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Spectral acceleration

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Spectral acceleration

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 (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.

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,[2][1] 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

External links

  • Spectral Acceleration Hazard Map of California - for 1 sec period
  • 2005 National Building Code of Canada - Spectral Acceleration Hazard Maps for various periods
  • Revision of Time-Independent Probabilistic Seismic Hazard Maps for Alaska
  • What is a ground shaking hazard map? - Includes explanations of SA and PGA

References

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