Hi All,
You may remember that there was a discussion a=20
while back concerning the signal delays produced by the filter circuits used=
in=20
seismic amplifiers.
After waiting patiently for any figures to be=20
produced, I eventually gave up and plugged the filter components shown on th=
e=20
circuit diagrams of two of Larry's amplifiers into experimenter board. I the=
n=20
made some approximate measurements for the characteristics and the signal=20
delays. I have put approx. after readings of less that - 30 dB, since t=
he=20
signals had a significant noise component from the opamp chains.
The capacitors were selected from a 5% polyeste=
r=20
range. I used a Wayne Kerr FG3 Function Generator down to 0.01 Hz and a Phil=
ips=20
PM3217 dual beam oscilloscope. I also checked the frequency calibration of t=
he=20
Function Generator with a counter timer. The test signals used were=20
continuous wave, not 2 (or more) cycle sine wave transient signals (a signal=
=20
which starts on zero, follows a sine wave pattern for two cycles and finishe=
s on=20
zero, followed by a zero level pause).
The 'older' type of amplifier circuit used 4 of=
f=20
LF412 opamps in a 6 pole filter circuit, nominally rated at 10 Hz turnover w=
ith=20
a Butterworth characteristic. This circuit is no longer in production, but I=
am=20
sure that many are still in use.
The measured signal delay was about 60 milli se=
c at=20
1 Hz and increased to about 70 milli sec at 10 Hz.
The gains were
10 Hz -5.4 dB
15 Hz -20 dB
20 Hz -35 dB approx.
The 'newer' 1 to 3 channel type amplifier uses=20=
a=20
TL074 opamp in an 8 pole filter circuit, nominally rated at 5 Hz with a=20
Butterworth characteristic for the Lehman configuration - see
http://psn.quake.net/eqamp.html=
The measured delay was 100 milli sec at 1 Hz an=
d it=20
was very nearly constant out to 5 Hz.
The gains were
5 Hz -2.2dB
7.5 Hz -7.3 dB
10 Hz -14 dB
15 Hz -32 db approx.
The 'newer' type with the geophone configuratio=
n is=20
rated at 10 Hz with a Butterworth characteristic. The component values in=20
the panel on the circuit diagram give a 10 Hz turnover, not t=
he=20
20 Hz stated. I note that there is still considerable signal gain at 20=
Hz,=20
which may be relevant when considering environmental noise pickup at your=20
location.
The measured delay at 1 Hz was 48 milli sec and=
=20
this appeared to stay constant out to 10 Hz.
The gains were
10 Hz -2.2 dB
15 Hz -6.8 dB
20 Hz -14 dB
30 Hz -33 dB approx.
I did not find any peaks in the delay=20
characteristics of the TL074 opamp filter types at about 0.8 x the cut-off=20
frequency, as shown on Texas' FilterPro design plots for Butterworth=20
Filters. Comparing this filter output characteristic with the older 6 p=
ole=20
Butterworth filter suggests a more gradual 'roll off' and near constant sign=
al=20
delays over the passband, more characteristic of Bessel type filters.
I did not test the latest 8 pole version of the=
1=20
to 4 channel amplifier filter which uses a LF444 opamp, but I would expect t=
hem=20
to be similar. The plots of the characteristics appear to be identical.=
See=20
http://psn.quake.net/serialamp.=
html
If you are digitising several channels with the=
=20
same A/D conveter, it may be worth measuring / calculating the delay in betw=
een=20
the channel readings. Even if a conversion only takes ~20 micro seconds, the=
=20
'speed' of the digital link to the computer may need to be considered.
These signal delays are of the same order as th=
e=20
errors which may be produced in estimating the start time of the signal=
and=20
are probably not significant for most 'amateur' work. If, however, you apply=
a=20
'real' narrow band multi pole filter at about 0.5 or 1 Hz to the=20
signal to dig P & S waves out of the general background, much larger tim=
ing=20
errors can be produced. I have no information on narrow band software=20
filters.
Regards,
Chris Chapman