber-domain constraints to be imposed simultaneously. In our implementation of the POCS algorithm, we make use of the fast Fourier transform to rapidly iterate between the space and Fourier-wavenumber domains. We test the method on synthetic data, and show that it significantly reduces the artifacts in the image, when compared to other methods. We then apply it to data from a cross-borehole experiment in Manitoba, Canada, that were previously studied by others. We achieve a tomographic image of the velocity field that is similar in many respects to the results of others, but which possesses fewer artifacts.
dc.description.sponsorship This work was supported by the National Science Foundation and the Office for Naval Research. This is Lamont- Doherty contribution number 5042.
dc.format.extent 941-948
dc.language.iso en
dc.publisher Society of Exploration Geophysicists
dc.relation.ispartofseries Geophysics;58(7)
dc.rights info:eu-repo/semantics/openAccess
dc.subject Jarðeðlisfræði
dc.subject Borholur
dc.subject Sneiðmyndatökur
dc.subject Reiknilíkön
dc.subject Jarðskjálftamælingar
dc.title Application of the POCS inversion method to cross‐borehole imaging
dc.type info:eu-repo/semantics/article
dc.description.version Peer Reviewed
dc.identifier.journal Geophysics
dc.identifier.doi 10.1190/1.1443485
dc.contributor.department Raunvísindastofnun (HÍ)
dc.contributor.department Science Institute (UI)
dc.contributor.school Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school School of Engineering and Natural Sciences (UI)


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