Geodesic quation coordinate time

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Svendsen
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Hi guys

So I am having trouble reparameterizing the geodesic equation in terms of coordinate time.
Normally you have:

[tex]\frac{d^2 x^{\alpha}}{d \tau^2} + \Gamma_{nm}^{\alpha} \frac{d x^{n}}{d \tau}\frac{d x^{m}}{d \tau} = 0[/tex]

Where [itex]\tau[/itex] is the proper time. I class we were told to express the above in terms of coordinate time and so i reasoned that one would use the chain rule:

[tex]\frac{d }{d \tau} = \frac{d t}{d \tau} \frac{d }{d t}[/tex]

When i do so i get the following:

[tex]\frac{d^2 x^{\alpha}}{d t^2} + \Gamma_{nm}^{\alpha} \frac{d x^{n}}{d t}\frac{d x^{m}}{d t} = - \frac{d^2t/d \tau^2}{dt/d\tau} \frac{d x^{\alpha}}{dt}[/tex]

Which - i guess - has the form that one would expect because t is non-affine.

However i don't know how to proceed from here. I´ve tried to use [itex]d\tau ^2 = g_{nm}dx^ndx^m[/itex] to find [itex]dt/d \tau[/itex], but i can´t seem to get anything meaningful.

Thanks for your time!
 
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I did something related to this once upon a time, but it's been a while. Are you looking to find the form of the geodesic equations given that you have ##x^1##, ##x^2##, ##x^3## as functions of t? If so I might try to reconstruct what I did if you haven't already figured it out by the time I get to it., As I recall it was a matter of using the chain rule, plus some algebra involving the geodesic equation for ##x^0## (which is another name for "t") in it's original form as a function of ##\tau##, i.e. the standard geodesic equation for ##x^0(\tau)## or ##t(\tau)##.
 
You cannot simplify it any further but you can express it in terms of meaningful quantities: ##\frac{dt}{d\tau} = u^0 = \gamma## where ##\gamma## is the "time dilation factor" of the particle in the coordinate system that it is moving through. In stationary space-times, that is those with a time-like Killing field, you can also express ##\frac{dt}{d\tau}## in terms of the conserved energy per unit mass ##e##. For example in Schwarzschild space-time we have ##e = (1 - \frac{2M}{r})\frac{dt}{d\tau}##. Furthermore you can use the geodesic equation for ##\alpha = t## to get rid of ##\frac{d^2 t}{d\tau^2}##.
 
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What did you mean by meaningful? This is the expression for geodesic parametrized by non-affine parameter and any actual physical manifestation might require information on the physical system. If you mean to eliminate the τ derivatives; then I think it is possible to set α to 0th component.

In case you have never done so, physical interpretations usually rely on the Newtonian weak field limit, where the τ derivatives are eliminated by the original geodesic equation under that limit (again by setting α to 0 and making suitable assumptions about the Christoffel connection coefficients).