For an affine parameter , the geodesic Lagrangian is
Varying gives the geodesic equations
The rotational Killing vector fields of the spherical symmetry conserve the angular-momentum vector. Its direction is fixed, so every nonradial orbit lies in the plane through the symmetry centre orthogonal to that vector. A spatial rotation can make this the equatorial plane. Equivalently, the initial conditions and solve the equation uniquely. This is the planarity of geodesics in spherical symmetry; a radial geodesic has zero angular momentum and may be assigned any plane.
On , the cyclic coordinates and produce geodesic conserved quantities from Killing vectors,
For a timelike geodesic parametrized by proper time, the proper-time normalization is . Substitution of and gives the first-order radial equation
This is the timelike geodesic effective potential for static Anti-de Sitter spacetime with curvature radius one.
A geodesic passing through must have . If it moves away from the origin, , and
Taking proper time at departure gives
It turns around at and first returns to the origin at
This energy-independent refocusing is the characteristic radial timelike geodesic in anti-de Sitter spacetime result; for curvature radius , the answer is .
Use the metric signature and abbreviate , with a length. Dots initially mean differentiation with respect to an affine parameter . The geodesic Lagrangian in the equatorial plane is
The planarity of geodesics in spherical symmetry permits this plane to be chosen. More explicitly, the full angular Euler-Lagrange equation is , so initial data , preserve it.
Both and are cyclic coordinates. Their Euler-Lagrange equations give conserved conjugate momenta and . Defining constants therefore gives
The corresponding second-order geodesic equations are
and variation of gives
The geodesic Lagrangian has no explicit dependence. Its conserved Lagrangian energy function is , since it is quadratic in the tangent components. Thus twice this function is a constant:
This is the constant squared tangent norm of an affinely parametrized geodesic.
For a massive particle choose , its proper time, and obtain . For a photon, the tangent is null and . A general rescaling of a massive particle's affine parameter rescales a positive ; the numerical value requires the proper time choice. With that choice, is signed specific angular momentum, of units , and is dimensionless conserved specific Killing energy. The time coordinate is normalized to proper time at infinity, so this is the particle's conserved energy referred to infinity. A photon's constants scale with the normalization of its null tangent; it has no rest frame or proper time parametrization.
Substitution of and into the norm gives the general radial first integral
For a massive particle this becomes
Adopting the usual half-normalization for the effective potential for timelike Schwarzschild geodesics, define
All terms have units , or energy per unit mass. The first two terms are the Newtonian gravitational and centrifugal contributions; the last is the relativistic correction.
A circular orbit requires both and . Differentiating at fixed gives
The radial first integral also gives
For the future-directed circular orbit at , these constants are , , and . Therefore
Since Schwarzschild time agrees with the clock time of a static observer at infinity, the intended infinity-referred tangential orbital speed is
This uses the circumferential areal radius with the clock at infinity; it is not a local measurement made at the orbit. A local static observer's clock instead has and measures . These two operationally different speeds explain the significance of the phrase “at infinity”.
The effective-potential stability of a circular orbit follows from
Consequently the orbit exists but is unstable to radial perturbations. The original plot below shows its position at a maximum, for .
For a weak-field elliptic orbit, the relativistic correction makes the direction of closest approach advance after each radial cycle. The derivations under i and ii below give
per orbit to first order, where is the semi-major axis and the orbital eccentricity. For Mercury, the additional Schwarzschild perihelion precession is approximately 43 arcseconds per century, over and above the much larger Newtonian precession produced primarily by other planets. It is the unexplained residual after those effects have been included that provides the classic quantitative test of general relativity; one should not identify the whole observed precession with this relativistic correction.[ref]
The labels i and ii in the original paper introduce optional orbit-equation aids, rather than separate mandatory subquestions. They are retained here for derivations of both aids and of the perihelion result.