Sinking a cylinder with varying hole sizes

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The discussion revolves around an experiment involving a cylinder with a hole at the bottom, where the radius of the hole is varied to observe its effect on the time taken for the cylinder to submerge. The initial hypothesis suggests that the submersion time is inversely proportional to the hole size. Participants analyze the forces acting on the cylinder, including gravity, buoyancy, and drag, while emphasizing the importance of pressure differences and flow rates. Key equations such as Bernoulli's principle and the continuity equation are suggested to derive relationships between the variables involved. The conversation highlights the need to consider steady-state conditions and the changing water levels inside and outside the cylinder as critical factors in the analysis.
  • #61
haruspex said:
Right.
So now let's think about what will happen when a cylinder with a small hole is placed on the water and released. The flow through the hole will be relatively slow, so the initial behaviour will be much the same as with no hole, namely, that it will immediately sink until it displaces volume ##\frac{M}{\rho}##.
What value of y will result?
So if it displaced volume ##\frac{M}{\rho}## that means volume ##A(y-h)## equals to that, so ##y=\frac{M}{\rho A}+h##.
 
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  • #62
lloydthebartender said:
So if it displaced volume ##\frac{M}{\rho}## that means volume ##A(y-h)## equals to that,
No, ##A(y-h)## is the volume of water inside the cylinder at some later time.
What is the volume of water displaced by the cylinder when hardly any water has come through the hole?
 
  • #63
haruspex said:
No, ##A(y-h)## is the volume of water inside the cylinder at some later time.
What is the volume of water displaced by the cylinder when hardly any water has come through the hole?
Right so is it ##Ay##? Making ##y=\frac{M}{\rho A}##
 
  • #64
lloydthebartender said:
Right so is it ##Ay##? Making ##y=\frac{M}{\rho A}##
Yes. So that is in effect the initial value of y for the time taken to sink. The point is that it will take very little time to reach that depth. Only after that is the rate of sinking constrained by the rate of flow of the water through the hole.
 
  • #65
haruspex said:
Yes. So that is in effect the initial value of y for the time taken to sink. The point is that it will take very little time to reach that depth. Only after that is the rate of sinking constrained by the rate of flow of the water through the hole.
So can I do ##\frac{dy}{dt}=u##, and this with the equation of #49?
 
  • #66
lloydthebartender said:
So can I do ##\frac{dy}{dt}=u##, and this with the equation of #49?
Yes.
 
  • #67
haruspex said:
Yes.
But ##\frac{d(\frac{M}{\rho A})}{dt}=0##, right?
 
  • #68
lloydthebartender said:
But ##\frac{d(\frac{M}{\rho A})}{dt}=0##, right?
Yes, but why is that a problem? ##\frac{M}{\rho A}## is just the initial value of y.
Thereafter, ##\frac {dy}{dt}=u=\frac{a\sqrt{2gh}}{(A+a)}##.
 
  • #69
haruspex said:
Yes, but why is that a problem? ##\frac{M}{\rho A}## is just the initial value of y.
Thereafter, ##\frac {dy}{dt}=u=\frac{a\sqrt{2gh}}{(A+a)}##.
But isn't the whole term of ##\frac{M}{\rho A}## constant?
 
  • #70
lloydthebartender said:
But isn't the whole term of ##\frac{M}{\rho A}## constant?
Initial values generally are constant.
 
  • #71
haruspex said:
Initial values generally are constant.
That would mean ##\frac{a\sqrt{2gh}}{(A+a)}## would equate to 0?
haruspex said:
Thereafter, dydt=u=a√2gh(A+a)
 
  • #72
lloydthebartender said:
That would mean ##\frac{a\sqrt{2gh}}{(A+a)}## would equate to 0?
No.
You have an equation for dy/dt. This describes how y changes with time from some initial value to its final value L, the length of the cylinder.
The initial value of y (i.e. the value at t=0) is M/(ρA).
Solve the differential equation for y and plug in the initial and final values of y as the bounds on the integral of dy/dt.
 
  • #73
haruspex said:
No.
You have an equation for dy/dt. This describes how y changes with time from some initial value to its final value L, the length of the cylinder.
The initial value of y (i.e. the value at t=0) is M/(ρA).
Solve the differential equation for y and plug in the initial and final values of y as the bounds on the integral of dy/dt.
So ##t=\int u dy## with the range ##t=\int_{\frac{M}{\rho A}}^{L} u dy##.
This gives ##u(L-\frac{M}{\rho A})##
 
  • #74
lloydthebartender said:
So ##t=\int u dy## with the range ##t=\int_{\frac{M}{\rho A}}^{L} u dy##.
This gives ##u(L-\frac{M}{\rho A})##
Since u is constant, yes. (It would not be that simple otherwise.)
Now plug in the expression you found for u in post #49.
 
  • #75
haruspex said:
No.
You have an equation for dy/dt. This describes how y changes with time from some initial value to its final value L, the length of the cylinder.
The initial value of y (i.e. the value at t=0) is M/(ρA).
Solve the differential equation for y and plug in the initial and final values of y as the bounds on the integral of dy/dt.
So I got an equation for d^2 against 1/t...and experimentally this was supported. All is well except for one thing. In post #25 you say ##h## is constant. Why is this?
 
  • #76
lloydthebartender said:
So I got an equation for d^2 against 1/t...and experimentally this was supported. All is well except for one thing. In post #25 you say ##h## is constant. Why is this?
In post #22 you found that ##h=\frac m{\rho\pi r^2}##, which is constant.
Suppose it is not constant and it increases a little. Now the buoyancy exceeds the weight of the cylinder so it slows its descent. But the pressure difference at the hole is increased, increasing the rate of inflow of water and reducing h again.
 
  • #77
haruspex said:
In post #22 you found that ##h=\frac m{\rho\pi r^2}##, which is constant.
Suppose it is not constant and it increases a little. Now the buoyancy exceeds the weight of the cylinder so it slows its descent. But the pressure difference at the hole is increased, increasing the rate of inflow of water and reducing h again.
Alright I'll come back after getting everything sorted
 
  • #78
haruspex said:
In post #22 you found that ##h=\frac m{\rho\pi r^2}##, which is constant.
Suppose it is not constant and it increases a little. Now the buoyancy exceeds the weight of the cylinder so it slows its descent. But the pressure difference at the hole is increased, increasing the rate of inflow of water and reducing h again.
But #22 doesn't take into account the drag force...and surely experimentally H diminishes to 0 when submerging.
 
  • #79
lloydthebartender said:
But #22 doesn't take into account the drag force...and surely experimentally H diminishes to 0 when submerging.
Feel free to repeat the analysis taking drag into account. You may find it cannot be solved analytically, though. As I recall, it can be modeled as a reduced hole size, but that could be wrong.

h will only diminish when the water outside reaches the top of the cylinder and flows in. Total submersion will follow swiftly, so the time taken for it to reduce to zero can be ignored.
There are three phases:
1. On placing the cylinder on the surface of the water and releasing, it quickly sinks to the point where its weight is balanced by the buoyancy.
2. It sinks slowly, limited by the rate at which water can flow through the hole. In this phase, h is nearly constant.
3. The water outside reaches the top and flows in, quickly reducing the airspace inside to zero.
For the purposes of the time to sink, only the second phase is interesting. The others are too brief.
 
  • #80
haruspex said:
Feel free to repeat the analysis taking drag into account. You may find it cannot be solved analytically, though. As I recall, it can be modeled as a reduced hole size, but that could be wrong.

h will only diminish when the water outside reaches the top of the cylinder and flows in. Total submersion will follow swiftly, so the time taken for it to reduce to zero can be ignored.
There are three phases:
1. On placing the cylinder on the surface of the water and releasing, it quickly sinks to the point where its weight is balanced by the buoyancy.
2. It sinks slowly, limited by the rate at which water can flow through the hole. In this phase, h is nearly constant.
3. The water outside reaches the top and flows in, quickly reducing the airspace inside to zero.
For the purposes of the time to sink, only the second phase is interesting. The others are too brief.
Thanks I get it now. One more thing...in the Bernoulli equation am I taking two points right above and below the hole, or at the surface of water and below the hole. Because it seems to me that if ##z_{1}=z_{2}## the pressure terms would be the same?
 
  • #81
lloydthebartender said:
Thanks I get it now. One more thing...in the Bernoulli equation am I taking two points right above and below the hole, or at the surface of water and below the hole. Because it seems to me that if ##z_{1}=z_{2}## the pressure terms would be the same?
What drives the water through the hole (at a much higher speed than that at which the cylinder sinks) is a pressure difference over a short distance, from just below the hole to just above it.
The z2-z1 term in Bernoulli is the change in altitude of the flow of water. It is not quite zero here, but it is small. Most of the work the pressure difference does is in accelerating the water; only a small amount goes into lifting the water the short distance through the hole.
 
  • #82
haruspex said:
What drives the water through the hole (at a much higher speed than that at which the cylinder sinks) is a pressure difference over a short distance, from just below the hole to just above it.
The z2-z1 term in Bernoulli is the change in altitude of the flow of water. It is not quite zero here, but it is small. Most of the work the pressure difference does is in accelerating the water; only a small amount goes into lifting the water the short distance through the hole.
But how can there be a difference in the depth (h or y-h) and the height from the bottom (##z_{1}## or ##z_{2}##)?
 
  • #83
lloydthebartender said:
But how can there be a difference in the depth (h or y-h) and the height from the bottom (##z_{1}## or ##z_{2}##)?
I forget which is z1... say z is the height of the hole from some common baseline, z1 is at z-d and z2 is at z+d, where d is small.
The pressure under the hole is ##\rho g(y+d)## and above the hole it is ##\rho g(y-h-d)##.
The pressure difference is ##\rho g(h+2d)##. The height difference is 2d.
Plug all that into Bernoulli and obtain an expression for v. You will see that
terms involving d are second order, so can be ignored.
 
  • #84
haruspex said:
I forget which is z1... say z is the height of the hole from some common baseline, z1 is at z-d and z2 is at z+d, where d is small.
The pressure under the hole is ##\rho g(y+d)## and above the hole it is ##\rho g(y-h-d)##.
The pressure difference is ##\rho g(h+2d)##. The height difference is 2d.
Plug all that into Bernoulli and obtain an expression for v. You will see that
terms involving d are second order, so can be ignored.
I don't understand why the pressure above the hole is ##\rho g(y-h)##. Why isn't it ##\rho g(y)##. if ##z_{1}=z_{2}##?
 
  • #85
lloydthebartender said:
I don't understand why the pressure above the hole is ##\rho g(y-h)##. Why isn't it ##\rho g(y)##. if ##z_{1}=z_{2}##?
As I just posted, z1 and z2 are not quite equal. In the gap between them there is a large pressure gradient pushing the water up through the hole.
Above z2 not much is happening. There is a stationary column of water of height y-h-z2, so the pressure there is that height multiplied by ##\rho g##.
Similarly, each side of z1 there is little movement, so the pressure there is the same as elsewhere at that depth below the level of water outside the cylinder.

What you seem not to be grasping is the large pressure gradient through the hole, making for a substantial pressure difference over a short distance.
 
  • #86
haruspex said:
As I just posted, z1 and z2 are not quite equal. In the gap between them there is a large pressure gradient pushing the water up through the hole.
Above z2 not much is happening. There is a stationary column of water of height y-h-z2, so the pressure there is that height multiplied by ##\rho g##.
Similarly, each side of z1 there is little movement, so the pressure there is the same as elsewhere at that depth below the level of water outside the cylinder.

What you seem not to be grasping is the large pressure gradient through the hole, making for a substantial pressure difference over a short distance.
So since the pressure of water within the cylinder is equal we use (y-h)? But wouldn't that be atmospheric pressure?
 
  • #87
lloydthebartender said:
So since the pressure of water within the cylinder is equal we use (y-h)? But wouldn't that be atmospheric pressure?
I don't understand your question.

We can ignore atmospheric pressure and just deal with gauge pressure. That's because we only care about the pressure difference through the hole, and atmospheric pressure contributes equally outside and in.

The gauge pressure inside the cylinder, at its bottom, is due to the depth of water in the cylinder, y-h.
The gauge pressure just under the cylinder is the ambient pressure at that depth in the water outside the cylinder, depth y.
 
  • #88
Did I miss something here? Did anyone measure the time it took for the cylinder to become completely submerged (with varying small hole sizes) as required in the Homework Statement? The Homework did not ask for some theory based on the Homework Equations or to even develop a hypothesis based on the observations of test results.
 
Last edited:
  • #89
under-the-sheet said:
Did I miss something here?
Apparently:
lloydthebartender said:
I'm trying to write up some theory for this experiment
No help was requested regarding the experiment itself.
 
  • #90
In #75, how would you integrate the equation you substitute in for u when you are integrating with respect to y and there aren't any y terms?

I apologise if I've totally misunderstood.
 

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