4.3 Article

Applicability of partition approximation source locating technique for a transversely isotropic medium

Journal

EPISODES
Volume 43, Issue 4, Pages 991-1002

Publisher

GEOLOGICAL SOC KOREA
DOI: 10.18814/epiiugs/2020/020063

Keywords

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Funding

  1. Basic Research and Development of the Korean Institute of Geoscience and Mineral Resources [20-3115]
  2. Technology Advancement under the Ministry of Land, Infrastructure and Transport in Korea [20CTAP-C152888-02]
  3. National Research Council of Science & Technology (NST), Republic of Korea [20-3115] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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Microfracturing in a solid generates elastic waves, being detected in a form of acoustic emission (AE). Using an array of AE sensors, the number and the location of AE sources can be successfully monitored. Rocks usually show anisotropic mechanical, thermal, and hydraulic characteristics. Especially, many sedimentary rocks present transversely isotropic features originated from complex geological processes. If the anisotropy were not properly considered, the accuracy and precision of the AE source locating would not be guaranteed. In this study, one of the source locating techniques, called partition approximation method, was investigated to check its applicability to a transversely isotropic medium. To validate the technique quantitatively, analytic and experimental investigations were conducted. Ideal and virtual two-dimensional specimens were used to check it and as a result, the technique was capable of locating both isotropic and transversely isotropic cases, showing maximum 6.9% of error when normalized by the size of specimen. Also, pencil lead break tests on artificial transversely isotropic specimen were performed. The averaged error was measured as 7.46 mm, which was smaller than the diameter of AE sensor used. In addition, Brazilian tension tests were conducted with AE monitoring as an application of the technique.

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