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

In summary, This is a conversation about how to solve an equation for a variable, specifically for a gravitational force. Daniel found an equation that he thought could be used, but realized that the mass of the Earth is not a point-like gravity source. He then proceeded to solve for the second solution, which involved finding the variation of a constant.
  • #1
dcppc
13
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
  • #2
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.
 
  • #3
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.
 
  • #4
[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...
 
  • #5
Thanks guys, it helps a lot
 
  • #6
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
 
  • #7
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
 
  • #8
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.
 
  • #9
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...:yuck:

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...)
 

What is simple integration?

Simple integration is a mathematical process used to find the area under a curve. It involves finding the antiderivative of a function and evaluating it at specific limits.

How is simple integration useful in science?

Simple integration is useful in science because it allows us to calculate important values such as displacement, velocity, and acceleration from measured data. It is also used to calculate the work done by a force and the energy stored in a system.

What are the steps involved in simple integration?

The steps for simple integration include identifying the function to be integrated, finding its antiderivative, choosing limits of integration, and plugging the limits into the antiderivative to solve for the area under the curve.

What are the common techniques used for simple integration?

The most common techniques used for simple integration are the power rule, substitution, and integration by parts. These techniques allow us to integrate a wide range of functions and solve complex integration problems.

How can simple integration be applied to real-world problems?

Simple integration can be applied to real-world problems in fields such as physics, engineering, economics, and biology. It helps us to analyze and understand the behavior of various systems and make predictions about their future behavior.

Similar threads

Replies
4
Views
347
Replies
2
Views
727
  • Calculus
Replies
3
Views
2K
Replies
11
Views
1K
Replies
4
Views
2K
  • Special and General Relativity
Replies
11
Views
185
  • Introductory Physics Homework Help
Replies
10
Views
263
  • Introductory Physics Homework Help
Replies
13
Views
2K
  • Introductory Physics Homework Help
Replies
2
Views
632
  • Calculus and Beyond Homework Help
Replies
9
Views
769
Back
Top