Discussion Overview
The discussion centers around the sensitivity of seismometers, the relationship between sensitivity and the Richter scale, and the order of magnitude of seismic background noise. It includes technical explanations, personal experiences, and inquiries about specific measurements and concepts in seismology.
Discussion Character
- Technical explanation
- Conceptual clarification
- Debate/contested
Main Points Raised
- Participants inquire about the unit of sensitivity for seismometers, specifically questioning the meaning of V/(m/sec) and its comparison to the Richter scale.
- One participant explains that V/(m/sec) refers to a "Velocity" type of sensor and provides an example of a commercial geophone's sensitivity.
- It is noted that accelerometers are used for recording strong local seismic events, with outputs expressed as a percentage of gravity, influenced by various factors such as ground type and distance from the event.
- A participant asserts that the Richter scale is not directly related to the sensitivity of seismometers and describes its historical context and limitations, mentioning the Moment magnitude scale as a more accurate alternative.
- Another participant shares personal experiences in amateur seismology, detailing the evolution of their seismic recording methods and the community of amateur seismologists.
- There is a question regarding the order of magnitude of seismic background noise, with a response indicating that it varies by location and can be influenced by man-made seismic noise.
- The participant describes their own seismic system's ability to detect environmental changes, such as approaching cold fronts and ocean wave activity.
Areas of Agreement / Disagreement
Participants express differing views on the relationship between seismometer sensitivity and the Richter scale, with no consensus reached on the implications of these measurements or the order of magnitude of seismic background noise.
Contextual Notes
Limitations in understanding the background noise level are acknowledged, as it depends on the seismometer's location and surrounding environmental factors.