Time it takes for submerged object to rise to surface

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Discussion Overview

The discussion revolves around the time it takes for a submerged spherical object to rise to the surface from a depth of 300 meters. Participants explore the physics involved, including buoyancy, forces acting on the object, and the effects of medium resistance, while also considering real-world applications and constraints.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • Some participants inquire about the formula to calculate the time for an object to rise from a specific depth, given its dimensions and weight.
  • Archimedes' principle is referenced, stating that the upward force on a submerged object equals the weight of the fluid displaced.
  • Calculations are presented regarding the volume of the sphere, the mass of water displaced, and the resulting buoyant force compared to the weight of the object.
  • Some participants express uncertainty about the effects of tension from a cable attached to the object, questioning how it influences the calculations.
  • Resistance of the medium (viscosity) is noted as a significant factor that is not accounted for in initial calculations.
  • Discussions arise about the feasibility of the scenario, including the pressure at depth and the material properties of the object, which could lead to structural failure.
  • Participants explore hypothetical scenarios, such as using mercury to fill the sphere to achieve desired buoyancy and weight characteristics.
  • Questions are raised about realistic dimensions and weights for the object to ensure it can withstand the pressure at 300 meters depth while remaining buoyant.

Areas of Agreement / Disagreement

Participants generally agree on the principles of buoyancy and the calculations involved but disagree on the implications of tension, the effects of viscosity, and the feasibility of the object under real-world conditions. The discussion remains unresolved regarding the realistic dimensions and materials for the object.

Contextual Notes

Limitations include assumptions about ignoring viscosity, the nature of the tension in the cable, and the structural integrity of materials at depth. The calculations depend on the definitions of buoyancy and density, which may vary based on the object's material composition.

  • #31
LastOneStanding said:
Actually, I lied: you just have to refer to a table of standard derivatives to see that: \frac{d}{dx}arctanh(x) = \frac{1}{1 - x^2}. You can check this if you like. Your calc textbook should also have a proof of this in it. Now just rescale the variables appropriately and you get the result.

Ah, ok, I think I'm getting close now! Great stuff on the terminal velocity too, that part makes total sense, thanks again!

\frac {1}{a} \int \frac {dv}{1-\alpha^{2} v^{2}} = t_{0} + t

\frac {tanh^{-1}\left(\alpha v\right)}{a} = t_{0} + t

Ignoring t_{0}:

tanh^{-1}\left(\alpha v\right) =a t

\alpha v = tanh\left(a t\right)

v = \frac {tanh\left(a t\right)}{\alpha}

Somewhere I lost an alpha! :P
 
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  • #32
Let's just focus on:
\int \frac {dv}{1-\alpha^{2} v^{2}}

Set u=\alpha v, du = \alpha dv. Thus we have:
\frac{1}{\alpha}\int \frac {du}{1-u^{2}} = \frac{1}{\alpha}arctanh(u)

There's your missing alpha. Not just sub u back in and multiply the \frac{1}{a} I ignored.

Incidentally, if you want to show that arctanh(x) = \int \frac{dx}{1 - x^2}, you can use trig substitution like I said—but with hyperbolic trig functions, not regular ones like you tried. Substitute x = tanh(u) and away you go. Of course, if you knew to do this off the top of your head, you could have just solved the original differential equation by inspection without all this fiddling. Solving diff eq's is as much an art as a science. Such is life.
 
  • #33
LastOneStanding said:
Let's just focus on:
\int \frac {dv}{1-\alpha^{2} v^{2}}

Set u=\alpha v, du = \alpha dv. Thus we have:
\frac{1}{\alpha}\int \frac {du}{1-u^{2}} = \frac{1}{\alpha}arctanh(u)

There's your missing alpha. Not just sub u back in and multiply the \frac{1}{a} I ignored.

Incidentally, if you want to show that arctanh(x) = \int \frac{dx}{1 - x^2}, you can use trig substitution like I said—but with hyperbolic trig functions, not regular ones like you tried. Substitute x = tanh(u) and away you go. Of course, if you knew to do this off the top of your head, you could have just solved the original differential equation by inspection without all this fiddling. Solving diff eq's is as much an art as a science. Such is life.

You are awesome, thank you once again. I was just coming back to look and see if I should have used u substitution there to get my missing alpha, and apparently should have. I should have known better on that one, but rushed it! I can't wait to take the course, but will be taking multivariable first for intro to mechanics followed by differential equations next semester.

I really appreciate both your's and voko's posts, but especially your added explanations! Enjoy the rest of your evening.
 
  • #34
My pleasure, good luck in the course.
 
  • #35
\frac {1} {a} \int_0^v \frac {dv} {1 - \alpha^2 v^2} = \frac {1} {2a} \int_0^v \left[ \frac {1} {1 - \alpha v} + \frac {1} {1 + \alpha v}\right]dv = \frac {1} {2\alpha a} \left[ -ln (1 - \alpha v) + ln(1 + \alpha v)\right]_0^v = \frac {1} {2\alpha a} \ln \frac {1 + \alpha v} {1 - \alpha v} Using Euler's formula for hyperbolic functions, we can see immediately that the latter is \frac {1} {\alpha a} \tanh^{-1} \alpha v, so \frac {1} {\alpha a} \tanh^{-1} \alpha v = \int_0^t dt = t
 
  • #36
The second integration is even easier: \frac {1} {\alpha} \int_0^t \tanh \alpha a t dt =\frac {1} {\alpha} \int_0^t \frac {\sinh \alpha a t} { \cosh \alpha a t }dt = \frac {1} {\alpha} \int_0^t \frac { (\frac {\cosh \alpha a t} {\alpha a})'} { \cosh \alpha a t }dt == \frac {1} {\alpha^2 a} \left[\ln \cosh \alpha a t\right]_0^t = \frac {1} {\alpha^2 a} \ln \cosh \alpha a t = \int_{x_0}^{x} dx = x - x_0
 
  • #37
Cool, thanks for sharing the way you worked them out! I think I prefer the u substitution and tanh^-1 identity over using logarithms and Euler's formula, but mostly just because I already have all the hyperbolic identities and their inverses memorized from differentiation. That's still an interesting way to see it done though, and I'm going to try to remember how to do it. I saw that last identity yesterday (Euler's formula) in my book when looking for hyperbolic identities, but didn't think it could be applied until I saw how you first expanded it and integrated into logarithms.

After the first integration was explained yesterday, the second integration became obvious, but still, thanks for walking me through the steps you took for both!
 

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