The seismic intensity is announced by Japan Meteorological Agency based on the value of the instrumental seismic intensity. The instrumental seismic intensity is determined by using a special filter, whose amplification characteristics are similar to those of the frequency response function determining the relative velocity response of a single-degree-of-freedom (SDOF) system subjected to earthquake ground motion. Accordingly, new seismic intensity can be proposed on the basis of the velocity response of a SDOF system under seismic excitation. In the present study, this new seismic intensity is called by “velocity response seismic intensity” (
IVR). The correspondence between the velocity response seismic intensity and the instrumental seismic intensity was recognized by comparing two kinds of seismic intensity calculated from 515 strong ground motion records of the seismographs of K-NET and KiK-net by National Research Institute for Earth Science and Disaster Prevention. By changing the natural frequency
fn (originally 0.7 Hz) of a SDOF system, the short-period velocity response seismic intensity
IVRS (
fn=3.333 Hz) and the long-period velocity response seismic intensity
IVRL (
fn=0.1666 Hz) can be defined to know the characteristics of the strong earthquake ground motion in other frequency ranges. It was found that the befalling of earthquake-induced sediment disasters has a relation to the value of
IVRS. The
IVRL value was found to relate to the occurrence of the earthquake damage of oil storage tanks.
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