Peak ground acceleration (PGA) is the maximum
acceleration of the ground by earthquake. However, the acceleration in the
structure is higher because of dynamic
amplification. In fact, for an average building the acceleration could be
increased up to 2.5 to 3.0 PGA (Melbourne). Rigid buildings are controlled by
acceleration. PGA can be well measured using strong motion accelerometers placed close of the epicenter of the
earthquake. The response of the structure depends on the duration of the pulse
and the time history as a whole, and not just the PGA.
Peak ground velocity (PGV) gives more
information about the response of structures, being a better indicator of
damage than PGA. The difference between PGV and the velocity in the center mass
of structure is less than PGA and a, that is to say, the velocity (V) is 1.8 to
2.0 PGV. Buildings less rigid are controlled for velocity. PGV can be measured
by seismometers place far away of the
epicenter, which could be quite complex. PGV is also related to MMI
intensity and with the PGA = PGV/750 (All the values for Rock in Melbourne)
Peak ground displacement (PGD) is related to
the drift of the building. In this case, the displacement of the center mass is
1.4 to 1.5 PGD. However, it is not possible to measure directly, but could it
be calculated using advanced seismometers,
like tele-seismometers from a long distance. Flexible buildings are
controlled by displacement.
Finally, the duration of a shaking depends of
the fault size and duration of the
rupture. Nonetheless, the duration can be prolonged by features in the wave
transmission a geological site. For instance, soil could amplify the seism and
increasing the dynamic properties of the earthquake, such as this happened in
the Mexican Earthquake of 1985.
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