Spinning a Bucket to measure gravity with the parabolic surface of the water

In summary, the method of spinning a bucket filled with water demonstrates gravitational effects through the formation of a parabolic surface. As the bucket rotates, the water rises along the sides due to centrifugal force, creating a paraboloid shape that reflects the balance between gravitational pull and the outward force from the spin. This setup allows for a practical measurement of gravitational acceleration, as the shape of the water's surface can be analyzed to derive the gravitational constant based on the relationship between the radius of the parabola and the angular velocity of the bucket's rotation.
  • #1
Samir_Khalilullah
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Homework Statement
When a bucket full of water is being rotated, the water surface makes a parabolic shape. If we take a cross section of the surface, its slope will be related to gravitational acceleration, g. That means that we can calculate the values of g by taking the slope measurement at various points.

(see figure in the attachments...)

(A) Suppose the bucket has ω angular velocity. Find the slope of the cross-section when the distance from the center of the bucket is x. Consider the horizontal and vertical components of the forces acting on a small packet of water, a distance "x" from the center of the bucket.

The height of the water surface will remain constant when x = R √2 , where R is the radius of the bucket. This is the condition of maintaining a constant column. This provides us with a stable point to measure slope.

Now, consider a laser placed at h height directly above the point is emitting a beam vertically downwards. After reflection, it reaches the height of the laser with d horizontal distance from the source. We can get the slope from the values of d and h. And ω can be measured by finding the time it takes to rotate 20 times. These data are tabulated below, here h = 13 cm , R = 7.25 cm.

__________________________________________________________________________________________
| 20T (s) | 42.68 | 31.6 | 28.44 | 23.98 | 23.48 | 20.9 | 19.8 | 18.8 | 18.16 | 16.78 |
__________________________________________________________________________________________
| d (mm) | 11 | 20 | 26 | 30 | 40 | 51 | 56 | 65 | 70 | 85 |
__________________________________________________________________________________________

(B) Using these data, draw an appropriate linear graph and calculate the value of g.
(C) Find out the relative error of your result using the reference value.
Relevant Equations
none
I did (A) by balancing force on point p (in the figure). I found slope , tanθ = (w^2)x/g. I dont know what to do next. Pls help
 

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  • #2
hello @Samir_Khalilullah ,
:welcome: ##\qquad ## !​

Samir_Khalilullah said:
Homework Statement: When a bucket full of water is being rotated, the water surface makes a parabolic shape. If we take a cross section of the surface, its slope will be related to gravitational acceleration, g. That means that we can calculate the values of g by taking the slope measurement at various points.

(see figure in the attachments...)

(A) Suppose the bucket has ω angular velocity. Find the slope of the cross-section when the distance from the center of the bucket is x. Consider the horizontal and vertical components of the forces acting on a small packet of water, a distance "x" from the center of the bucket.

The height of the water surface will remain constant when x = R √2 , where R is the radius of the bucket. This is the condition of maintaining a constant column. This provides us with a stable point to measure slope.

Now, consider a laser placed at h height directly above the point is emitting a beam vertically downwards. After reflection, it reaches the height of the laser with d horizontal distance from the source. We can get the slope from the values of d and h. And ω can be measured by finding the time it takes to rotate 20 times. These data are tabulated below, here h = 13 cm , R = 7.25 cm.

__________________________________________________________________________________________
| 20T (s) | 42.68 | 31.6 | 28.44 | 23.98 | 23.48 | 20.9 | 19.8 | 18.8 | 18.16 | 16.78 |
__________________________________________________________________________________________
| d (mm) | 11 | 20 | 26 | 30 | 40 | 51 | 56 | 65 | 70 | 85 |
__________________________________________________________________________________________

(B) Using these data, draw an appropriate linear graph and calculate the value of g.
(C) Find out the relative error of your result using the reference value.
Relevant Equations: none

I did (A) by balancing force on point p (in the figure). I found slope , tanθ = (w^2)x/g. I dont know what to do next. Pls help

Well, perhaps you want to continue with part B :wink: ? In that case you will need a relationship between slope ##\theta## and distance ##d##.

1708515424930.png
A little geometry around point ##P## should do the trick !


PS I must say I don't understand "The height of the water surface will remain constant when x = R √2". Can you explain it ?

##\ ##
 
  • #3
Let's see your solution for part A.
 
  • #4
BvU said:
hello @Samir_Khalilullah ,
:welcome: ##\qquad ## !​



Well, perhaps you want to continue with part B :wink: ? In that case you will need a relationship between slope ##\theta## and distance ##d##.

A little geometry around point ##P## should do the trick !


PS I must say I don't understand "The height of the water surface will remain constant when x = R √2". Can you explain it ?

##\ ##
my bad, it was supposed to be R/sqrt(2). well, that means, even if i change the angular velocity, the height of the water column would remain constant
 
  • #5
BvU said:
hello @Samir_Khalilullah ,
:welcome: ##\qquad ## !​



Well, perhaps you want to continue with part B :wink: ? In that case you will need a relationship between slope ##\theta## and distance ##d##.

A little geometry around point ##P## should do the trick !


PS I must say I don't understand "The height of the water surface will remain constant when x = R √2". Can you explain it ?

##\ ##
also, after a bit of geometry, i did find the angle adjacent to h (at point P) to be 2 times theta. but i dont know how to proceed from there
 
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  • #6
Chestermiller said:
Let's see your solution for part A.
(I'm new here so i cant really write with latex, sorry)

So I balanced the forces at point P.(otherwise the height of water column would not remain same). we have centripetal acceleration (w^2)*x towards +ve x axis and gravity g at -ve y axis ( taking point P as centre). So the two forces acting along the tangent to P are ((w^2)*x)cos(theta) and gsin(theta). these forces have to be of equal magnitude. thus i find tangent , tan(theta)=(w^2)x/g
 
  • #7
Samir_Khalilullah said:
also, after a bit of geometry, i did find the angle adjacent to h (at point P) to be 2 times theta. but i dont know how to proceed from there
So you want to expresss ##d## in terms of ##\theta## and ##h##. How about a tangent?

##\LaTeX## tutorial button under lower left of edit panel. Worth the investment, and fun!

##\ ##
 
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  • #8
BvU said:
So you want to expresss ##d## in terms of ##\theta## and ##h##. How about a tangent?

##\LaTeX## tutorial button under lower left of edit panel. Worth the investment, and fun!

##\ ##
yeah i realized that. ## \tan 2 \theta = \frac d h ##. And i also know, ## \tan \theta = \frac {\omega^2 R} {g \sqrt{2}} ## . I can relate these two with $$ \tan 2 \theta = \frac {2 \tan \theta} {1 - {\tan^2 \theta}} $$ . But that would give me a complex equation. i need to get a linear equation so that i can plot this in a graph and find its slope and then find the value of g. So i need help . ( ALSO THANK YOU VERY MUCH FOR THE LATEX GUIDE)
 
Last edited:
  • #9
Samir_Khalilullah said:
But that would give me a complex equation.
Nothing that you can't handle. It's a quadratic in ##g## of the form ##Ag^2+Bg+C=0##. You know that the solution of that is $$g=\frac{-B\pm\sqrt{B^2-4AC}}{2A}.$$Throw out the solution that does not make physical sense and plot ##g## vs. order of measurement. You should get a straight horizontal line.
 
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  • #10
kuruman said:
Nothing that you can't handle. It's a quadratic in ##g## of the form ##Ag^2+Bg+C=0##. You know that the solution of that is $$g=\frac{-B\pm\sqrt{B^2-4AC}}{2A}.$$Throw out the solution that does not make physical sense and plot ##g## vs. order of measurement. You should get a straight horizontal line.
ok i did what you told .i got , $$ g = \frac {\sqrt{2} \omega^2 R \left( h + \sqrt{h^2 + d^2} \right)} {2 d} $$

now what do i do? They have given me data of "d" and "T"(from which i can get ## \omega ##). i need to plot a linear equation in the graph and estimate its slope. pls help.

data.png
 
  • #11
Use the equation you got to find 10 values of g. If you did everything right, a plot of the value you got vs. the order of the measurement (1, 2, 3,..., 10) should give you a straight horizontal line. If you don't get that, you did something wrong. Go back and check your work.
 
  • #12
kuruman said:
Use the equation you got to find 10 values of g. If you did everything right, a plot of the value you got vs. the order of the measurement (1, 2, 3,..., 10) should give you a straight horizontal line. If you don't get that, you did something wrong. Go back and check your work.
Thanks, I think I'm getting somewhere. here's the graph i got.

graph of g.png

Though I'm a bit doubtful about the result of data number 4, g can't be that high. Do i have to draw a best fit line?? everything else seems to be almost in a straight line. Or do i just have to calculate the average?
 
  • #13
I am doubtful about data point 4 too. You can ignore as long as you justify your reasons for doing so. For the remaining points, taking an average would mask a non-zero slope. Do a linear fit and see if the slope you get is within experimental error. If it's not, you have to explain what it could possibly mean.

This looks like a test with made up numbers so there is no actual experiment involved.
 
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  • #14
I am a lazy bugger and prefer to let the computer do the work :smile:
So I let it calculate ##\theta = \arctan(d/h)/2 ## and plot ##\tan\theta## as a function of ##\omega^2##:

1708538146341.png
where I consider point 4 a typo or something definitely wrong.

So I leave that out and then let it plot a trendline. Result ##\tan\theta = 0.0054 \,x -0.0065 ## (confirmed by a regression -- not that lazy, apparently).

Slope of 0.0054 should be ##\displaystyle {R\over g \sqrt 2} ## so that ##g = 9.82## m/s2

Bull's eye !!?! Too good to be true ?

So I wholeheartedly agree with
kuruman said:
This looks like a test with made up numbers so there is no actual experiment involved.

And then we can earn a meagre 0.5 points in part C:

1708540796638.png


A serious error discussion is something else ....

I have no idea what reference value is meant here. Maybe 9.81 m/s2 ?
In which case we are less than 0.1% off. :rolleyes:

##R = 0.075 ## m ; any (relative) error goes straight to ##g## (i.e. is a systematic error in the determination of ##g##). An optimistic estimate is, say 1 mm, so 1.3 %
( Not very big, this 'bucket' :smile: )

##h = 0.13 ## m ; error goes straight into ##\theta##; estimate 2 mm means 1.5% for ##g##, again a systematic error (i.e. doesn't average out but all work in the same direction in ##g##)

##d## let's assume (optimistically) errors average out...

If the systematic errors are independent, we may add them in quadrature and get 2%.
Meaning ##g = 9.8 \pm 0.2## m/s2 is what we should report.

And all that without a decent motivation for throwing out an observation that may or may not be 'in error' ...

##\ ##
 
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  • #15
BvU said:
So I leave that out and then let it plot a trendline. Result ##\tan\theta = 0.0054 \,x -0.0065 ## (confirmed by a regression -- not that lazy, apparently).

Slope of 0.0054 should be ##\displaystyle {R\over g \sqrt 2} ## so that ##g = 9.82## m/s2

With R = 7.25 cm instead of 7.50 cm, g = 9.49 m/s2. Still in the ballpark.

I like this method of getting g from the slope of a linear graph. From the wording of the problem statement, I tend to think this is the approach they want.
 
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  • #16
TSny said:
I like this method of getting g from the slope of a linear graph. From the wording of the problem statement, I tend to think this is the approach they want.
I am a purist. I believe that plots should only have directly measured quantities on the right hand side.
BvU said:
I have no idea what reference value is meant here. Maybe 9.81 m/s2 ?
For a meagre 0.5 pts, I think that "relative error" here means discrepancy $$\text{Relative error %}=\frac{\text{Plot value}-\text{Accepted value}}{\text{Accepted value}}\times 100.$$
 
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  • #17
kuruman said:
I am a purist. I believe that plots should only have directly measured quantities on the right hand side.
Me too ( a purist, that is; always disliked parity plots ). But I wonder what the righthand side of a plot is. And measured/calculated tend to contaminate frequently despite good intentions.

And I do prefer the figure in #12 over the figure in #10.

... there is the smalll matter that it's accidentally the wrong figure (with intercept 0).
The one intended is:
1708561530113.png


:smile: with a 4% different ##g## 🤔

(more work needed: discarding a point is a no-no; slope is ##0.00540\pm 0.00005##, intercept ##-0.00650\pm 0.0020## -- yes/no intercept zero, etc, etc)

##\ ##
 
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  • #18
BvU said:
Me too ( a purist, that is; always disliked parity plots ). But I wonder what the righthand side of a plot is. And measured/calculated tend to contaminate frequently despite good intentions.
I composed the message in a hurry. I meant the right hand side of the equation that is being plotted. Sorry for the confusion.

As for discarding a point collected in lab, I too was taught that it is a no-no. However, I was also advised to "plot as you go along" just in case you need to retake a measurement. Look at points 4 and 5.
4: 23.98 s, 30 mm
5: 23.48 s, 40 mm
If I were doing this experiment, I would go back and retake the two measurements just to make sure I have not accidentally discovered a hitherto unknown phase transition of water that shows up only when it is spinning at a certain frequency. (Right!)
 
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FAQ: Spinning a Bucket to measure gravity with the parabolic surface of the water

What is the basic principle behind spinning a bucket to measure gravity?

When you spin a bucket of water, the water inside forms a parabolic surface due to the combined effects of gravity and the centrifugal force. The shape of this surface can be analyzed to understand the relationship between these forces and measure the acceleration due to gravity.

How does the parabolic shape of the water surface relate to gravity?

The parabolic shape is a result of the balance between the centrifugal force pushing the water outward and the gravitational force pulling it downward. By measuring the curvature of the parabola, you can derive the acceleration due to gravity using mathematical equations that describe the forces involved.

What equations are used to relate the parabolic surface to gravity?

The primary equation used is \( z = \frac{\omega^2 r^2}{2g} \), where \( z \) is the height of the water at radius \( r \), \( \omega \) is the angular velocity of the spinning bucket, and \( g \) is the acceleration due to gravity. By measuring \( \omega \) and \( r \), and observing the height \( z \), you can solve for \( g \).

What equipment is needed to perform this experiment?

You need a bucket, water, a way to spin the bucket at a known and constant angular velocity (such as a turntable or a motor with a speed controller), and a ruler or other measuring device to measure the height of the water at different radii from the center of the bucket.

What are the potential sources of error in this experiment?

Potential sources of error include inaccuracies in measuring the angular velocity, imprecise measurements of the water's height, and external disturbances that affect the spinning motion. Ensuring a stable and consistent spin, as well as precise measurement tools, can help minimize these errors.

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