Are Geodesics and Projectile Trajectories Equivalent in Curved Space-Time?

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Discussion Overview

The discussion revolves around the equivalence of geodesics and projectile trajectories in the context of curved space-time, particularly focusing on the Schwarzschild metric and its implications for gravitational motion. Participants explore theoretical aspects, mathematical derivations, and potential approximations relevant to general relativity and classical mechanics.

Discussion Character

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

Main Points Raised

  • One participant asserts that geodesics in curved space-time should be equivalent to projectile trajectories, starting from specific approximations of the Schwarzschild metric.
  • Another participant suggests simplifying the calculations by approximating \(\sigma^{-1}\) as \(1 + 2gr\) and defining a new coordinate \(\rho = gr\).
  • A different participant questions the validity of approximating \(\sigma^{-1}\) as \(1 + 2gr\), arguing that they are not quite equal, especially at the Earth's surface.
  • Concerns are raised about the use of kinematic equations in deriving results, with one participant stating that this approach may not yield the Newtonian result.
  • One participant mentions that the geodesic equation is derived by extremizing the action for a free particle, referencing the proper length and the metric tensor.
  • Another participant discusses the process of deducing Newton's law of gravitation from general relativity, mentioning the concept of weak field theory.
  • Further mathematical developments are presented, including the leading term yielding the Newtonian value when considering static rest particles.
  • Participants express interest in understanding the relationship between the Euler-Lagrange Equation and the Geodesics Equation.

Areas of Agreement / Disagreement

The discussion contains multiple competing views and remains unresolved regarding the equivalence of geodesics and projectile trajectories, the appropriateness of certain approximations, and the methods used to derive classical mechanics from general relativity.

Contextual Notes

Participants highlight limitations in their assumptions and the dependence on specific conditions, such as the approximation of gravitational effects near the Earth's surface and the validity of using kinematic equations in the context of general relativity.

Black Integra
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Yes, I want to make sure that geodesics of a particle moving in curved space time is the same thing of projectile trajectories.
I start from assuming that 1-\frac{2GM}{r}\approx1-2gr and then calculate the schwarzschild metric in this form
\Sigma_{\mu\nu}=\begin{bmatrix}\sigma & 0\\ 0 & -\sigma^{-1}\end{bmatrix} where \sigma = 1-2gr

and I calculated for the Christoffel symbols for this metric:
\Gamma^0_{\mu\nu}=-\sigma g\begin{bmatrix}0 & 1\\ 1 & 0\end{bmatrix}
\Gamma^1_{\mu\nu}=-\frac{g}{\sigma^2}\Sigma_{\mu\nu}

I plugged them to a geodesics equation

\partial^2_\tau x^\mu = -\Gamma^\mu_{\alpha\beta}\partial_\tau x^\alpha\partial_\tau x^\beta
where d\tau^2 = dx^\mu dx^\nu\Sigma_{\mu\nu}

and I got these ugly conditions:
\partial^2_\tau t = \sigma\partial_\tau t\partial_\tau \sigma
\partial^2_\tau \sigma = \frac{2g^2}{\sigma^2}

what I expect is just something like
x=-\frac{g}{2}t^2

I havn't finished these differential equations yet. But I want to know that I'm going through the right track, right? Any suggestion?
 
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In the level of approximation you're using, you might as well make your life easier and approximate \sigma^{-1} as 1+2gr. I would also define a new coordinate \rho=gr to avoid having to write all the factors of g.
 
I can't see why we can assume that \sigma^{-1} = 1+2gr, they're not quitely equal.(at least at the Earth's surface)

But i think i can apporximate σ to be -2gr because 1 is very small comparing with -2gr. But I still can't find a way to prove this.

Please, any can help me?
 
Black Integra said:
I can't see why we can assume that \sigma^{-1} = 1+2gr, they're not quitely equal.(at least at the Earth's surface)

It IS an approximation. The taylor series expansion of 1/(1-x) is 1+x+x^2 + o(x^3), basically. So if x is small, it's a good approximation.
 
I don't think this approach can give the Newtonian result because you are using kinematic equations. The full equation for r is

<br /> \ddot{r}=-\frac{\left( m\,{r}^{2}-4\,{m}^{2}\,r+4\,{m}^{3}\right) \,{\dot{t}}^{2}-m\,{r}^{2}\,{\dot{r}}^{2}}{{r}^{4}-2\,m\,{r}^{3}}<br />
setting \dot{t}=1 and doing a Maclaurin-Taylor expansion of the RHS in m
<br /> \ddot{r}=-\frac{\left( 1-{\dot{r}}^{2}\right) \,m}{{r}^{2}}+\frac{2\,\left(1+{\dot{r}}^{2}\right) \,{m}^{2}}{{r}^{3}}+\frac{4\,{\dot{r}}^{2}\,{m}^{3}}{{r}^{4}}+ ...<br />
assuming m << r we get
<br /> \ddot{r}=-\frac{\left( 1-{\dot{r}}^{2}\right) \,m}{{r}^{2}}<br />
which does not have a closed form solution. In this m=GM/c2.

However it is possible to deduce Newton's law of gravitation from GR by another approach.
 
Last edited:
pervect said:
It IS an approximation. The taylor series expansion of 1/(1-x) is 1+x+x^2 + o(x^3), basically. So if x is small, it's a good approximation.

That's the point. I use 1-2GM/r = 1-2gr because I calculate in case where g=9.8 and r is around the Earth's radius (not small, is it?)


Mentz114 said:
I don't think this approach can give the Newtonian result because you are using kinematic equations.
Oh. I have never heard something like this before, it's new for me. What's the name of the other way, other than kinematic equation?

Mentz114 said:
However it is possible to deduce Newton's law of gravitation from GR by another approach.
What is the other approach to deduce the classical mechanics? Mainly, I just want to find out that Euler-Lagrange Equation and Geodesics Equation are the same concept.
 
The geodesic equation is found by extremizing the action for a free particle which is
<br /> \int_{\lambda_1}^{\lambda_2}\frac{ds}{d\lambda}d \lambda = \int_{\lambda_1}^{\lambda_2}\sqrt{g_{\mu\nu}\frac{dx^\mu}{d\lambda}\frac{dx^\nu}{d\lambda}}d\lambda<br />
where s is the proper length.

Look up 'weak field theory' in the context of GR to see how Newton's law can be inferred from GR. It's too involved for me to reproduce here.
 
After some reading I found the correct procedure. From my post #5
<br /> \ddot{r}=-\frac{\left( 1-{\dot{r}}^{2}\right) \,m}{{r}^{2}}+\frac{2\,\left(1+{\dot{r}}^{2}\right ) \,{m}^{2}}{{r}^{3}}+\frac{4\,{\dot{r}}^{2}\,{m}^{3 }}{{r}^{4}}+ ...<br />
Now for static rest particle \dot{r}=0 so the leading term gives the Newtonian value.
<br /> \ddot{r}=-\frac{m}{{r}^{2}}=-\frac{GM}{{r}^{2}}<br />

A longer way is to start with
<br /> g_{\mu\nu}=\eta_{\mu\nu}+f_{\mu\nu}<br />
and
<br /> \frac{d^2 x^a}{d\tau^2}= -\Gamma^a_{bc}\frac{dx^b}{d\tau}\frac{dx^c}{d\tau}<br />
throwing away lots of stuff and setting the 4-velocities to (1,0,0,0) getting
<br /> \frac{d^2 x^a}{dt^2}= -\Gamma^a_{00}= \frac{1}{2}\eta^{ab}g_{00,b}= \frac{1}{2}\eta^{ab}f_{00,b}<br />
which works for f_{00}=2m/r
 
Last edited:
thx, that's clear :)
 

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