SUMMARY
The sensitivity of a seismometer is measured in units of V/(m/sec) or V/in/sec, indicating the voltage output per unit of velocity. For example, a commercial geophone with a 4.5Hz resonant frequency has a sensitivity of 0.810V/in/sec. The Richter scale, often misrepresented in media, measures the peak movement on a seismogram and is limited to local events within approximately 100km. Modern evaluations of earthquake magnitude utilize the Moment magnitude scale, which more accurately reflects the energy released during seismic events.
PREREQUISITES
- Understanding of seismometer sensitivity units (V/(m/sec), V/in/sec)
- Familiarity with the Richter scale and its limitations
- Knowledge of Moment magnitude scale for earthquake evaluation
- Basic concepts of seismic background noise and its variability
NEXT STEPS
- Research the principles of seismometer sensitivity and calibration techniques
- Study the differences between the Richter scale and Moment magnitude scale
- Explore methods for measuring seismic background noise in various environments
- Investigate the design and functionality of modern digital seismographs
USEFUL FOR
Seismologists, geophysicists, amateur seismology enthusiasts, and anyone interested in understanding earthquake measurement and seismometer technology.