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Spectral acceleration
In seismology and earthquake engineering

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. 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, although there is normally a correlation between [short period] SA and PGA.

Some seismic hazard maps are also produced using spectral acceleration.

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See also

References

  1. Intensity Measure Type (IMT) Archived 2015-10-04 at the Wayback Machine OpenSHA, accessed 2011-04-14 http://www.opensha.org/glossary-intensityMeasureType#SA

  2. Intensity Measure Type (IMT) Archived 2015-10-04 at the Wayback Machine OpenSHA, accessed 2011-04-14 http://www.opensha.org/glossary-intensityMeasureType#SA

  3. FAQs – What is "spectral acceleration" or SA? United States Geological Survey, accessed 2011-04-14 https://earthquake.usgs.gov/learn/faq/?faqID=221

  4. FAQs – What is "spectral acceleration" or SA? United States Geological Survey, accessed 2011-04-14 https://earthquake.usgs.gov/learn/faq/?faqID=221