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Application of the shear-tensile source model to acoustic emissions in Westerly granite

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    SYSNO ASEP0531789
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleApplication of the shear-tensile source model to acoustic emissions in Westerly granite
    Author(s) Petružálek, Matěj (GLU-S) RID, SAI, ORCID
    Jechumtálová, Zuzana (GFU-E) ORCID, RID
    Šílený, Jan (GFU-E) ORCID, RID
    Kolář, Petr (GFU-E) ORCID, RID
    Svitek, Tomáš (GLU-S) SAI, RID
    Lokajíček, Tomáš (GLU-S) RID, SAI, ORCID
    Turková, I. (CZ)
    Kotrlý, M. (CZ)
    Onysko, R. (CZ)
    Article number104246
    Source TitleInternational Journal of Rock Mechanics and Mining Sciences. - : Elsevier - ISSN 1365-1609
    Roč. 128, April (2020)
    Number of pages12 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsfracturing ; acoustic emission ; source mechanism ; shear-tensile crack ; Westerly granite
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    OECD categoryVolcanology
    Subject RIV - cooperationInstitute of Geology - Geology ; Mineralogy
    R&D ProjectsGA16-03950S GA ČR - Czech Science Foundation (CSF)
    GA18-08826S GA ČR - Czech Science Foundation (CSF)
    Method of publishingLimited access
    Institutional supportGLU-S - RVO:67985831 ; GFU-E - RVO:67985530
    UT WOS000536484200008
    EID SCOPUS85079340829
    DOI10.1016/j.ijrmms.2020.104246
    AnnotationTraditionally in seismology and in acoustic emission (AE), full moment tensor (MT) is applied as a default model of the mechanism. We present an alternative - an application of shear tensile crack (STC) source model to AEs generated by uniaxial compression loading of Westerly granite. The advantages of STC over the conventional MT are as follows: (i) contrary to the MT, the STC is physical source since it describes straight and simple fracture modes anticipated inside a loaded sample, namely the shear-slip and both of opening and closing tensile cracks, and (ii) the STC is simpler because it is described by fewer parameters (five instead of six required for an unconstrained MT), an essential feature for stabilizing the inverse problem. Better suitability of STC over MT is demonstrated by three exemplary AEs (tensile, shear, and combined). The obtained results were confirmed using a statistical analysis of 1630 reliably determined source mechanisms. The STC, as compared to the MT, provides smaller confidence regions for orientation and even smaller regions for decomposition parameters. Thus, the STC solution appeared to be substantially more useful than the MT, namely for mechanisms with a high content of non-double-couple (non-DC) component, as it allowed better distinction between tensile and shear AEs. Grain scale cracks of tension and combined source type, localized within the middle-height circumferential portion of the specimen, dominated fracturing. Azimuthal distribution of fault planes was found to be approximately uniform for all three source types. The fault dip increased with increasing content of the non-DC component. The average values were 16 degrees, 21 degrees, and 26 degrees for the tensile, combined and shear source types, respectively. The specimen failed by flaking in areas of a high AE activity. AE locations and failure mechanisms indicate a perfect confinement end-boundary conditions between the tested specimen and the loading platens.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2021
    Electronic addresshttps://www.sciencedirect.com/science/article/pii/S1365160919310263
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