PSN-L Email List Message
Subject: Re: tin cries - dithering
From: Christopher Chapman chrisatupw@.......
Date: Mon, 22 Aug 2011 18:56:34 -0400 (EDT)
Brett Nordgren brett3nt@.............
Sent: Tue, 16 Aug 2011 18:14
Subject: Re: tin cries - dithering
Hi Chris,
****Thanks for your suggestion. I understand your=20
approach, though implementing it will be a bit difficult.
Hi Brett,
That rather depends on how you go about it !!=20
An alternative might be to fit two coils close to=20
the centre of the spring and just excite them ?=20
.
***Normally, to get a decent idea of long-period noise we=20
have to record for at least a day, and preferably several.=20
And to separate instrument noise unambiguously from true=20
ground noise we would need to record three instruments and=20
use correlation techniques to distinguish their individual=20
noise contributions. See:
leeman, Wettum and Trampert
Three-Channel Correlation Analysis: A New Technique to=20
Measure Instrumental Noise of Digitizers and Seismic Sensors"
SSA v96 n1 p258
.
***As it stands, at the lowest frequencies, the noise spectrum=20
we normally see rises smoothly as 1/f and looks almost exactly=20
like the best instruments except, of course, it's not as low. =20
It is entirely possible that some of the noise we see may be=20
true ground noise. We just don't have a quiet enough location=20
to tell without playing the correlation game, which could be=20
a pain. =20
.
You don't happen to have a well locally in which you could float the se=
ismometer?
=20
That is if you want absolute readings, but they will still=20
be variable. If you just want to check if the noise is lower,=20
you might have a reference seismometer and an experimental=20
seismometer and look at the long period noise of both ?
=20
****If anyone could suggest what is the magnitude of the=20
effect on the spring characteristics, I could at least model=20
the instrument response to such stepwise force changes.=20
Someone must have studied this and come up with some real=20
numbers.
.
You have traces of a sensor with an Annealed spring=20
and an As Supplied spring.
****Wouldn't the six-second microseisms be an effective=20
dither mechanism? They're usually large compared with=20
everything else.
I don't think so. You are using a FORCE FEEDBACK=20
SEISMOMETER ! The increase in the strain of the spring=20
may be << 1% of the indicated signal. You are trying=20
to keep the position of the mass constant with respect=20
to the frame.
How much feedback are you using?=20
Regards,
Chris
=
Brett Nordgren brett3nt@bnordgren=
..org
Sent: Tue, 16 Aug 2011 18:14
Subject: Re: tin cries - dithering
Hi Chris,
****Thanks for y=
our suggestion. I understand your
approach, though implementing it wil=
l be a bit difficult.
.
Hi Brett,
That rather depends on how you go about it !! An alternative might=
be to fit two coils close to
the centre of the spri=
ng and just excite them ?
<=
TT>.
****Normally, to get a decent idea of long-period=
noise we
have =
to record for at least a day, and preferably seve=
ral.
And=
to separate instrument noise u=
nambiguously from true <=
/TT>
ground noise we =
would need to record three instruments and
use correlation techniques to distin=
guish their individual <=
/TT>
noise contributions. See:
Sleeman, Wettum =
and Trampert
"Three-Channel C=
orrelation Analysis: A New Technique to
Measure =
Instrumental Noise of Digitizers
and Sei=
smic Sensors"
BSSA v96 n1 p258
.
.=
****As it stands=
, at the =
lowest frequencies, the =
noise spectrum
we normal=
ly see rises smoothly as 1/f and=
looks almost ex=
actly
li=
ke the best instruments except, of course, it's not as low. It =
is entirely possible that some of=
the noise we see may be<=
/FONT>
true ground noise. We just don't have a quiet enough location
=
to tell with=
out playing the correlation game, which<=
/FONT> could be
a pain.
.
You don't happen to have a well loca=
lly in which you could float the seismometer?
That is if you want absolute readings, but they will st=
ill
be v=
ariable. If you just want to check if the noise is lower, you might have a referenc=
e seismometer and an experimental
seismometer and look at the long period noise of =
both ?
<=
/FONT>
****If anyone co=
uld suggest what is the magnitude=
of the
effect on the spring characteristics, I could at least model the instrument response to such stepwise force changes.
Someone must have studied <=
FONT size=3D2>this and come up with some=
real
numbers.
.
You have traces of a sensor with an Annealed spring
and an As Supp=
lied spring.
****Wouldn't the six-second microseisms =
be an effective<=
/FONT>
dither mechanism? They're usually large compare=
d with
everything else.
.
SEISMOMET=
ER ! The increase in the strain of the sprin=
g
may be=
<< 1% of the indicated signal. You are trying
to keep th=
e position of the mass constant with respect
to the frame.
How much feedback are you using?
Regards,
=
Chris
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