Application of the POCS inversion method to cross‐borehole imaging

dc.contributorHáskóli Íslandsen_US
dc.contributorUniversity of Icelanden_US
dc.contributor.authorBjarnason, Ingi Þorleifur
dc.contributor.authorMenke, William
dc.contributor.departmentRaunvísindastofnun (HÍ)en_US
dc.contributor.departmentScience Institute (UI)en_US
dc.contributor.schoolVerkfræði- og náttúruvísindasvið (HÍ)en_US
dc.contributor.schoolSchool of Engineering and Natural Sciences (UI)en_US
dc.date.accessioned2019-03-04T13:12:20Z
dc.date.available2019-03-04T13:12:20Z
dc.date.issued1993-07
dc.descriptionPublisher's version (útgefin grein)en_US
dc.description.abstractCross-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.en_US
dc.description.sponsorshipThis work was supported by the National Science Foundation and the Office for Naval Research. This is Lamont- Doherty contribution number 5042.en_US
dc.description.versionPeer Revieweden_US
dc.format.extent941-948en_US
dc.identifier.citationMenke, W., & Bjarnason, I. T. (1993). Application of the POCS inversion method to cross-borehole imaging. Geophysics, 58(7), 941-948. doi:10.1190/1.1443485en_US
dc.identifier.doi10.1190/1.1443485
dc.identifier.issn0016-8033
dc.identifier.issn1942-2156 (eISSN)
dc.identifier.journalGeophysicsen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11815/1035
dc.language.isoenen_US
dc.publisherSociety of Exploration Geophysicistsen_US
dc.relation.ispartofseriesGeophysics;58(7)
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectJarðeðlisfræðien_US
dc.subjectBorholuren_US
dc.subjectSneiðmyndatökuren_US
dc.subjectReiknilíkönen_US
dc.subjectJarðskjálftamælingaren_US
dc.titleApplication of the POCS inversion method to cross‐borehole imagingen_US
dc.typeinfo:eu-repo/semantics/articleen_US

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