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Bulletin of the Seismological Society of America; December 2002; v. 92; no. 8; p. 3152-3164; DOI: 10.1785/0120020009
© 2002 Seismological Society of America
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Article

Properties of Vertical Ground Motions

Igor A. Beresnev, Amber M. Nightengale and Walter J. Silva

Department of Geological and Atmospheric Sciences
Iowa State University
253 Science I
Ames, Iowa 50011-3212
beresnev{at}iastate.edu
amnight{at}iastate.edu
(I.A.B., A.M.N.)
Pacific Engineering and Analysis
311 Pomona Avenue
E1 Cerrito, California 94530
pacificengineering{at}juno.com
(W.J.S.)

Manuscript received 11 January 2002.

A typical engineering approach to developing site-specific design vertical ground motions starts with rock-outcrop horizontal motions, converts them into the vertical component using an empirical vertical-to-horizontal (V/H) ratio for response spectra, and propagates the resulting motion through the soil column as a vertically incident P wave. In the absence of data on strain-dependent soil properties in compressional deformation, strain-compatible shear-wave properties from the horizontal-component analyses are utilized. This approach makes two assumptions: (1) that the vertical motions are primarily composed of compressional waves and (2) that strain-dependent material properties in shear deformation can be extrapolated to compressional deformation. Our study deals with the empirical validation of both assumptions. First, we investigated the ratio of SV- to P-wave spectra of the vertical component of ground motions from significant recent events in California to find which wave type predominantly contributed to vertical motions, in the frequency range of 0.5-25 Hz. The results indicate that shear waves dominate the vertical motions at frequencies up to approximately 10 Hz, above which the contribution of compressional deformation is about as strong or greater. This result holds for both soil and rock sites. Second, using the data from the KiK-net borehole arrays in Japan, we estimated the nonlinearity in compressional deformation by studying P-wave amplification at variable amplitude levels. Frequency shifts and in some instances reduced amplification, compatible with the hysteretic softening type of nonlinearity known for shear waves, is found as the amplitude of compressional strain increases. A tentative curve of constrained-modulus reduction is also similar to the existing shear-modulus reduction curves.

The results of this study suggest that, for most practical applications, vertical motions can be modeled as nonvertically propagating SV waves. This could be implemented through conventional one-dimensional horizontal-component modeling using SHAKE and the application of empirical depth-dependent V/H correction factors to account for the inclined propagation path. At high frequencies, vertical motions may have to be modeled as near-vertically propagating P waves, with strain-dependent properties specifically developed for compressional deformation; however, these frequencies may be of lesser importance for design applications.




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