Questioning the applicability of soil amplification factors as defined by NEHRP (USA) in the Israel building standards

Abstract

In this study we examined the applicability of the NEHRP soil classification which is based on the VS,30 parameter and the corresponding Fa and Fv factors to correct acceleration response spectra for local site classification. We calculated acceleration response spectra (10% in 50 years) for more than 1900 sites across Israel. Computations were made for hard rock conditions and for the actual site conditions, while considering nonlinear response of the soils. Based on synthetic acceleration response spectra of real sites (using stochastic procedures), it is concluded that generalizing site classification and consequently, amplification, by means of a single parameter VS, 30 is not recommended. The geology of Israel is complex and may vary significantly over short distances. Sites of similar class, show different soil effects both in shape, amplitude and in frequency. In many cases there is no correlation between amplification and VS, and in other cases, the scatter is unacceptably high.

Share and Cite:

Zaslavsky, Y. , Shapira, A. , Gorstein, M. , Perelman, N. , Ataev, G. and Aksinenko, T. (2012) Questioning the applicability of soil amplification factors as defined by NEHRP (USA) in the Israel building standards. Natural Science, 4, 631-639. doi: 10.4236/ns.2012.428083.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] Building Seismic Safety Council (1997) National earthquake hazard reduction program (NEHRP) recommended provisions for seismic regulations for new buildings and other structures. Part 1: Provisions (FEMA 302). Building Seismic Safety Council, Washington, DC.
[2] Klimis, N.S., Margaris, B.N. and Koliopoulos, P.K. (1999) Site-dependent amplification functions and response spectra in Greece. Journal of Earthquake Engineering, 3, 237-270. doi:10.1080/13632469909350346
[3] Dobry, R., Borcherdt, R., Crouse, C.B., Idriss, I.M., Joyner, W.B., Martin, G.R., Power, M.S., Rinne, E.E. and Seed, R.B. (2000) New site coefficients and site classification system used in recent building seismic code provisions. Earthquake Engineering, 16, 41-67.
[4] Barani, A., De Ferrari, R., Ferretti, G. and Eva, C. (2008) Assessing the effectiveness of soil parameters for ground response characterization and soil classification. Earthquake Spectra, 24, 565-597. doi:10.1193/1.2946440
[5] Gallipoli, M. and Mucciarelli, M. (2009) Comparison of site classification from VS,30, VS,30 and HVSR in Italy. Bulletin of the Seismological Society of America, 99, 340-351. doi:10.1785/0120080083
[6] Zaslavsky, Y., Shapira, A., Gorstein, M., Kalmanovich, M., Giller, V., Perelman, N., Livshits, I., Giller, D. and Dan, I. (2005) Site response from ambient vibrations in the towns Lod and Ramle (Israel) and earthquake hazard assessment. Bulletin of Earthquake Engineering, 3, 355-381. doi:10.1007/s10518-005-1243-1
[7] Zaslavsky, Y., Ataev, G., Gorstein, M., Kalmanovich, M., Perelman, N. and Shapira, A. (2008a) Assessment of site specific earthquake hazard in urban areas—Case study: The town of Afula, Israel, and neighboring settlements. Bollettino Di Geofisica, Teorica and Applicata, 49, 93-108.
[8] Zaslavsky, Y., Ataev, G., Gorstein, M., Kalmanovich, M., Hofstetter, A., Perelman, N., Aksinenko, T., Giller, V., Dan, H., Giller, D., Livshits, I., Shvartsburg, A. and Shapira, A. (2008b) Microzoning of site response parameters in the towns of Dimona and Bet Shean (Israel). Bollettino Di Geofisica, Teorica and Applicata, 49, 109-130.
[9] Zaslavsky, Y., Shapira, A., Ataev, G., Gorstein, M., Aksinenko, T., Kalmanovich, M., Perelman, N. and Hofstetter, R. (2009) Using ambient noise measurements in the process of assessing earthquake hazards in urban areas: Examples from Israel. In: Miura, T. and Ikeda, Y., Eds., Earthquake engineering: New Research, Nova Science Publisher, Inc., New York, 155-218.
[10] Nakamura, Y. (1989) A method for dynamic characteristics estimation of subsurface using microtremor on the ground surface. Quarterly Report of Railway Technical Research, 30, 25-33.
[11] Theodulidis, N., Bard, P.Y., Archuleta, R. and Bouchon, M. (1996) Horizontal-to-vertical spectral ratio and geological conditions: The case of Garner valley downhole in Southern California. Bulletin of the Seismological Society of America, 86, 306-319.
[12] Reinoso, E. and Ordaz, M. (1999) Spectral amplification for Mexico City from free-field recordings. Earthquake Spectra, 15, 273-295. doi:10.1193/1.1586041
[13] Pratt, T. and Brocher, T. (2006) Site response and attenuation in the Puget Lowland, Washington state. Bulletin of the Seismological Society of America, 96, 536-552. doi:10.1785/0120040200
[14] Schnabel, P.B., Lysmer, J. and Seed, H.B. (1972) SHAKE —A computer program for earthquake response analysis of horizontal layered sites. Report. No. EERC 71-12, Earthquake Engineering Research Center, Berkeley.
[15] Joyner, W.B. (1977) A Fortran program for calculating nonlinear seismic response. Open File Report 77-671, US Geological Survey, Rolla.
[16] Shapira, A. and van Eck, T. (1993) Synthetic uniform hazard site specific response spectrum. Natural Hazard, 8, 201-215. doi:10.1007/BF00690908
[17] Boore, D.M. (1983) Stochastic simulation of high-frequency ground motions. Bulletin of the Seismological Society of America, 73, 1865-1894.
[18] Boore, D. and Atkinson, G. (1987) Stochastic prediction of ground motion and spectral response parameters at hard-rock site in eastern North America. Bulletin of the Seismological Society of America, 77, 440-467.
[19] Shapira, A. and Hofstetter, A. (1993) Source parameters and scaling relationships of earthquakes in Israel. Tectonophysics, 217, 217-226. doi:10.1016/0040-1951(93)90005-5
[20] Shapira, A. and Hofstetter, A. (2002) Seismicity parameters of seismogenic zones. http://www.seis.mni.gov.il/heb/Teken/seismicity-rprt.htm
[21] Boore, D. and. Atkinson, G. (2008) Ground-motion prediction equations for the average horizontal component of PGA, PGV, and 5%-damped PSA at spectral periods between 0.01 s and 10.0 s. Earthquake Spectra, 24, 99-138. doi:10.1193/1.2830434
[22] Campbell, K.W. and Bozorgnia Y. (2008) NGA ground motion for the mean horizontal component of PGA, PGV, PGD and 5% damped linear elastic response spectra for periods ranging from 0.01 to 10 s. Earthquake Spectra, 24, 139-171. doi:10.1193/1.2857546

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.