An evolutionary stochastic ground-motion model defined by a seismological scenario and local site conditions |
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Authors: | S. Sgobba P.J. Stafford G.C. Marano C. Guaragnella |
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Affiliation: | 1. The International Telematic University UNINETTUNO, Engineering Faculty—Corso Vittorio Emanuele II, 3900186 Rome, Italy;2. Department of Civil & Environmental Engineering, Imperial College London, London SW7 2AZ, UK;3. Department of Electrics and Electronics, Technical University of Bari, Technical University of Bari, via Orabona 4, 70125 Bari, Italy;4. Department of Environmental Engineering and Sustainable Development, Technical University of Bari, viale del Turismo 10, 74100 Taranto, Italy |
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Abstract: | This paper is concerned with modeling earthquake-induced ground accelerations and the simulation of the dynamic response of linear structures through the principles of stochastic dynamics. A fully evolutionary approach, with nonstationarity both in amplitude and in frequency content, is proposed in order to define the seismic action, based on seismological information in the form of a small number of input parameters commonly available in deterministic or probabilistic seismic design situations. The signal is obtained by filtering a Gaussian white-noise. The finite duration and time-varying amplitude properties are obtained by using a suitable envelope function. By utilizing a subset of the records from the PEER-NGA strong-motion database, and time-series analysis tools extended to nonstationary processes, the key transfer-function properties, in terms of circular frequency, damping ratio and spectral intensity factor, are identified. A regression analysis is conducted for practical and flexible application of this model, in order to empirically relate the identified time-varying parameters of the filter to the characteristics defining earthquake scenarios such as magnitude, rupture distance and soil type. A validation study and a parametric investigation using elastic response spectra is also included. Results show that the final seismic model can reproduce, with satisfactory accuracy, the characteristics of acceleration records in a region, over a broad range of response periods. |
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