Number of the records: 1  

Differentiating between artificial and natural sources of electromagnetic radiation at a seismogenic fault

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    SYSNO ASEP0564839
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDifferentiating between artificial and natural sources of electromagnetic radiation at a seismogenic fault
    Author(s) Baroň, Ivo (USMH-B) ORCID, SAI
    Koktavý, P. (CZ)
    Trčka, T. (CZ)
    Rowberry, Matthew David (USMH-B) RID, ORCID, SAI
    Stemberk, Josef (USMH-B) RID, ORCID
    Balek, Jan (USMH-B) ORCID
    Plan, L. (AT)
    Melichar, R. (CZ)
    Diendorfer, G. (AT)
    Macků, R. (CZ)
    Škarvada, P. (CZ)
    Number of authors11
    Article number106912
    Source TitleEngineering Geology. - : Elsevier - ISSN 0013-7952
    Roč. 311, DEC 20 (2022)
    Number of pages15 s.
    Languageeng - English
    CountryNL - Netherlands
    KeywordsElectromagnetic radiation ; Brittle rock strain ; Microcracking ; Seismogenic fault ; Eastern Alps
    Subject RIVDB - Geology ; Mineralogy
    OECD categoryGeology
    R&D ProjectsLM2015079 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Method of publishingOpen access
    Institutional supportUSMH-B - RVO:67985891
    UT WOS000886066300001
    EID SCOPUS85141259533
    DOI10.1016/j.enggeo.2022.106912
    AnnotationUltralow frequency (ULF) to low frequency (LF) electromagnetic radiation represents one of the most promising effects of brittle rock strain and microcracking that might be potentially helpful for short term earthquake forecasting. In this study the results of a six month monitoring campaign are presented from Obir Cave in the eastern Alps. Direct experimental observations of electromagnetic radiation have been made using a customised broadband data logger installed next to the Obir Faultthis seismogenic fault near the Periadriatic Lineament is known to be related to at least three large prehistoric earthquakes. On the basis of these measurements it has been possible to characterise a number of distinct signals: artificial constant narrowband signals at discrete frequencies, short serial broadband impulses, high energy broadband impulses, and low energy broadband im-pulses. The narrowband artificial signals were removed from the electromagnetic radiation time series analysis so that the natural signals were enhanced and could be compared more easily to meteorological parameters and rock strain indicators. Critically, the high energy broadband impulses show a strong correlation with lightning activity across much of central Europe and the eastern Mediterranean while the low energy broadband impulses appear to be associated with local rock strain in and around Obir Cave. Unfortunately, it seems certain that some of the essential strain related impulses are likely to have been overprinted by the larger lightning related impulses.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2023
    Electronic addresshttps://www.sciencedirect.com/science/article/pii/S0013795222003970
Number of the records: 1  

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