American Society of Civil Engineers


In Situ Soil-Specific Nonlinear Properties Back-Calculated from Vertical Array Records during 1995 Kobe Earthquake


by Takaji Kokusho, M.ASCE, (Prof., Dept. of Civ. Engrg., Fac. of Sci. and Engrg., Chuo Univ., 1-13-27 Kasuga, Bunkyo-ku, Tokyo, 112 Japan), Tomohiro Aoyagi, (Civ. Engr., Saitama Prefecture; formerly, Ex-Graduate Student, Chuo Univ.), and Akihiro Wakunami, (Civ. Engr., Ministry of Land and Transp.; formerly, Ex-Graduate Student, Chuo Univ.)

Journal of Geotechnical and Geoenvironmental Engineering, Vol. 131, No. 12, December 2005, pp. 1509-1521, (doi:  http://dx.doi.org/10.1061/(ASCE)1090-0241(2005)131:12(1509))

     Access full text
     Purchase Subscription
     Permissions for Reuse  

Document type: Journal Paper
Abstract: 1995 Hyogoken Nambu earthquake (Kobe earthquake) at soft soil sites near the earthquake fault zone. Spectrum ratios between ground surface and deeper levels are calculated for the main shock and associated small shocks and S-wave velocities and damping ratios in surface soil layers to best reproduce them are back-calculated by means of an inversion analysis (extended Bayesian method) assuming one-dimensional vertical horizontal shear (SH)-wave propagation. Obvious differences in S-wave velocities and damping ratios are found between the main shock and the small shocks. Clear strain-dependent modulus degradations which can be differentiated for different soil types are recognized. The degradations are essentially consistent with some of laboratory test results to date for each soil type at least for G/G0≈0.5 or larger, though for gravelly soils back-calculated values tend to show milder degradations than laboratory test results presumably due to large inclusion of fines in actual ground. Back-calculated damping ratios show essentially the same trend as in laboratory tests, although the absolute values are in most case a few percent higher in the strain range smaller than 10.-4.


ASCE Subject Headings:
Degradation
Damping
Japan
Earthquakes
Wave propagation
Seismic effects