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

• Seismic scale

External links

• Spectral Acceleration Hazard Map of California – for 1 sec period Archived 2015-05-11 at the Wayback Machine
• 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. Intensity Measure Type (IMT) Archived 2015-10-04 at the Wayback Machine OpenSHA, accessed 2011-04-14
2. FAQs – What is "spectral acceleration" or SA? United States Geological Survey, accessed 2011-04-14