Pulse‐period – moment‐magnitude relations derived with wavelet analysis and their relevance to estimate structural deformations
Eleftheria Efthymiou, Nicos Makris
Abstract
Abstract Motivated from the quadratic dependence of peak structural displacements to the pulse period, , of pulse‐like ground motions, this paper revisits the pulse‐period – moment‐magnitude (–) relations of ground motions generated from recorded near‐source ground motions with epicentral distances, 20 km. A total of 1260 ground motions are interrogated with wavelet analysis to identify energetic acceleration pulses (not velocity pulses) and extract their optimal period, , amplitude, , phase, and number of half‐cycles, . The interrogation of acceleration records with wavelet analysis is capable of extracting shorter‐duration distinguishable pulses with engineering significance, which override the longer near‐source pulses and they are not necessarily of random character. Our wavelet analysis identified 109 pulse‐like records from normal faults, 188 pulse‐like records from reverse faults and 125 pulse‐like records from strike‐slip faults, all with epicentral distances 20 km. Regression analysis on the extracted data concluded that the same – relation can be used for pulse‐like ground motions generated either from strike‐slip faults or from dip‐slip normal faults; whereas, a different – relation is proposed for dip‐slip reverse faults. The study concludes that for the same moment magnitude, , the pulse periods of ground motions generated from strike‐slip faults are on average larger than these from reverse faults — a result that is in agreement with findings from past investigations. Most importantly, our wavelet analysis on acceleration records produces – relations with a slope that is lower than the slopes of the – relations presented by past investigators after merely fitting velocity pulses. As a result, our proposed – relations yield lower values for larger‐magnitude earthquakes (say 6), allowing for the estimation of dependable peak structural displacements that scale invariably with .