In general relativity, a geodesic generalizes the notion of a "straight line" to curved spacetime. Importantly, the world line of a particle free from all external, non-gravitational forces is a particular type of geodesic. In other words, a freely moving or falling particle always moves along a geodesic. In general relativity, gravity can be regarded not as a force but a consequence of a curved spacetime geometry where the source of curvature is the stress–energy tensor (representing matter, for instance). Thus, for example, the path of a planet orbiting a star is the projection of a geodesic of the curved four-dimensional (4-D) spacetime geometry around the star onto three-dimensional (3-D) space.
Mathematical expression The full geodesic equation is
d 2 x μ d s 2 + Γ μ
α β d x α d s d x β d s = 0 {\displaystyle {d^{2}x^{\mu } \over ds^{2}}+\Gamma ^{\mu }{}_{\alpha \beta }{dx^{\alpha } \over ds}{dx^{\beta } \over ds}=0\ }
where s is a scalar parameter of motion (e.g. the proper time), and Γ μ
α β {\displaystyle \Gamma ^{\mu }{}_{\alpha \beta }} are Christoffel symbols (sometimes called the affine connection coefficients or Levi-Civita connection coefficients) symmetric in the two lower indices. Greek indices may take the values: 0, 1, 2, 3 and the summation convention is used for repeated indices α {\displaystyle \alpha } and β {\displaystyle \beta } . The quantity on the left-hand-side of the sum in this equation is the acceleration of a particle, so this equation is analogous to Newton's laws of motion, which likewise provide formulae for the acceleration of a particle. The Christoffel symbols are functions of the four spacetime coordinates and so are independent of the velocity or acceleration or other characteristics of a test particle whose motion is described by the geodesic equation.
Using coordinate time as parameter So far the geodesic equation of motion has been written in terms of a scalar parameter s. It can alternatively be written in terms of the time coordinate, t ≡ x 0 {\displaystyle t\equiv x^{0}} (here we have used the triple bar to signify a definition). The geodesic equation of motion then becomes:
d 2 x μ d t 2 = − Γ μ
α β d x α d t d x β d t + Γ 0
α β d x α d t d x β d t d x μ d t . {\displaystyle {d^{2}x^{\mu } \over dt^{2}}=-\Gamma ^{\mu }{}_{\alpha \beta }{dx^{\alpha } \over dt}{dx^{\beta } \over dt}+\Gamma ^{0}{}_{\alpha \beta }{dx^{\alpha } \over dt}{dx^{\beta } \over dt}{dx^{\mu } \over dt}\ .}
This formulation of the geodesic equation of motion can be useful for computer calculations and to compare General Relativity with Newtonian Gravity. It is straightforward to derive this form of the geodesic equation of motion from the form which uses proper time as a parameter using the chain rule. Notice that both sides of this last equation vanish when the mu index is set to zero. If the particle's velocity is small enough, then the geodesic equation reduces to this:
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