J
John Popelish
Guest
Ken Smith wrote:
up this so called "microseism" is the test that any seismometer is
functioning. But I agree that if I can digitize faster than the 20 or
so samples needed to record the arriving waves, then I can use
multiple samples to increase my net A/D resolution.
independent of any earthquakes (a sort of crustal resonance). PickingIn article <xr2dnTBmcZF_nAzfRVn-jA@adelphia.com>,
John Popelish <jpopelish@rica.net> wrote:
[...]
For now, the seismometer application is an excuse for me to explore
the world of nonlinear transfer functions and their uses. I have
built a seismometer mechanism, and am in the process of building the
amplifier and filter electronics. I happen to already have a 10 bit
A/D serial interface for a PC.
The earth seriously rolls off any frequencies above 1KHz. If you apply a
high frequency boost to the analog signal before the digitizer and a low
pass in software land, you can easily end up with more bits in the result
than the bits in the converter.
It gives you a dithering effect for free.
It seems that the Earth provides a 6 hertz rumble that is fairly
up this so called "microseism" is the test that any seismometer is
functioning. But I agree that if I can digitize faster than the 20 or
so samples needed to record the arriving waves, then I can use
multiple samples to increase my net A/D resolution.