Determining the Solution for d^2r/dt^2 = G*M/r^2 with Constant G and M

  • Context: Undergrad 
  • Thread starter Thread starter dcppc
  • Start date Start date
  • Tags Tags
    Intergration
Click For Summary

Discussion Overview

The discussion revolves around solving the second-order ordinary differential equation (ODE) \(\frac{d^2r}{dt^2} = G\frac{M}{r^2}\), where \(G\) and \(M\) are constants. Participants explore various methods of integration, the implications of initial conditions, and the physical interpretations of the equation in the context of gravitational forces.

Discussion Character

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

Main Points Raised

  • Some participants clarify that \(G\) is the universal gravitational constant and \(M\) is the mass of the attracting body, while \(r\) varies.
  • One participant notes the complexity of integrating the nonlinear second-order ODE and suggests consulting celestial mechanics literature.
  • A method involving the substitution \(w = \frac{dr}{dt}\) is proposed, leading to an integral that participants express skepticism about solving for \(r\) as a function of time.
  • Another participant raises a separate problem involving integration that leads to a logarithmic expression, questioning how to resolve constants when \(r\) approaches zero.
  • Concerns are expressed about the physical implications of \(r = 0\) in the context of gravitational forces, with discussions on the undefined nature of logarithmic functions at zero.
  • Some participants discuss the gravitational field outside a planet being equivalent to a point mass at its center, while others challenge the applicability of Coulomb-like potentials in this context.
  • One participant suggests a potential solution form \(r(t) = B t^A\) and discusses the method of variation of constants for finding solutions.

Areas of Agreement / Disagreement

Participants express differing views on the implications of \(r = 0\) and the validity of certain mathematical approaches. There is no consensus on how to handle the integration constants or the physical interpretation of the gravitational forces at \(r = 0\).

Contextual Notes

Participants note that the gravitational potential becomes undefined at the origin and that the assumptions about the mass distribution of Earth affect the applicability of certain models.

Who May Find This Useful

This discussion may be useful for students and enthusiasts of classical mechanics, particularly those interested in gravitational dynamics and the mathematical techniques used to solve related differential equations.

dcppc
Messages
13
Reaction score
0
Here is a stupid question
How would you solve for [tex]\frac{d^2r}{dt^2}=G\frac{M}{r^2}[/tex]
I'm new at this stuff, can anyone tell me??
Assume G and M are constants
 
Physics news on Phys.org
Yes, they are constants. G is your universal gravitational constant. M is the mass of the body your object is being attracted to.

The distance away from the center of the body (r) is the only thing that changes.
 
It's not that simple to integrate that ODE.Technically,it's nonlinear second order.Since that equation appears in the Kepler problem in classical mechanics,i would advise you to look for a book on celestial mechanics which would deal nicely with this equation.

Daniel.
 
[tex]\frac{d^{2}r}{dt^{2}}=\alpha r^{-2}[/tex]

Let [tex]w=dr/dt[/tex].

Then [tex]dw/dt=d^{2}r/dt^{2}[/tex].

Chain Rule:
[tex]dw/dt=\frac{dw}{dr}\frac{dr}{dt}=\frac{dw}{dr}w[/tex].

[tex]\frac{dw}{dr}w=\alpha r^{-2}.[/tex]

[tex]\int wdw=\int \alpha r^{-2}dr[/tex]

[tex]w^{2}=-2\alpha r^{-1}+C_{1}[/tex]

At this point, solve for the constant using the initial velocity of the body.

[tex]dr/dt=\sqrt{-2\alpha r^{-1}+C_{1}}[/tex]


[tex]\int \frac{dr}{\sqrt{-2\alpha r^{-1}+C_{1}}}=\int dt[/tex]

If you type in
(-2 a x^(-1) + c)^(-1/2)
to integrals.wolfram.com , you get something. Realize that what you get is t on one side and r (which is x in the website) is in the mess on the left hand side. I doubt that you can solve for r as a function of time. You can still get a graph though.

It's kinda cool to see a graph whose *acceleration* is changing. Or maybe that's just me...
 
Thanks guys, it helps a lot
 
I ran into another problem, I was doing a problem similar to this
[tex]\int \frac{dr}{\sqrt{\alpha r^{2}+C}}=\int dt[/tex]
then

[tex]\frac{\log{[2\sqrt{\alpha}r+2\sqrt{C+\alpha r^2]}}}{\sqrt{\alpha}}+C_{1}=t[/tex]
and my lst constant is 0

[tex]\frac{\log{[4\sqrt{\alpha}r]}}{\sqrt{\alpha}}+C_{1}=t[/tex]
and my r and t are zero
but I can't solve for [tex]C_{1}[/tex] because log 0 is undefined, even if I let r approach to 0, it's value will still be negative infinity.
How would I solve this problem because I need a numerical value for t when r=6.37*10^6
 
I found out another thing
If I plug in 0 for my constant fisrt, then the intergral will be different
[tex]\int \frac{dr}{\sqrt{\alpha r^{2}}}=\int dt[/tex]

the intergral is
[tex]\frac{r\log{r}}{\sqrt{\alpha r^2}}+C_{1}=t[/tex]
why is that
 
It can't be.

[tex]\int \frac{dr}{\sqrt{\alpha r^{2}}} =\frac{1}{\sqrt{\alpha}}\int \frac{dr}{|r|} =\frac{1}{\sqrt{\alpha}}\ln |r| +C[/tex]

,which is something else.

Daniel.
 
but still, ln 0 still is undefined
Is there anyway to solve C?
 
  • #10
Depends on the initial conditions.Give them and u can find all integration constants (there must be 2).Notice that [itex]r\neq 0[/itex] which can be seen from the ODE.


Daniel.
 
  • #11
What if the only known value is t=0 and r=0, because since something is going to the center of the earth, then when it's 0 second, the distance it traveled must be 0
 
  • #12
r=0 doesn't work. Let's say I have a perfect point particle of arbitrary nonzero mass. What is the gravitational force on another point particle of arbitrary mass (again nonzero) at the exact same location as the first particle?
 
Last edited:
  • #13
Gravitational potential (Coulomb type) is not finite in the origin (= the point where u have the pointlike source) (it "blows up",just like the electrostatic one).Unfortunately it's not renormalizable either...

Daniel.
 
  • #14
you guys are right, I thought r=x but that does't mean that x=r, but still, when r approches to 0, the gravity should also gets smaller. Instead I got negative numbers when my r is less than 1
 
Last edited:
  • #15
Earth is not a pointlike gravity source.Coulomb potential will not apply.

Daniel.
 
  • #16
Well...I don't know, but I think it was proven outside of the earthbulk, the graviation field is equivalent to the whole mass concentrated at the center of mass...(of course with the Newtonian potential only, for the relativistic equivalent one I don't know)

For the differential equation, I think you can use first a guess :

r(t)=B*t^A...giving in particular A=2/3.

Then u can use the variation of the constant to find the second solution...but that's a bit of work.
 
  • #17
kleinwolf said:
Well...I don't know, but I think it was proven outside of the earthbulk, the graviation field is equivalent to the whole mass concentrated at the center of mass...(of course with the Newtonian potential only, for the relativistic equivalent one I don't know)

For the differential equation, I think you can use first a guess :

r(t)=B*t^A...giving in particular A=2/3.

Then u can use the variation of the constant to find the second solution...but that's a bit of work.

---------------------------------------------------------------
Where did your differential equation came from?
and actually, I'm assuming that the mass of the Earth is the same all throughout
 
  • #18
When you're outside of a large body, such as a planet, you can essentially treat it as a point mass located at its center. When you're inside that planet, the force you experience is proportional to your distance from the center. Both facts directly follow from Gauss' law (assuming Newtonian gravity, of course).
 
  • #19
dcppc :

I'm just trying a solution by chance or maybe by experience (you can also call it an Ansatz)...it's just a guess, it turns out it works...but it could also not...(monomial ansatz are quite useful, also for functional equations, aso...)
 

Similar threads

  • · Replies 2 ·
Replies
2
Views
2K
  • · Replies 6 ·
Replies
6
Views
2K
  • · Replies 4 ·
Replies
4
Views
5K
  • · Replies 4 ·
Replies
4
Views
3K
  • · Replies 11 ·
Replies
11
Views
2K
  • · Replies 1 ·
Replies
1
Views
3K
  • · Replies 4 ·
Replies
4
Views
3K
  • · Replies 11 ·
Replies
11
Views
3K
  • · Replies 19 ·
Replies
19
Views
3K
  • · Replies 4 ·
Replies
4
Views
2K