Exploring Speed of Sound in Water with Hydrophones and Oscilloscope

In summary, the two hydrophones are close together because the water bath is only 30*16*20cm in dimension. The water bath is of metal construction, but I have wrapped the walls in bubblewrap, placed pebbles in the bottom and various bits of foam floating on top to try and minimise reflections from the container. The hydrophones are moved closer or farther to see if the waveform delay changes. It is possible to measure the delay with a signal burst that lasts only several periods @ ~100 kHz and then turns off, but this is not possible with the function generator that I have.
  • #1
cork-spotters
2
0
I hope this is applicable to this section.

Basically I have two hydrophones immersed in a water bath, approximately 12cm apart. One is connected to a function generator, the other to an oscilloscope.

I'm comparing both the transmitted and received waveforms on the scope, but I'm finding it difficult to explain my results. Basically my observed waveform is at best in phase with the input, and at high freq (~100kHz) actually leads the input signal on the scope!

Doing a basic v = s/t, and taking the accepted value of v=1482m/s, I reckon I should be getting a Δt of 80μs between the waveforms.

Have I broken physics??
 
Engineering news on Phys.org
  • #2
I doubt it.
How big is your water bath?
What material is used to construct the water bath container?
Why are your two hydrophones so close together?
Any possibility of the HF sound setting up resonance in the container itself?
Are the sound waves reflecting of the sides of the water bath?
 
  • #3
cork-spotters said:
I hope this is applicable to this section.

Basically I have two hydrophones immersed in a water bath, approximately 12cm apart. One is connected to a function generator, the other to an oscilloscope.

I'm comparing both the transmitted and received waveforms on the scope, but I'm finding it difficult to explain my results. Basically my observed waveform is at best in phase with the input, and at high freq (~100kHz) actually leads the input signal on the scope!

Doing a basic v = s/t, and taking the accepted value of v=1482m/s, I reckon I should be getting a Δt of 80μs between the waveforms.

Have I broken physics??

When sinusoidal waves are displayed on a dual-trace o'scope and they appear to be "in phase" that would mean within a few degrees of one another. Have you considered that the received waveform may be say, 355 degrees later?
 
  • Like
Likes scottdave
  • #4
The bath is approximately 30*16*20cm in dimension internally.

The water bath is of metal (stainless steel I think) construction, but I have wrapped the walls in bubblewrap, placed pebbles in the bottom and various bits of foam floating on top to try and minimise reflections from the container.

The hydrophones are close together due to the small size of the bath.

I'd hope with the padding being used that reflections wouldn't be a problem, but it is a possibility.

I'm going to measure the time delay between the two waves assuming 355* or greater phase difference to see if that explains things, but I think I tried this last week and it didn't really explain it. I'll post back with results though.

Thanks guys.
 
  • #5
cork-spotters said:
I hope this is applicable to this section.

Basically I have two hydrophones immersed in a water bath, approximately 12cm apart. One is connected to a function generator, the other to an oscilloscope.

I'm comparing both the transmitted and received waveforms on the scope, but I'm finding it difficult to explain my results. Basically my observed waveform is at best in phase with the input, and at high freq (~100kHz) actually leads the input signal on the scope!

Doing a basic v = s/t, and taking the accepted value of v=1482m/s, I reckon I should be getting a Δt of 80μs between the waveforms.

Have I broken physics??

Welcome to Physics Forums.

The wave period for ~100 kHz is only ~10 μs. A delay of 80 μs (that you calculated correctly, btw) will show up many periods later, and so be indistinguishable from a delay that is less than 1 period. Bobbywhy was pretty much on the right track, but the problem is a lot worse than being ~360°, it's more like ~8*360°.

The easy thing to try is to move the hydrophones slightly closer or farther, by a few mm, and see if the waveform delay changes by the appropriate amount. Best if you can observe the waveforms while moving the hydrophones.

Another thing to try is a much lower frequency, with a period considerably longer than 80 μs. This would mean considerably lower than 10 kHz.

If possible, try a signal burst that lasts only several periods @ ~100 kHz and then turns off, and look for when the receiver picks up the burst. May or may not be possible with the generator you have. The off time should be considerably longer than 80 μs before sending the next burst.
 
Last edited:
  • #6
Years ago, I had the telecom students build a simple TDR, Time Domain Reflectometer.
I had them create the pulse with a d flip-flop, D tied high, and -Q tied to clr.
clk is tied to a 1 khz clock. The output of Q will be about a 100 ns pulse occurring at 1 khz.
You can make the pulse longer by adding a resistor and capacitor.
Something like this should let you see your exact delay, as the pulse rep rate is much slower
than travel time.
I expect you will be able to see the secondary reflections from the sides of the tank,
but they may get lost in the general pulse dispersion.
You can increase the clock input rate to more closely match the scope scan.
have fun, sounds like an interesting experiment.
 

Related to Exploring Speed of Sound in Water with Hydrophones and Oscilloscope

What is the speed of sound in water?

The speed of sound in water varies depending on several factors such as temperature, salinity, and depth. On average, it is around 1484 meters per second, which is about four times faster than the speed of sound in air.

How does the speed of sound in water compare to the speed of sound in air?

The speed of sound in water is significantly faster than the speed of sound in air due to the higher density of water molecules. This means that sound travels much farther and quicker in water compared to air.

What factors affect the speed of sound in water?

Temperature, salinity, and depth are the main factors that affect the speed of sound in water. As water temperature and salinity increase, the speed of sound also increases. However, as depth increases, the speed of sound decreases due to the increasing pressure.

Why is the speed of sound in water important?

The speed of sound in water is important for various applications such as underwater communication, navigation, and sonar technology. Understanding the speed of sound in water is crucial for accurately measuring distances and detecting objects in the ocean.

Can the speed of sound in water be affected by human activities?

Yes, human activities such as underwater construction, shipping, and oil drilling can have an impact on the speed of sound in water. These activities can change the temperature, salinity, and pressure of the water, thereby altering the speed of sound and potentially disrupting underwater communication and navigation systems.

Similar threads

Replies
14
Views
2K
  • General Math
Replies
1
Views
792
Replies
7
Views
2K
Replies
1
Views
7K
  • Introductory Physics Homework Help
Replies
1
Views
3K
  • Introductory Physics Homework Help
Replies
12
Views
3K
  • Introductory Physics Homework Help
Replies
1
Views
2K
Replies
3
Views
3K
  • Introductory Physics Homework Help
Replies
6
Views
3K
Back
Top