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- W2061035367 abstract "PreviousNext No AccessSEG Technical Program Expanded Abstracts 2008Mapping salt tracer penetration into the hyporheic zone with GPR attenuationAuthors: Emily HinzJohn BradfordEmily HinzBoise State UniversitySearch for more papers by this author and John BradfordBoise State UniversitySearch for more papers by this authorhttps://doi.org/10.1190/1.3059154 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail Abstract Because ground penetrating radar (GPR) attenuation is strongly dependent on effective conductivity, time‐lapse changes in attenuation should be able to be used to map conductivity changes. We tested the validity and field practicality of using surface‐based multi‐offset reflection gathers to map attenuation changes due to the introduction of a saline solution into the hyporheic zone of a mountain stream. A preliminary analysis of our GPR data revealed an unexpectedly high level of system noise in the GPR amplitudes. The noise masked the true conductivity‐induced attenuation, and only a broad conductivity trend could be discerned over portions of the GPR transects.Permalink: https://doi.org/10.1190/1.3059154FiguresReferencesRelatedDetails SEG Technical Program Expanded Abstracts 2008ISSN (print):1052-3812 ISSN (online):1949-4645Copyright: 2008 Pages: 3713 publication data© 2008 Copyright © 2008 Society of Exploration GeophysicistsPublisher:Society of Exploration Geophysicists HistoryPublished: 15 Dec 2008 CITATION INFORMATION Emily Hinz and John Bradford, (2008), Mapping salt tracer penetration into the hyporheic zone with GPR attenuation, SEG Technical Program Expanded Abstracts : 1298-1302. https://doi.org/10.1190/1.3059154 Plain-Language Summary PDF DownloadLoading ..." @default.
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