Second order geodesic equation.

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SUMMARY

The discussion centers on the interpretation of second order geodesic equations in the context of extremizing action in differential geometry. The participants explore the implications of having two independent geodesic equations, particularly in a two-dimensional space with coordinates {x1, x2}. The equation presented,  𝑥(𝜏)a = 𝐴ab(𝜏) 𝑥(𝜏)b, indicates that the matrix 𝐴ab is orthogonal, leading to discussions on the nature of solutions and constants of integration in second order differential equations.

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ozone
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Hello all,

I have a geodesic equation from extremizing the action which is second order. I am curious as to what the significance is of having 2 independent geodesic equations is. Also I was wondering what the best way to deal with this is.
 
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What do you mean by two independent geodesic equations? Are you working in a 2 dimensional space with coordinates ##\{x^1,x^2\}## and have two geodesic equations, one for each coordinate?

As an aside, usually the easiest way to deal with the geodesic equation is to not deal with it at all. What I mean by this is that if your space has obvious symmetries then just use first integrals of conserved quantities. It's the same thing as using conservation of energy instead of Newton's 2nd law for classical mechanics problems.
 
Sorry I should have been more clear, I believe that I have two independent solutions to the geodesic equation for a single direction, but perhaps I am misinterpreting the result. The equation is written as

\ddot{x}(\tau)^a = A_{ab}(\tau) x(\tau)^b

Here a,b are the two orthogonal directions to the wavefront of a pp-wave. Luckily I am in a system where A_{ab} is an orthogonal matrix. This was derived using some symmetries and conversations with the Lagrangian. However I am having trouble interpreting what it means to have a second order geodesic equation (when we write down our geodesic equation in terms of Christoffel symbols it is always first order).
 
Perhaps we're using different definitions of the geodesic equation but AFAIK it is always second order in ##\tau##: ##\ddot{x}^{\mu} = -\Gamma ^{\mu}_{\alpha\beta}\dot{x}^{\alpha}\dot{x}^{\beta}##.
 
True but the equation above should only have one independent solution as best I can ascertain.. Suppose for simplicity we had a diagonal connection coefficient which is valued at 1 in some \bar{x}direction, I don't see how that is different from writing \dot{x}= x^2 (by substitutingx = \dot{\bar{x}}),this is only a first order equation... or am I missing something blatant?
 
ozone said:
True but the equation above should only have one independent solution as best I can ascertain.. Suppose for simplicity we had a diagonal connection coefficient which is valued at 1 in some \bar{x}direction, I don't see how that is different from writing \dot{x}= x^2 (by substitutingx = \dot{\bar{x}}),this is only a first order equation... or am I missing something blatant?
This is one of the standard tricks/methods for solving differential equations. Define p = dx/dt and hope that you can write a DE containing p alone. If so, it will be first order and you can solve it to get p(t). There will be one constant of integration.

But then you still have to solve p = dx/dt to get x(t), and this will produce a second constant of integration. It's a second order DE, you haven't changed that, all you have done is to solve it in stages.
 
Fair enough, I agree with what you are saying. My main question then is what do we do with these constants of integration? May we just arbitrarily set them equal to one?
 
ozone said:
Fair enough, I agree with what you are saying. My main question then is what do we do with these constants of integration? May we just arbitrarily set them equal to one?
E.g. they can be used to specify the two initial conditions for the geodesic: the initial position and velocity.
 

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