I've just been gifted some old equipment. I grabbed it mostly for the very nice weather resistant metal case it was in.
On taking it apart, I find that it has a sensor, an ADXL105, and whilst it's almost 15 years old, the technology seems similar to what is used in these things today.
I wonder if the 0.2mG resolution makes it at all useful for a sensor in a seismograph?
It has an analogue output and the (analog) sensor output is 250mV per G.
I guess the output is noise limited and they quote a noise figure of 225uV/sqrt(Hz) but considering that you're going to be looking for seismic signals at the very low frequency end of the spectrum, 1/f noise is going to be far more significant isn't it?
That noise figure suggests for a DC to 10Hz bandwidth, the noise figure (0.7mV) will be at about 2.8mG. That corresponds to being tilted by 0.2 of a degree (which is significant because the device is (was) also touted as an inclinometer).
How do I calculate what the 1/f noise will be?
Some further research suggests that an earthquake is noticeable to humans at about 10 to 20 mG, so (at best) 2 orders of magnitude better than this is probably not going to be really useful.
On taking it apart, I find that it has a sensor, an ADXL105, and whilst it's almost 15 years old, the technology seems similar to what is used in these things today.
I wonder if the 0.2mG resolution makes it at all useful for a sensor in a seismograph?
It has an analogue output and the (analog) sensor output is 250mV per G.
I guess the output is noise limited and they quote a noise figure of 225uV/sqrt(Hz) but considering that you're going to be looking for seismic signals at the very low frequency end of the spectrum, 1/f noise is going to be far more significant isn't it?
That noise figure suggests for a DC to 10Hz bandwidth, the noise figure (0.7mV) will be at about 2.8mG. That corresponds to being tilted by 0.2 of a degree (which is significant because the device is (was) also touted as an inclinometer).
How do I calculate what the 1/f noise will be?
Some further research suggests that an earthquake is noticeable to humans at about 10 to 20 mG, so (at best) 2 orders of magnitude better than this is probably not going to be really useful.