Solving the Equation of Geodesic Deviation

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SUMMARY

The discussion focuses on solving the equations of geodesic deviation in spacetime, highlighting both numerical and analytical methods. The equations can be approached as a simple ordinary differential equation (ODE) using numerical methods in specific spacetimes. Notably, solutions are expressible in terms of the spacetime's world function, or Synge's function, which relates to geodesic distances. Additionally, iterative approximation schemes utilizing the Riemann tensor are suggested for scenarios with significant but manageable variations in the tensor.

PREREQUISITES
  • Understanding of ordinary differential equations (ODEs)
  • Familiarity with Fermi-like coordinates and Riemann normal coordinates
  • Knowledge of Synge's function and its applications
  • Basic concepts of bitensor perturbation theory
NEXT STEPS
  • Research numerical methods for solving ordinary differential equations in general relativity
  • Study Synge's function and its role in geodesic deviation
  • Explore bitensor perturbation theory and its applications in gravitational physics
  • Investigate iterative approximation techniques involving the Riemann tensor
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Physicists, mathematicians, and students specializing in general relativity, particularly those interested in the dynamics of geodesic deviation and spacetime geometry.

Altabeh
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Hello

Anybody know how we can solve the equations of geodesic deviation in a given spacetime whether approximately or exactly?

Thanks in advance
 
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There are lots of things you can do. It is a simple ODE, and can be solved straightforwardly using numerical methods in specific spacetimes. If you write the equation in Fermi-like coordinates based around the worldline of interest, it turns into something like a harmonic oscillator equation with variable (and possibly negative) spring constant.

More interestingly, all solutions are known analytically (at least in a finite region) in terms of the spacetime's world function (also known as Synge's function). This is a two-point scalar [itex]\sigma(x,x') = \sigma(x',x)[/itex] that returns one-half of the geodesic distance between its arguments. See Dixon, Proc. R. Soc. A 314, 499 (1970) or http://arxiv.org/abs/0807.1150" . Standard results in bitensor perturbation theory can be used to turn this solution into a power series near the initial point, if desired. Part of the exact solution also looks very nice in Riemann normal coordinates (without approximation).

Alternatively, one can write down an equation that leads to an iterative approximation scheme using integrals of the Riemann tensor. This is useful for cases where the Riemann tensor changes considerably but never gets particularly large. See the GR textbooks by Synge or de Felice and Clark.
 
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