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If
you would like to watch other IEST presentations by Wayne
via Webex, please click on the links below:
October
15, 2002 - What is Resonance all about?
January 21, 2003 - Vibration Aspects
of Reliability Enhancement via HALT, ESS and HASS
May 6, 2003 -
Vibration Testing and Screening of PCBs
Nov 18,
2003 - Fixtures for Vibration and Shock Testing
December 9, 2003 - Resonance
can damage your hardware
Measurement
and Analysis
by Wayne Tustin
(December
3, 2002)
Hello.
Yes, this is Wayne Tustin. Sometimes I'm called "Mr. Random
Vibration," about which I'll teach in late January at
Caterpillar in Illinois and here at Santa Barbara in February.
We thank Bruel & Kjaer for this web time and the Chicago
Chapter of the Institute of Environmental Sciences and
Technology for arranging these presentations and for inviting
me today to discuss "Measurements and Analysis". |
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Here
in Figure 1, we need to decide. Shall we measure displacement?
Or velocity? Or acceleration? What do these words mean?
Visualize sitting in your car, engine off. Over time,
your trip odometer tells you that you've not moved. Your
position, your location, your displacement, hasn't
changed, black graph. Over time, your speedometer tells
you that your speed, your velocity, remains at
zero, green graph. Thus your rate of velocity change,
your acceleration, also remains at zero, red graph.
An accelerometer would confirm the latter. |
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In
Figure 2 we change the situation to unidirectional motion.
Now your car is accelerating at oh, let's say 1/10 g,
1/10 the acceleration that Sir Isaac Newton's falling
apple experienced. An accelerometer would confirm
that acceleration, graphed in red. As we consider the
passage of time, the area under the acceleration curve
increases, as plotted by the rising green velocity graph.
Your car's speedometer confirms this. The area under the
velocity curve increases even more rapidly, as plotted
by the exponential black displacement graph. Your car's
odometer confirms this. Mathematically, what have we done?
We have integrated acceleration twice. Remember
this when you connect an accelerometer to a double integrator,
making it possible for you to measure displacement or
to control the vibratory displacement of your shaker. |
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Now let's discuss classical sinusoidal
vibration, Figure 3. Instead of unidirectional motion,
we now have a motion that reverses. The time history
repeats in a period T of oh, let's say 0.1 second. We'll
talk about the frequency, f, the reciprocal of T. That
is, 10 hertz.
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Our red sine wave, low here in Figure
4, can represent that acceleration. The integral, the
area under that graph, is plotted in green, representing
velocity, also a sine wave but ¼ cycle later in time.
The integral, the area under that graph is plotted in
black, representing displacement, also a sine wave but
another ¼ cycle later in time. Let's suppose that these
graphs represent the 10 cycle per second, the 10 hertz
motion of a shaker armature moving up1/2 inch and then
down ½ inch, 1 inch peak-to-peak displacement. What
is the peak velocity?
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As
you can see, peak velocity V can be calculated by fD,
so that if we substitute 10 for f and 1 inch for D, we
see that peak velocity V =31.4 inches per second. What
is the peak acceleration A? A can be calculated by 0.0511
f2D, so that if we substitute 10 for f and
1 inch for D, we see that peak acceleration A is 5.11g,
5.11 times the acceleration of Sir Isaac Newton's famous
apple. If accuracy is not important, perhaps you can borrow
a technician's cardboard vibration calculator, such as...
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...
the unit shown here in Figure 5. Similar units are given
by Wilcoxon, Ling, MB, Wyle and other manufacturers.
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Figure
6 shows the internal construction of a "compression" style
accelerometer, attached to some structure you are studying.
If your structure drives the base upward, the seismic
mass (probably high-density tungsten) resists being accelerated.
Its inertial reaction force (Newton taught us that F =
MA) further compresses the piezoelectric element, literally
squeezing out some electrons, giving us an electrical
signal representing your structure's acceleration.
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Figure 7 shows the internal construction of a "shear"
style accelerometer, attached to some structure you
are studying. If your structure drives the base upward,
the seismic masses (probably high-density tungsten)
resist being accelerated. Their inertial reaction forces
shear the piezoelectric elements, literally squeezing
out some electrons, giving us an electrical signal representing
your structure's acceleration. We lack time, today,
to discuss other accelerometer types: piezoresistive,
capacitive, servo and others. Almost all vibration measurements
today utilize accelerometers for sensing. For simultaneous
acceleration measurements in three orthogonal directions,
you could purchase and use three accelerometers.
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Or
you could purchase and use one so-called "tri-axial"
accelerometer, as in Figure 8.
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We
utilize the broad flat frequency response (Figure 9) of
our accelerometers, found at lower frequencies. We ask,
"What is the highest forcing frequency present?"
When testing to say 2,000 Hz, the resultant chattering,
buzzing, rubbing, etc. inside our test article can reach
say 20,000 Hz. We seek an accelerometer whose natural
frequency
is 100,000 Hz or higher, so that resonant magnification
does not exceed 4%. |
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Figure
10 suggests comparison calibration, determining the
sensitivity of an "unknown" accelerometer. It is mounted
atop a "known" accelerometer whose sensitivity was previously
determined by a standards lab. Here the two accelerometers
are being vibrated by a small electrodynamic shaker.
Their electrical signals are being compared.
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How
will you attach your accelerometer to a structure you
are investigating or testing? Figure 11 shows that best
results utilize a manufactured mounting stud similar to
that used at the accelerometer factory and at calibration
labs. See sketch 6 and graph 6. Other mounting techniques
include (see sketches and graphs 5, 4, 3 and 2) adhesive,
adhesive mounting pad, flat magnet and 2-pole magnet.
Least good: the hand-held probe of sketch 1 and graph
1. Note how seriously the useable frequency range is compromised.
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On
what instrument will you display vibration quantities?
Will you display magnitude on some form of voltmeter?
Will you display the "time history" on an oscilloscope
or record it on an oscillograph? Or will you perhaps
process, store and display on a computer?
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Figure
12 shows one (of many) dedicated spectrum analyzers
for showing the frequency content of your accelerometer's
electrical signal. To a degree, it's electrical functioning
is mimicked by ...
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...
the mechanical behavior of the "mechanical spectrum
analyzer" of Figure 13. It contains a series of reeds.
Each is mechanically tuned to respond when vibrated
at the cerrtain frequency. Here we see the 1,750RPM
(29 Hz) reed responding to shaft unbalance in a motor
that is spinning at 1,750 revs per minute (29 revs per
second). H H Sticht of New York still makes these analyzers,
calling them tachometers.
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Strike
the unit with your knuckle. Now all the reeds respond,
each quivering at its own natural frequency. This suggests
that mechanical shock (in service or in a test lab)
excites all of a product's resonances. So does random
vibration. Until this video clip, we have been assuming
that vibration is single-frequency-at-a-time. Rarely,
in the "real world", is this true.
Click on the image to see this
video clip.
You will need Real Player to watch the video. Just click
here to download it for free.
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Consider
Figure 14. The sound of one piano string, struck by
a hammer, or ...
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... the sound of one plucked guitar
string, Figure 15, will be multi-frequency, since string
vibration is multi-frequency. To identify the various
frequencies and their individual magnitudes requires spectrum
analysis. You can purchase a dedicated spectrum analyzer
such as we saw in Figure12, or you can buy hardware and
software suggested by ... |
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...
Figure 16 to convert your PC into a spectrum analyzer.
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Video
clip 2, showing our mechanical spectrum analyzer resting
on the vibrating table of a shaker, conveys the idea
of a continuous spectrum with all forcing frequencies
present, as with the broad spectrum random vibration
many of us use for random vibration testing, HALT, ESS
and HASS.
Click on the image to see this
video clip.
You
will need Real Player to watch the video. Just click
here to download it for free.
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Here
are some upcoming "open" courses which you might attend.
Santa Barbara in February is not considered to be punishment!
I'm lucky to live there. While you are at this website,
please see the details of these courses by clicking
here. Or consider having us "tailor" training
to meet your needs, for presentation at your site,
as last month at Redstone Arsenal and at Daimler-Chrysler.
Details about CD-ROM training
are also shown. |
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Thanks again to B&K and to IEST! |
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