Abstract

This study attempts to develop empirical correlations between average penetration resistance (), averaged velocities over depth up to bedrock depth () and 30 m () for shallow depth sites (having bedrock at a depth less than 25 m). A total of 63 shallow sites were assessed for penetration resistance values up to the bedrock from Standard Penetration Tests (SPT) and dynamic soil property analysis, i.e., Shear Wave Velocity (VS) from Multichannel Analysis of Surface Waves. The study shows that 30 m averaged shear wave velocities are more than the average velocity up to bedrock depth in shallow bedrock sites because of inclusion of rock site velocity. Furthermore, averaged SPT-N() and average VS () up to bedrock depth were correlated with the 30 m average() values. This is the first attempt in developing empirical relationships of this kind for seismic site classification. These correlations can be made useful for seismic site classification of sites in regions with Standard Penetration Test (NSPT) values and limited VS values. Further surface and bedrock motion recordings of 12 selected KiK-net shallow depth sites were collected and amplifications were estimated with the respective peak ground acceleration, spectral acceleration and thereby related to the average shear wave velocity up to bedrock and 30 m. The results show that the amplification is better correlated to the than for shallow depth sites, and more data can be added to strengthen this correlation.

Highlights

  • Seismic hazard parameters at a site depend on earthquake magnitude and the distance from the focus of an earthquake, and on the topography and subsurface lithology

  • This study shows that amplification is correlatable in terms of average shear wave velocity up to bedrock (VSÀ R ) rather than 30 m average shear wave velocity (VS30 )

  • It can be seen that the two classifications do not match, since most of the sites are classified as class ‘C’ by National Earthquake Hazard Reduction Program (NEHRP)[14], whereas the classification based on average shear wave velocity results in the class ‘D’ range when same NEHRP[14] bands were considered for average shear wave velocity

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Summary

Introduction

Seismic hazard parameters at a site depend on earthquake magnitude and the distance from the focus of an earthquake, and on the topography and subsurface lithology. A generalisation of the obtained curve for each site follows the condition that the VS predicted from the regression function at the terminating depth should match the VS at the terminating depth Such regional specific methods of extrapolation, Wang and Wang [13] estimated VS30 using travel time averaged shear wave velocities (which here refered as average velocities) up to two different depths (Z1 < Z2). A total of 63 shallow depth sites from the central to eastern coastal region of the Indian peninsula (Bangalore, Coimbatore, Chennai, Vizag) were considered for this study These were classified as per National Earthquake Hazard Reduction Program (NEHRP)[14] classifications based on the predicted 30 m averaged velocity from the proposed correlations, compared with conventional site classifications based purely on the measured VS30. This study shows that amplification is correlatable in terms of average shear wave velocity up to bedrock (VSÀ R ) rather than 30 m average shear wave velocity (VS30 )

Experimental site data
Correlation for VS30 in terms of NSPTÀ R
Correlation for VS30 in terms of VSÀ R
Correlation for VSÀ R in terms of NSPTÀ R
Site classification using the proposed correlations
Amplification in shallow bedrock sites
Conclusion
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