Cauchy problem as a two-surface based ‘geometrodynamics’

Four-dimensional spacetimes foliated by a two-parameter family of homologous two-surfaces are considered in Einsteins theory of gravity. By combining a 1 + (1 + 2) decomposition, the canonical form of the spacetime metric and a suitable specification of the conformal structure of the foliating two-s...

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Veröffentlicht in:Classical and quantum gravity 2015-01, Vol.32 (1), p.15006-15033
1. Verfasser: Racz, Istvan
Format: Artikel
Sprache:eng
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Zusammenfassung:Four-dimensional spacetimes foliated by a two-parameter family of homologous two-surfaces are considered in Einsteins theory of gravity. By combining a 1 + (1 + 2) decomposition, the canonical form of the spacetime metric and a suitable specification of the conformal structure of the foliating two-surfaces, a gauge fixing is introduced. It is shown that, in terms of the chosen geometrically distinguished variables, the 1 + 3 Hamiltonian and momentum constraints can be recast into the form of a parabolic equation and a first order symmetric hyperbolic system, respectively. Initial data to this system can be given on one of the two-surfaces foliating the three-dimensional initial data surface. The 1 + 3 reduced Einsteins equations are also determined. By combining the 1 + 3 momentum constraint with the reduced system of the secondary 1 + 2 decomposition, a mixed hyperbolic-hyperbolic system is formed. It is shown that solutions to this mixed hyperbolic-hyperbolic system are also solutions to the full set of Einsteins equations provided that the 1 + 3 Hamiltonian constraint is solved on the initial data surface &${{\Sigma }_{0}}$; and the 1 + 2 Hamiltonian and momentum type expressions vanish on a world-tube yielded by the Lie transport of one of the two-surfaces foliating &${{\Sigma }_{0}}$; along the time evolution vector field. Whenever the foliating two-surfaces are compact without boundary in the spacetime and a regular origin exists on the time-slices-this is the location where the foliating two-surfaces smoothly reduce to a point-it suffices to guarantee that the 1 + 3 Hamiltonian constraint holds on the initial data surface. A short discussion on the use of the geometrically distinguished variables in identifying the degrees of freedom of gravity are also included.
ISSN:0264-9381
1361-6382
DOI:10.1088/0264-9381/32/1/015006