Spectral acceleration

Spectral acceleration (SA) is a unit measured in g (the acceleration due to Earth's gravity, equivalent to g-force) that describes the maximum acceleration in an earthquake on an object – specifically a damped, harmonic oscillator moving in one physical dimension. This can be measured at (or specified for) different oscillation frequencies and with different degrees of damping, although 5% damping is commonly applied.[1] The SA at different frequencies may be plotted to form a response spectrum.

Ground motion hazard map for Hawaii, based on a 2% probability of exceeding 0.2 second spectral acceleration at 5 Hz in 50 years

Spectral acceleration, with a value related to the natural frequency of vibration of the building, is used in earthquake engineering and gives a closer approximation to the motion of a building or other structure in an earthquake than the peak ground acceleration value,[1][2] although there is normally a correlation between [short period] SA and PGA.[2]

Some seismic hazard maps are also produced using spectral acceleration.

See also

References
  1. Intensity Measure Type (IMT) OpenSHA, accessed 2011-04-14
  2. FAQs – What is "spectral acceleration" or SA? United States Geological Survey, accessed 2011-04-14


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