Planetary motion in a viscous medium

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Homework Help Overview

The discussion revolves around planetary motion in a viscous medium, specifically analyzing the dynamics using Newton's laws and polar coordinates. Participants are exploring the validity of different approaches to solving the problem, particularly focusing on sub-questions (c) and (d).

Discussion Character

  • Mixed

Approaches and Questions Raised

  • Participants discuss the derivation of differential equations in polar coordinates and question the appropriateness of approximations used in the official solution. There is a focus on the implications of varying radius and the nature of velocity in non-circular orbits.

Discussion Status

Some participants express uncertainty about their approaches and seek clarification on the validity of the official solution. There is acknowledgment of the limitations of exact solutions and a recognition that approximations are necessary. Guidance regarding the virial theorem is also introduced, contributing to the discussion.

Contextual Notes

Participants note that the problem involves assumptions about the motion of the planet and the nature of the forces acting on it, which may affect the interpretation of the equations derived.

Leo Liu
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Homework Statement
none
Relevant Equations
F=ma
1605614759603.png

1605614814611.png

The answer to (c) is ##-2\pi AGMm##.
Answer to (d)
1605614872478.png


For sub-question d, I used a different approach and I don't know why the solution to (d) is an appropriate approximation.
What I did was that I use Newton's laws to obtain two differential equation in polar coordinate, as shown:
$$\text{Assume that the planet moves counterclockwise}$$
$$-\frac{GMm}{r^2}\boxed{\hat r}-Amv^2\boxed{\hat\theta} =m(\ddot r-r\dot\theta ^2)\boxed{\hat r}+m(r\ddot\theta+2\dot r \dot\theta)\boxed{\hat\theta}$$
$$\begin{cases}
-A(r\dot\theta)^2=r\ddot\theta+2\dot r\dot\theta\\
-GM/r^2=\ddot r-r\dot\theta^2\\
\end{cases}$$
I would like to know if my solution is correct, and why the official solution works. Thanks a lot.
 

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Leo Liu said:
Homework Statement:: none
Relevant Equations:: F=ma

View attachment 272709
View attachment 272711
The answer to (c) is ##-2\pi AGMm##.
Answer to (d)
View attachment 272712

For sub-question d, I used a different approach and I don't know why the solution to (d) is an appropriate approximation.
What I did was that I use Newton's laws to obtain two differential equation in polar coordinate, as shown:
$$\text{Assume that the planet moves counterclockwise}$$
$$-\frac{GMm}{r^2}\boxed{\hat r}-Amv^2\boxed{\hat\theta} =m(\ddot r-r\dot\theta ^2)\boxed{\hat r}+m(r\ddot\theta+2\dot r \dot\theta)\boxed{\hat\theta}$$
$$\begin{cases}
-A(r\dot\theta)^2=r\ddot\theta+2\dot r\dot\theta\\
-GM/r^2=\ddot r-r\dot\theta^2\\
\end{cases}$$
I would like to know if my solution is correct, and why the official solution works. Thanks a lot.
I wouldn't do it by your way, the velocity vector is, actually is$$\dot{r}\widehat{r} + r\dot{\theta}\widehat{\theta}$$, what you show is the velocity in an circular orbital, if it was a circular orbital, the radius wouldn't varies anyway :S

And, what you didn't understand in the approximation? From c we have "the radius varies to low in a period", so it is a understandable approximation.
Remember the differentials theory

$$\Delta R = \frac{dr}{dt}\Delta t$$
 

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I think your approach though it is aiming for the exact solution, has a big disadvantage:
We can't find the exact solution cause the system of ODEs you write has no closed form solution.

So we have to do approximations as the main solution suggests. All the equations for ##\Delta r## and ##\Delta t## are approximations in the given solution for d).
 
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LCSphysicist said:
what you show is the velocity in an circular orbital, if it was a circular orbital, the radius wouldn't varies anyway :S
Oh yes you are definitely correct. I found out this problem after I could edit my post. Should the first equation be ##-A[(r\dot\theta)^2+\dot r ^2]=r\ddot\theta+2\dot r\dot\theta##?

Even this is not accurate because the direction of velocity is not the same as hat theta. I think we have to assume the angle between the tangent and the velocity is phi and make use of the following identity: ##\tan\phi=\dot r/r\dot\phi##
LCSphysicist said:
And, what you didn't understand in the approximation? From c we have "the radius varies to low in a period", so it is a understandable approximation.
Remember the differentials theory
What I don't understand is why the first equation of the official solution is valid.

Thanks.
 
Last edited:
Leo Liu said:
Oh yes you are definitely correct. I found out this problem after I could edit my post. Should the first equation be ##-A[(r\dot\theta)^2+\dot r ^2]=r\ddot\theta+2\dot r\dot\theta##?

Even this is not accurate because the direction of velocity is not the same as theta.

What I don't understand is why the first equation of the official solution is valid.

Thanks.
The first equation is what they call, in short words, the virial theorem. I recommend you to seek it at wikipedia.
" For gravitational attraction,... the average kinetic energy equals half of the average negative potential energy"
Knowing that E = Epot + Ekin, i think you can understand now how the equation arose ;)
Anyway, while it is approximately true in ellipse orbital, it is exactly true in circular orbits, as follows:
E = mv²/2 - GmM/r
-GmM/r² = -mv²/r (centripetal)
E = GmMr/2r² - GmM/r
E = -GmM/2r
 
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LCSphysicist said:
The first equation is what they call, in short words, the virial theorem. I recommend you to seek it at wikipedia.
This is exactly what I have been looking for. What puzzled me was the reason a small change in energy corresponded to the force times an infinitesimal movement :P
 

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