Second order geodesic equation.

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Discussion Overview

The discussion revolves around the nature and implications of second order geodesic equations in the context of general relativity. Participants explore the significance of having two independent geodesic equations and the methods for addressing them, particularly in relation to symmetries and conservation laws.

Discussion Character

  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant expresses curiosity about the significance of having two independent geodesic equations derived from extremizing the action.
  • Another participant questions the meaning of two independent geodesic equations, suggesting it may relate to working in a two-dimensional space with separate equations for each coordinate.
  • A participant clarifies that they have two independent solutions for a single direction, referencing a specific form of the geodesic equation involving an orthogonal matrix.
  • There is a discussion about the standard form of the geodesic equation being second order in terms of proper time, with a participant asserting that it typically has one independent solution.
  • One participant proposes a simplification using a diagonal connection coefficient, questioning the difference between their approach and a first order equation.
  • Another participant discusses a method for solving differential equations by introducing a new variable, leading to a first order equation, but acknowledges that this does not change the second order nature of the original equation.
  • Participants discuss the role of constants of integration in the context of geodesics and whether they can be arbitrarily set, with one suggesting they specify initial conditions for the geodesic.

Areas of Agreement / Disagreement

Participants express differing views on the nature of the geodesic equations, with some asserting the presence of two independent solutions while others maintain that there should only be one independent solution. The discussion remains unresolved regarding the implications of these differing interpretations.

Contextual Notes

There are unresolved assumptions regarding the definitions of geodesic equations and the implications of second order versus first order formulations. The discussion also highlights the dependence on specific mathematical forms and conditions.

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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