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Application of the horizontal to vertical spectral ratio technique for estimating the site characteristics of ground motion caused by mining induced events

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The work presents an attempt of application of the horizontal-to-vertical spectral ratio (HVSR) method for estimating the local amplification of ground motion caused by mining seismic events in the Legnica Głogów Copper District. Amplifying properties of the surface layer are assessed from the ratio of amplitude spectra of the horizontal and vertical components of ground acceleration, recorded at the surface. The location of a local maximum of the ratio in the frequency band up to 8 Hz assigns the resonant frequency of the surface layer; the maximal value estimates the amplification factor at the measurement point. The spectral ratio was evaluated for 219 ground acceleration records from ten recording stations. The HVSR curves for induced seismicity turned out to be similar to the typical HVSR-s for natural earthquakes. Amplification factors estimated by the HVSR method were used to reduce the observed peak ground accelerations (PGA-s) to the bedrock. The reduction significantly improved an agreement beween the PGA values order and the order of epicentral distances. The obtained results suggest that the HVSR method can be successfully used to evaluate the local influence of the surface layer also for induced seismicity, in spite of the fact that in this case the conditions for application of the method essentially differ from the conditions met in natural seismicity.
Rocznik
Strony
301--318
Opis fizyczny
Bibliogr. 19 poz.
Twórcy
autor
  • Faculty of Geology, Geophysics and Environmental Protection, Department of Geophysics, AGH University of Science and Technology, Aleja Mickiewicza 30, 30-059 Kraków
autor
  • Faculty of Geology, Geophysics and Environmental Protection, Department of Geophysics, AGH University of Science and Technology, Aleja Mickiewicza 30, 30-059 Kraków
Bibliografia
  • 1. Ansal, A., R. lyisan and M. Ozkan, 1997, A preliminary microzonation study for the town of Dinar. In: P.S. Sêco e Pinto (ed.), "Seismic Behaviour of Ground and Geotechnical Structures", Balkema, Rotterdam, 3-9.
  • 2. Atkinson, G.M., and J.F. Cassidy, 2000, Integrated use of seismograph and strong-motion data to determine soil amplification: response of the Fraser River Delta to the Duvall and Georgia Strait earthquakes, Bull. Seismol. Soc. Am. 90, 1028-1040.
  • 3. Bard, M.P.-Y., 2002, Site effects in urban areas, Key-Note Lecture XVIII Gen. Assem. ESC, Genua, Italy 1-6.09.2002, Abstract. In: Book of Abstracts, 10.
  • 4. Diagourtas, D., A. Tzanis and K. Makropoulos, 2001, Comparative study of microtremor analysis method, Pure Appl. Geophys. 158, 2463-2479.
  • 5. Dimitriu, P.P., 2002, The HVSR technique reveals pervasive nonlinearly sediment response during the 1994 Northidge earthquake (Mw 6.7), J. Seismol. 6, 247-255.
  • 6. Dubiński, J., and G. Mutke, 1998 Mining tremors. In: "Ochrona Obiektów Budowlanych na Terenach Górniczych", Wyd. GIG, Katowice, 533-583 (in Polish).
  • 7. Dubiński, J., and K. Stec, 2002, Ground motion amplification due to near-surface strata in the light of geological and geophysical studies conducted in the Upper Silesian Coal Basin area, Publs. Inst. Geophys. Pol. Acad. Sc. M-27 (352), 91-105 (in Polish with English abstract and figure captions).
  • 8. Giampiccolo, E., S. Gresta, M. Mucciarelli, G. De Guidi and M.R. Gallipoli, 2001, Informatio on subsoil geological structure in the city of Catania (eastern Sicily) from microtremor measurements, Ann. di Geofis. 44, 1-11.
  • 9. Konno, K., and T. Ohmachi, 1998, Ground-motion characteristics estimated from spectral ratio between horizontal to vertical components of microtremor, Bull. Seismol. Soc. Am. 88,228-241.
  • 10. Lachet, C., and M.P.-Y. Bard, 1994, Numerical and theoretical investigations on the possibilities and limitations of Nakamura 's technique, J. Phys. Earth 42, 377-397.
  • 11. Lermo, J., and F.J. Chavez-Garcia, 1994, Are microtremors useful in site response evaluation? Bull. Seismol. Soc. Am. 84, 1350-1364.
  • 12. Luzon, F., Z. Al Yuncha, F.J. Sanchez-Sesma and C. Ortiz-Aleman, 2001, A numerical experiment on the horizontal to vertical spectral ratio in flat sedimentary basins, Pure Appl. Geophys. 158, 2451 -2461.
  • 13. Mirek, J., 2001, SEJS-NET: Wide area network system for ground vibration monitoring, Publs. Inst. Geophys. Pol. Acad. Sc., M-22 (310), 283-292 (in Polish with English abstract and figure captions).
  • 14. Mutke, G., and J. Dworak, 1992, Factors affecting the seismic effect of strong mining tremors on the surface structures in the Upper Silesia coal field, Publs. Inst. Geophys. Pol., Acad. Sc. M-16 (245), 115-129 (in Polish with English abstract and figure captions).
  • 15. Nakamura, Y., 1989, A method for dynamic characteristic estimation of subsurface using microtremor on the ground surface, Quart. Rep. Railway Techn. Res. Inst. (RTRI) 30,25-33.
  • 16. Nakamura, Y., 2000, Clear identification of fundamental idea of Nakamura's technique and its applications. In: Proceedings 12WCEE, 1-8.
  • 17. Nakamura, Y., and J. Saita, 1994, Characteristic of ground motion and structures around the damaged area of the Northridge earthquake by microtremor measurement, lst Prelim. Rep. Railway Tech. Res. Inst. (RTRI).
  • 18. Satoh, T., H. Kawase and S. Matsushima, 2001, Differences between site characteristics obtained from microtremors, S-waves, P-waves and codas, Bull. Seismol. Soc. Am. 91, 313-334.
  • 19. Tsuboi, S., M. Saito and Y. Ishihara, 2001, Verification of horizontal-to-vertical spectral-ratio technique for estimation of site response using borehole seismographs, Bull. Seismol. Soc. Am. 91,499-510.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0008-0011
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