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Information Journal Paper

Title

COMPUTATION OF EARTHQUAKE RESPONSE VIA FOURIER AMPLITUDE SPECTRA

Pages

  147-152

Abstract

 A theoretical relation is presented between the seismological Fourier amplitude spectrum and the mean squared value of the elastic RESPONSE, which is defined by Gaussian distribution. By shifting a general process to its mean value, spectrum of the mean squared value of the displacements computed from the Fourier amplitude spectrum and the real part of the relative displacement transfer function of the single-degree-of-freedom elastic oscillator. It is shown that the relation presented in this work opens the door for a better understanding of the relationship between time invariant mean squared value of linear RESPONSE of a single degree freedom system and seismological variables, such as magnitude, focal distance, and path and SOIL CONDITIONs. For illustrating the proposed theoretical relation, the mean squared values of a drift have been calculated for earthquake ground motions with different magnitude, focal distance and soil.

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  • Cite

    APA: Copy

    YAZDANI, A., & KOMACHI, Y.. (2009). COMPUTATION OF EARTHQUAKE RESPONSE VIA FOURIER AMPLITUDE SPECTRA. INTERNATIONAL JOURNAL OF ENGINEERING, 22(2 (TRANSACTIONS B: APPLICATIONS)), 147-152. SID. https://sid.ir/paper/552672/en

    Vancouver: Copy

    YAZDANI A., KOMACHI Y.. COMPUTATION OF EARTHQUAKE RESPONSE VIA FOURIER AMPLITUDE SPECTRA. INTERNATIONAL JOURNAL OF ENGINEERING[Internet]. 2009;22(2 (TRANSACTIONS B: APPLICATIONS)):147-152. Available from: https://sid.ir/paper/552672/en

    IEEE: Copy

    A. YAZDANI, and Y. KOMACHI, “COMPUTATION OF EARTHQUAKE RESPONSE VIA FOURIER AMPLITUDE SPECTRA,” INTERNATIONAL JOURNAL OF ENGINEERING, vol. 22, no. 2 (TRANSACTIONS B: APPLICATIONS), pp. 147–152, 2009, [Online]. Available: https://sid.ir/paper/552672/en

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