Lemaître–Tolman metric

In mathematical physics, the Lemaître–Tolman metric is the spherically symmetric dust solution of Einstein's field equations was first found by Lemaître in 1933 and then Tolman in 1934. It was later investigated by Bondi in 1947. This solution describes a spherical cloud of dust (finite or infinite) that is expanding or collapsing under gravity. It is also known as the Lemaître-Tolman-Bondi metric and the Tolman metric.

The metric is:

\mathrm{d}s^{2} = \mathrm{d}t^2 - \frac{(R')^2}{1 + 2 E} \mathrm{d}r^2 - R^2 \, \mathrm{d}\Omega^2

where:

\mathrm{d}\Omega^2 = \mathrm{d}\theta^2 + \sin^2\theta \, \mathrm{d}\phi^2
R = R(t,r)~,~~~~~~~~ R' = \partial R / \partial r~,~~~~~~~~ E = E(r) > -\frac{1}{2}

The matter is comoving, which means its 4-velocity is:

u^a = \delta^a_0 = (1, 0, 0, 0)

so the spatial coordinates (r, \theta, \phi) are attached to the particles of dust.

The pressure is zero (hence dust), the density is

8 \pi \rho = \frac{2 M'}{R^2 \, R'}

and the evolution equation is

\dot{R}^2 = \frac{2 M}{R} + 2 E

where

\dot{R} = \partial R / \partial t

The evolution equation has three solutions, depending on the sign of E,

E > 0:~~~~~~~~ R = \frac{M}{2 E} (\cosh\eta - 1)~,~~~~~~~~ (\sinh\eta - \eta) = \frac{(2 E)^{3/2} (t - t_B)}{M}~;
E = 0:~~~~~~~~ R = \left( \frac{9 M (t - t_B)^2}{2} \right)^{1/3}~;
E < 0:~~~~~~~~ R = \frac{M}{2 E} (1 - \cos\eta)~,~~~~~~~~ (\eta - \sin\eta) = \frac{(-2 E)^{3/2} (t - t_B)}{M}~;

which are known as hyperbolic, parabolic, and elliptic evolutions respectively.

The meanings of the three arbitrary functions, which depend on r only, are:

Special cases are the Schwarzschild metric in geodesic coordinates M = constant, and the Friedmann–Lemaître–Robertson–Walker metric, e.g. E = 0~,~~ t_B = constant for the flat case.

See also

References


This article is issued from Wikipedia - version of the Wednesday, October 07, 2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.