Equatorial plane 2026-10-31
Given a polar axis, the equatorial plane passes through the sphere's centre and is perpendicular to that axis. In spherical coordinates with polar angle , it is the plane . For motion in a spherically symmetric gravitational field, conservation of angular momentum permits rotation of axes so that a nonradial orbit lies in such a plane. This is a choice of orientation, rather than an additional physical restriction on a spherically symmetric problem.
Put , use proper time , and denote its derivatives by dots. The timelike geodesic equations, away from the Schwarzschild coordinate singularity, are
with normalization . Spherical symmetry permits an equatorial plane, , and the cyclic coordinates give . Normalization then gives .
For and , . Thus
At , , the right side factors as . Set , so and . Integrating the regions and gives, up to angular shifts and time reversal,
The constant , or , is the corresponding circular timelike orbit. The hyperbolic-tangent branch lies at and approaches that orbit from outside as ; the hyperbolic-cotangent branch lies at and approaches it from inside. Near the limit decays exponentially as . Since tends to , the limiting approach also takes infinite proper time. Neither nonconstant branch reaches and joins the circular orbit at a finite angular parameter.
Differentiating the orbit equation gives . A perturbation about obeys , showing that the circular orbit is unstable. The two explicit curves are its separatrix branches, not ordinary small stable oscillations. For the energy is marginally bound, so the outer critical branch is the limiting orbit between scattering and Schwarzschild marginally bound capture from infinity. Time-reversed inner and outer branches describe the corresponding approach or departure from that unstable orbit. These are the Explicit separatrices of the marginally bound Schwarzschild orbit.