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Analysis of the spatial variation of seismic waves and ground movements from smart‐1 array data
Author(s) -
Loh ChinHsiung
Publication year - 1985
Publication title -
earthquake engineering and structural dynamics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.218
H-Index - 127
eISSN - 1096-9845
pISSN - 0098-8847
DOI - 10.1002/eqe.4290130502
Subject(s) - seismometer , spatial variability , strong ground motion , seismic wave , geology , frequency domain , seismology , displacement (psychology) , geodesy , ground motion , mathematics , mathematical analysis , psychology , statistics , psychotherapist
Specially designed arrays of strong motion seismographs located near earthquake sources are required for engineering studies of the near‐source properties and the spatial variation of seismic waves. The SMART‐1 array in Taiwan provides good records for this type of study. Careful study of the observed strong motion data permits the identification of wave types, directions and apparent wave velocities. In this paper, a principal direction ratio R ( f ,α) is defined; this indicates the principal direction of the motion (along a nearly straight line) within the range 0 < R < 1. Vertical motion of the ground is also included in this study. Orbit spectrum analysis is used to verify the identification of wave directions and wave types. The spatial variation of seismic waves along the principal direction is studied. From frequency‐domain analysis, mathematical models of the spatial variation of ground displacement are developed using a wave‐number spectrum and the cross‐spectral density function between two spatial coordinates; these models in turn can provide two alternative models for the random vibration analysis of extensive structures subject to multiple point seismic excitation. The SMART‐1 array data gathered during the January 29, 1981 earthquake also are used to demonstrate calculation of the ground strains and differential movements of the array site. From time‐domain analysis, the spatial variation of seismic waves is defined for ground motion along the identified principal direction. The time variation of evolutionary spectra characterized by frequency‐dependent parameters is used for this formulation. The SMART‐1 array data again form the basis for discussion of the spatial variation of model parameters.