Accelerometers: measuring acceleration and vibrations

Traditionally, accelerations and vibrations were measured with mechanical sensors. Earthquakes are still detected with a geophone to this day, which is essentially an acceleration sensor. In these devices, a seismic vibration causes a coil to move over a magnetic core. The current generated is easy to measure.

The system is free of noise, and no better solution has been devised thus far that is able sense the small vibrations of an earthquake. An incredibly stable mechanical concept of this type is also a viable method for measuring vibrations in a building over a longer period of time.

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Featured accelerometers

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