In the limit that the charge (or equivalently, the length scale) goes to zero, one recovers theSchwarzschild metric. The classical Newtonian theory of gravity may then be recovered in the limit as the ratio goes to zero. In the limit that both and go to zero, the metric becomes theMinkowski metric forspecial relativity.
In practice, the ratio is often extremely small. For example, the Schwarzschild radius of theEarth is roughly9 mm. Even at the surface of the Earth, the corrections to Newtonian gravity are only one part in a billion. The ratio only becomes large close toblack holes and other ultra-dense objects such asneutron stars.
Although charged black holes with are similar to theSchwarzschild black hole, they have two horizons: theevent horizon and an internalCauchy horizon.[8] As with the Schwarzschild metric, the event horizons for the spacetime are located where the metric component diverges; that is, where
If magnetic monopoles are included in the theory, then a generalization to include magnetic charge is obtained by replacing by in the metric and including the term in the electromagnetic potential.[clarification needed]
Instead of working in the holonomic basis, one can perform efficient calculations with atetrad.[13] Let be a set ofone-forms with internalMinkowski index, such that. The Reissner metric can be described by the tetrad
where. Theparallel transport of the tetrad is captured by theconnection one-forms. These have only 24 independent components compared to the 40 components of. The connections can be solved for by inspection from Cartan's equation, where the left hand side is theexterior derivative of the tetrad, and the right hand side is awedge product.
TheRiemann tensor can be constructed as a collection of two-forms by the second Cartan equation which again makes use of the exterior derivative and wedge product. This approach is significantly faster than the traditional computation with; note that there are only four nonzero compared with nine nonzero components of.
Because of thespherical symmetry of the metric, the coordinate system can always be aligned in a way that the motion of a test-particle is confined to a plane. For brevity andwithout loss of generality one may use instead of. In dimensionless natural units of, the motion of an electrically charged particle with the charge is given bywhich yields
All total derivatives are with respect to proper time.
Constants of the motion are provided by solutions to the partial differential equation[15]after substitution of the second derivatives given above. The metric itself is a solution when written as a differential equation
The separable equationimmediately yields the constant relativistic specific angular momentuma third constant obtained fromis the specific energy (energy per unit rest mass)[16]
Substituting and into yields the radial equation
Multiplying under the integral sign by yields the orbital equation
The totaltime dilation between the test-particle and an observer at infinity is
The first derivatives and thecontravariant components of the local 3-velocity are related bywhich gives the initial conditions
Thespecific orbital energyand thespecific relative angular momentumof the test-particle are conserved quantities of motion. and are the radial and transverse components of the local velocity-vector. The local velocity is therefore
^Nordström, G. (1918). "On the Energy of the Gravitational Field in Einstein's Theory".Koninklijke Nederlandsche Akademie van Wetenschappen Proceedings.20 (2):1238–1245.Bibcode:1918KNAB...20.1238N.
^Chandrasekhar, Subrahmanyan (2009).The mathematical theory of black holes. Oxford classic texts in the physical sciences (Reprinted ed.). Oxford: Clarendon Press. p. 205.ISBN978-0-19-850370-5.And finally, the fact that the Reissner–Nordström solution has two horizons, an external event horizon and an internal 'Cauchy horizon', provides a convenient bridge to the study of the Kerr solution in the subsequent chapters.
^Misner, Charles W.; Thorne, Kip S.; Wheeler, John Archibald; Kaiser, David; et al. (2017).Gravitation. Princeton, N.J: Princeton University Press. pp. 656–658.ISBN978-0-691-17779-3.OCLC1006427790.