Počet záznamů: 1  

Power spectra of quarry blasting works measured in different depths

  1. 1.
    SYSNO ASEP0539568
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevPower spectra of quarry blasting works measured in different depths
    Tvůrce(i) Kaláb, Zdeněk (UGN-S) RID
    Lyubushin, A. A. (RU)
    Celkový počet autorů2
    Zdroj.dok.Acta Montanistica Slovaca. - : Technická univerzita v Košiciach - ISSN 1335-1788
    Roč. 25, č. 3 (2020), s. 302-309
    Poč.str.8 s.
    Forma vydáníOnline - E
    Jazyk dok.eng - angličtina
    Země vyd.SK - Slovensko
    Klíč. slovaseismic measurement ; power spectrum ; spectral time-frequency ; diagram
    Vědní obor RIVDC - Seismologie, vulkanologie a struktura Země
    Obor OECDEnvironmental and geological engineering, geotechnics
    Způsob publikováníOpen access
    Institucionální podporaUGN-S - RVO:68145535
    UT WOS000642070300004
    EID SCOPUS85101181643
    DOI10.46544/AMS.v25i3.4
    AnotaceVibrations generated by quarry blasting are the most intensive manifestation of technical seismicity. Comparative measurements of vibrations from blasting generated in open-pit mines were performed in the Jeroným Mine near Čistá (Czech Republic). A detailed evaluation of vibrations on underground spaces is very important here because this mine is a significant heritage site of medieval tin mining. The distance between the nearest feldspathic quarry named Krásno and the Jeroným Mine is 4.7 km east, Vítkov quarries (granite) is located north in the distance of 6.3 km. Maximum values from the nearest quarry Krásno are usually within the range of 10-3 – 10-2 mm.s-1. Prevailing frequency range of recorded waves is 1 - 6 Hz for both quarries.
    To qualify seismic loading of mine, one seismic station was located on the surface, the second one in the mine at a depth of about 30 m. Power spectra could be used for distinguishing, but the difference in spectra shapes is rather evident. Especially the difference is most explicit for the frequency range 70 - 100 Hz between power spectra of surface and underground records. Fitted trends were calculated for the mentioned frequency range of power spectra. Spectral time-frequency diagrams were also defined.
    PracovištěÚstav geoniky
    KontaktLucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354
    Rok sběru2021
    Elektronická adresahttps://actamont.tuke.sk/pdf/2020/n3/4kalab.pdf
Počet záznamů: 1  

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