Event horizons play an important role in relativistic astrophysics, especially for black holes, but also for other spacetimes. It is fundamental to be able to determine whether a given surface is an event horizon, a one-sided trap. Yet in the textbooks and lectures I know of, I cannot find any precise computational recipes that, when done, reveal the horizon character. Usually it is just stated and illustrated, for example by plotting the inclination of light cones.
I will formulate the question precisely using the example of Schwarzschild spacetime: at the Schwarzschild radius, (R=2GM/c^2) the metric diverges. We first examine it in terms of curvature, for which we calculate the corresponding curvature scalars from the Ricci tensor. We get that they are finite, smooth values, so there is no real singularity here, only a coordinate singularity was involved. Then we would have to show that this surface in turn functions as an event horizon. What kind of quantities can we calculate to determine this? Naively, I would think that one would have to admit: any world line that passes through it is such that if the test object is moving inwards, it does so at a velocity less than c, but if it is moving outwards, it would need a velocity v > c. What mathematical tool can be used to calculate this accurately? Or is it enough to look at the light-like motions? If we are at the Schwarzschild radius, then all light signals are such that if the time coordinate increases, the r coordinate cannot increase? How can we see this in a general way, and how can we conclude from this about time-like motions?
The question arises more significantly in the case of Kerr space-time. Here, two horizons and two infinite redshift surfaces result from the analysis of the metric tensor. What calculation proves that the inner boundary of the ergosphere is also an event horizon, but the outer one is not? It is also important to determine these precisely, since for rotating black holes, the possibility of a possible escape from the event horizon arises in the analysis of the maximal geodetic extension. The effective potential becomes repulsive at a point, the geodetic motion reverses and again passes through the r+ surface. So as not to be contradicted, it is usually resolved that this r+ surface is not the same as the r+ surface of our world through which we entered - but belongs to some other part of the world. This involves making a special topological choice. However, it is not clear that then the surface we call the external event horizon does not act as a trap one hundred percent? Could there be, in principle, world lines that we can exceptionally use to get out from under it?
The previous question leads us a far way, so my main question now is: what kind of precise calculations can we use to determine whether a suspicious surface is an event horizon?