Hydrostatic problem - Impossible integral

In summary, the conversation discusses a hydrostatic problem involving a U-Tube filled with water and a constant vertical force. The goal is to find the position of the water's surface over time using principles of energy conservation. The conversation includes various calculations and equations, but a solution is yet to be found.
  • #1
jaumzaum
434
33
Hydrostatic problem - Impossible integral!

Just studying hidrostatic over the internet and I saw the following problem:

A U-Tube filled with water, initially at rest in a horizontal table, has A1=40cm2, A2 = 20cm2, A3=30cm2, h1 = 80cm, h2 = 20cm and L = 100cm (below piture). It is pressed in A1 by a constant vertical force F of 4N. Find the position x of the surface A1 in function of time (initial position is x=0). Given: g = 10m/s2, density of water is 1kg/L

http://img191.imageshack.us/img191/2825/78925268.png

How can I solve this? I tried some stuff but it didn't worked.

A1.dx1 = A2.dx2 = A3.dx3 (where dx is the infinitesimal variation of position for a infinitesimal variation of time).

By energy conservation:

F.dx1 = Δ(mechanic energy)

Potential Energy -> Now imagine that the dx1.A1 volume of water has just raised and become the dx2.A2 volume. It raised dx1.(A1+A2)/(2A2)
Ep = dx1.(A1+A2)/(2A2).dm.g
But dm = A1.dx1
Ep = dx12.(A1+A2)/(2A2).A1.ρ.g

Kinetic Enegrgy -> Ek = ∫(dm.v.dv)
dm = A1.v1.dt/ρ (v1 is the instantaneum velocity for the surface A1)
v = A1.v1/A (A is the area of the surface considered)
dv = A1.dv1/A

Ek = ∫[(A13v12.dt.dv1)/(ρ.A2)]

But I don't know how to solve this. I don't know even if it is right.
Can anyone help me?
 
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  • #2


Remember, water is incompressible.

Apply Pascal's law to the two columns after application of the force.
 
  • #3


SteamKing said:
Apply Pascal's law to the two columns after application of the force.
Not sure that helps. The fluid is accelerating, so it's hydrodynamics, not hydrostatics. jaumzaum, I didn't understand your KE calculation. Can you not just add up the KEs of the three sections (ignoring complications at the corners)? At time t the force has advanced x, the volumes will be (h1-x)A1, LA3 and (h1+xA1/A2))A2; the speeds v (=dx/dt), vA1/A3, and vA1/A2.
But the corners bother me. Not sure how to use h2.
 
  • #4


I considered the process to be very slow (as the force is 4N). So I think the column of water tend to move orderly. I don't know how to use the h2 too! Actually this problem was from this university: http://www.ita.br/

It was a test applied on the school. You could use computers and you had to plot the graphic position xtime. The other exercises in the same test resulted in integrals that had to be series-aproximated, so I think you have to do some assumptions. But I don't know what!

[]'s
Joao
 
  • #5


Not sure that helps. The fluid is accelerating, so it's hydrodynamics, not hydrostatics. jaumzaum, I didn't understand your KE calculation. Can you not just add up the KEs of the three sections (ignoring complications at the corners)?

I think you can ignore the corners. I calculated KE for a random "surface" (it is actually a infinitesimal cylinder) of area A. Then I just added the 3 integrals for the 3 surfaces. But I still can't solve it! I mean, inside the integral is there dx and dt. To take the integral signal off I have to derivate. But derivate in relation to what? Time? Velocity? Position? And I also don't know how to derivate F.dx, for example! Another thing I noticed is that dx12.(A1+A2)/(2A2).A1.ρ.g is very smaller than F.dx, can we ignore it?

How can I solve this?
 
  • #6


Working in terms of energy, you don't need dx's in the PE expression. Just consider that the total advancement of the force at time t is x. Abbreviating h1 to h:
PE = x2.(A1+A2)/(2A2).A1.ρ.g
2*KE = (h-x)A1ρv2 + Lρv2A12/A3 + (h+xA1/A2)ρv2A12/A2
PE+KE = Fx
v2{h(1+A1/A2)+LA1/A3+x((A1/A2)2-1)} = 2Fx/(ρA1) - x2.g(A1+A2)/A2
 
  • #7


haruspex said:
Working in terms of energy, you don't need dx's in the PE expression. Just consider that the total advancement of the force at time t is x. Abbreviating h1 to h:
PE = x2.(A1+A2)/(2A2).A1.ρ.g
2*KE = (h-x)A1ρv2 + Lρv2A12/A3 + (h+xA1/A2)ρv2A12/A2
PE+KE = Fx
v2{h(1+A1/A2)+LA1/A3+x((A1/A2)2-1)} = 2Fx/(ρA1) - x2.g(A1+A2)/A2

This looks like a very nice development. The OP should also know that

v=dx/dt

This results in a first order ordinary differential equation for calculating x as a function of t. After taking the square root of both sides of the equation, it probably would be best to substitute
x=y2 and solve for y.
 
  • #8


haruspex said:
Working in terms of energy, you don't need dx's in the PE expression. Just consider that the total advancement of the force at time t is x. Abbreviating h1 to h:
PE = x2.(A1+A2)/(2A2).A1.ρ.g
2*KE = (h-x)A1ρv2 + Lρv2A12/A3 + (h+xA1/A2)ρv2A12/A2
PE+KE = Fx
v2{h(1+A1/A2)+LA1/A3+x((A1/A2)2-1)} = 2Fx/(ρA1) - x2.g(A1+A2)/A2

When I try to solve this (using Wolfram Mathematica of couse), the function does not accept the contour value of 0 for initial value of position.

v2 (3.73333 + 3 x) = 2 x - 30 x2

http://www.wolframalpha.com/input/?i=(x')^2+(3.73333+++3+x[t])+==+2+x[t]+-+30+x[t]^2

What this means?
 
  • #9


As you can see, plugging in x=0 gives v=0, which is true. You would get the same trying to determine a trajectory under gravity using the energy equation y'2 = 2gy. This stops any numerical attempt to produce a plot from there - things never move. You can validly get around it by plugging in a very small nonzero starting value.
 
  • #10


jaumzaum said:
When I try to solve this (using Wolfram Mathematica of couse), the function does not accept the contour value of 0 for initial value of position.

v2 (3.73333 + 3 x) = 2 x - 30 x2

http://www.wolframalpha.com/input/?i=(x')^2+(3.73333+++3+x[t])+==+2+x[t]+-+30+x[t]^2

What this means?

What it means is that you need to follow the advice I gave you in my previous response. Substitute v = dx/dt, divide both sides of the equation by (3.733 + 3x), take the square root of both sides of the equation, substitute x = y2, and factor y out from both sides of the equation. Then solve the resulting first order ordinary differential equation for y(t). At short times, the solution should be of the approximate form y ~ kt, or x ~ at2/2, where a is the initial acceleration, and where a can be determined analytically in terms of the constants in your equation.

Wolframalpha won't be able to solve the equation until you work it into the form that I indicated.
 
  • #11


haruspex said:
As you can see, plugging in x=0 gives v=0, which is true. You would get the same trying to determine a trajectory under gravity using the energy equation y'2 = 2gy. This stops any numerical attempt to produce a plot from there - things never move. You can validly get around it by plugging in a very small nonzero starting value.

As I said in my previous post, plugging in a small starting value isn't necessary. If

y'2 = 2gy

If you take the square root of both sides, you get:

[tex]y'=\sqrt{2gy}[/tex]

Next, substitute y = z2 to get

[tex]2z\frac{dz}{dt}=z\sqrt{2g}[/tex]
or
[tex]\frac{dz}{dt}=\frac{\sqrt{2g}}{2}[/tex]

This can now easily be integrated with respect to t. The same type of approach applies to the problem at hand.
 
  • #12


Chestermiller said:
As I said in my previous post, plugging in a small starting value isn't necessary.
Sure - an analytic solution gets past the problem. Just wanted to explain that numerical methods can still be made to work when necessary.
 
  • #13


haruspex said:
Sure - an analytic solution gets past the problem. Just wanted to explain that numerical methods can still be made to work when necessary.

Actually, I was alluding to using this approach (substitution of x = y2) to solve the problem numerically, starting out at y = x = 0 at t = 0. I've done this trick many times in obtaining numerical solutions to problems of this type of form.
 
  • #14


haruspex said:
PE+KE = Fx
v2{h(1+A1/A2)+LA1/A3+x((A1/A2)2-1)} = 2Fx/(ρA1) - x2.g(A1+A2)/A2

I believe the factor shown in blue should be 1 + (A1/A2)^2. [EDIT: Nevermind, my mistake!]

Anyway, for the numbers given in the problem, I think it's safe to neglect the term in red. Then to a good approximation, the solution is SHM with a small amplitude. [Edit: I'm getting an amplitude of 10/3 cm and a period of about 2.2 s]
 
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What is a hydrostatic problem?

A hydrostatic problem is a type of physics problem that involves calculating the pressure at different points in a fluid, typically a liquid, at rest. This can be used to determine the forces acting on an object submerged in the fluid.

What makes the integral in a hydrostatic problem impossible?

The integral in a hydrostatic problem is considered impossible because it cannot be solved using traditional mathematical methods. It involves finding the inverse of a function that is not continuously differentiable, making it impossible to find a solution using standard techniques.

Why is the hydrostatic problem still studied despite the impossible integral?

The hydrostatic problem is still studied because it has real-world applications in fields such as engineering, meteorology, and oceanography. While the integral may be impossible to solve, approximations and numerical methods can be used to provide useful solutions.

What are some challenges in solving hydrostatic problems?

One of the main challenges in solving hydrostatic problems is accurately modeling the fluid and its behavior. This can be difficult because fluids can have complex properties and behaviors, such as viscosity and turbulence, that can affect the calculations.

What are some practical uses of hydrostatic problems?

Hydrostatic problems have many practical uses, including determining the buoyancy of ships and other objects in water, predicting the behavior of fluids in pipelines and tanks, and understanding weather patterns and ocean currents. They are also important in designing structures that can withstand the pressure of fluids, such as dams and submarines.

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