Experimental Plan

Linear Pulse Propagation and Dispersion

Background

Primer on dispersion in waveguides -- find out the basic physics

I. Animated experiment -- a simulation

Run the LabVIEW Virtual Instrument Mode Conditions.vi. This models a travelling wave of a certain frequency and particular direction as it travels down the acoustic waveguide. It gives a snapshot frozen in time of the wavefronts of the wave, together with three reflections from the walls. Under the 'wrong' conditions, the reflections are in no particular relation to the original wave, or to each other, and they tend each other out. Under the 'right' conditions, after two bounces, from opposing walls, the reflected wave drops onto the original wave in phase -- the wavefronts are 'in step' -- and add constructively. If the oscillations cancel each other, the wave does not propagate down the channel. If the reflections are constructive with each other, the wave does propagate down the tube.

Play with the angle, at a fixed frequency; play with the frequency, at a fixed angle.

Set up the model to give a constructive-interference solution (a propagating wave).

Hands On

II. Dispersion relations for different modes

The animated model above will have given you a pretty good idea of what you're looking for inside the waveguide -- now do it for real.

Analysis and Interpretation

Going back to experiment with revised/refined ideas

III. Phase velocity

The primer will have introduced you to the difference between phase velocity and group velocity, if you haven't already seen it in lectures in physics or engineering. Click here for an animation which shows a pulse travelling by at the group velocity, with the carrier wave travelling inside the envelope at the phase velocity.

How can you measure phase velocity, using Rover or the other microphones? You'll need to track a wave-crest, and follow it; see what time it takes to travel a measured distance.

Measure phase velocities for different modes, and for different drive-frequencies. Use the dispersion relations you found in Section I, above, and determine from them the phase speed which follows, for your mode and frequency. How does your measured value compare to the value you deduce or infer from your dispersion relation measurements? How does your measured phase velocity compare to predictions from analytic theory, starting with the dispersion formulae in the Primer.

Track your error estimates in all cases, and see whether your measurements give comparable answers, within estimated error.

IV. Group velocity

How can you measure group velocity, using Rover or the other microphones? Hint: PolyDriver.vi lets you drive not just a sine wave, but a pulse of a certain carrier frequency. And you have microphones at different distances. How fast does the pulse travel, for different carrier frequencies? Be careful to use at least 20 cycles in your pulse -- if you go shorter, you'll have larger and larger freqency content in your shorter and shorter pulses, so you will have big error bars in actual frequency, and weird effects which are part of the next section. The bandwidth of your pulses, shown in PolyDriver.vi, will be part of your error-bars on the frequency.

Start at frequencies well above the cutoff, where the dispersion-curve is nearly linear, and then work down toward the cutoff frequency. What happens when you try to propagate a pulse that has a center-frequency below the cut-off frequency? How do you explain this? Can you quantify the effect, by measuring the amplitude of your pulse as it propagates down the waveguide, for different frequencies? Can you connect this to results from the simple analytic theory in the Primer?

Compare your measured group velocities, for different centre-frequencies and different modes, to the value which you can determine from your measured dispersion relations (how is that found?). Then compare also to values found from analytic theory, for the dimensions of the lab waveguide. As always, track your error estimates, which will serve as a prediction for how closely you might expect experimental results to match theory, or the values expected from other experimental results.

V. Pulse dispersion

CoolEdit 2000 is software that does a very nice job with the SoundBlaster Card installed -- the input jack is in the back of the computer, and a stereo patch cord leads out, to make it easy for you to connect without fussing behind the computer. CoolEdit 2000 can let you look at the time/amplitude waveform, or let you visualize the spectrum evolving in time, in a time-frequency analysis. When opening a new file, to record into, use a digitization rate well above the Nyquist criterion, which is twice the highest frequency in the pulse spectrum; I use 44kS/s.

You know, from the dispersion relation, that the energy in different frequencies will travel at different group velocities. If you make a short pulse (only a few cycles, or even less if you wish to make a half-cycle pulse or an impulse), it will all at once contain a substantial range of frequencies, each travelling at it's own speed. So the pulse will unravel, or stretch out, as it propagates. Look at the shape of your pulse on the oscilloscope: as it was generated; as it appeared at different points along the waveguide using the fixed microphones.

Record the waveform from different microphones into CoolEdit 2000, and then use the menu to convert from waveform to spectrogram. Explain the shapes you see, in terms of the dispersion relations you measured above, or the analytic formulae. What is the lowest group velocity you see? You may want to make a series of rough measurements from the spectrogram and from them reconstruct the dispersion relations for each mode.

VI. Pulse compression

The experiment is ready, but the writeup is not -- ask your T.A. or Professor Marjoribanks for suggestions. Or do you need any? Hint: CoolEdit 2000 can let you record a short pulse launched in a mode, near the band-edge cutoff, and then time-reverse it to reverse the sign of the frequency chirp, and play it back into the driving speakers. This pulse will compress, as it travels, and reach optimum at the distance at which it was itself recorded.

 

 

Last revised: 12 March 2003 -- rsm