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Seismic Beacon-A New Instrument for Detection of Changes in Rock Massif

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    SYSNO ASEP0584937
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleSeismic Beacon-A New Instrument for Detection of Changes in Rock Massif
    Author(s) Lukešová, Renata (USMH-B) ORCID, RID
    Málek, Jiří (USMH-B) RID, ORCID, SAI
    Number of authors2
    Article number234
    Source TitleSensors. - : MDPI
    Roč. 24, č. 1 (2024)
    Number of pages16 s.
    Publication formOnline - E
    Languageeng - English
    CountryCH - Switzerland
    Keywordsseismic beacon ; nonlinear phenomena ; harmonic seismic wave
    OECD categoryGeology
    R&D ProjectsTP01010055 GA TA ČR - Technology Agency of the Czech Republic (TA ČR)
    Method of publishingOpen access
    Institutional supportUSMH-B - RVO:67985891
    UT WOS001140346300001
    EID SCOPUS85181958381
    DOI10.3390/s24010234
    AnnotationThe seismic beacon is a new instrument that allows for the measurement of changes in a rock massif with high sensitivity. It is based on effects, which affect the propagation of harmonic seismic waves generated continuously with stable and precise frequency and amplitude. These seismic waves are registered by a system of seismic stations. The amplitude of the seismic signal is very small, and it is normally hidden in a seismic noise. Special techniques are applied to increase the signal-to-noise ratio. In 2020, the first prototype of the seismic beacon was constructed in a laboratory, and field tests were performed in 2022 and 2023. During the tests, the changes in spectral amplitude and phase of seismic waves were detected, which is interpreted as the changes in material properties. These measurements testified the basic functionality of the device. The seismic beacon has been developed primarily for the detection of critical stress before an earthquake, which is manifested by non-linear effects such as higher harmonics generation. In addition, it could be used, for example, in the detection of magma movements, groundwater level changes, changes in hydrocarbon saturation in rocks during the extraction of oil and natural gas, or the penetration of gases and liquids into the earth's crust.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2025
    Electronic addresshttps://doi.org/10.3390/s24010234
Number of the records: 1  

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