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Geodesics of the Kerr metric

Geodesics of the Kerr metric

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where Σ ,θ = −2a 2 sin θ cos θ and Σ ,r =2r. It is easy to check that<br />

θ ≡ π/2 is a solution <strong>of</strong> equation (4.13).<br />

If, at λ = 0, <strong>the</strong> particles moves in <strong>the</strong> equatorial plane, θ(λ =<br />

0) = π/2 and ˙θ(λ =0)=0;<strong>the</strong>nwehaveawell-posedCauchy<br />

problem <strong>of</strong> <strong>the</strong> form<br />

¨θ = ...<br />

˙θ(λ =0) = 0<br />

θ(λ =0) = π 2<br />

(4.15)<br />

which admits one and only one solution; since θ ≡ π/2 is a solution,<br />

it is <strong>the</strong> solution. Thus, a geodesic which starts in <strong>the</strong> equatorial<br />

plane, remains in <strong>the</strong> equatorial plane.<br />

This also happens in <strong>the</strong> Schwarzschild <strong>metric</strong>. But, while in that<br />

case it is possible to generalize <strong>the</strong> result to any orbit, thanks to <strong>the</strong><br />

spherical symmetry, and prove that allSchwarzschildgeodesicsare<br />

planar, such a generalization is not possible for <strong>the</strong> <strong>Kerr</strong> <strong>metric</strong><br />

which is axially sym<strong>metric</strong>. We only can say that geodesics starting<br />

in <strong>the</strong> equatorial plane are planar.<br />

On <strong>the</strong> equatorial plane, Σ = r 2 ,<strong>the</strong>refore<br />

(<br />

g tt = − 1 − 2M )<br />

r<br />

and<br />

E = −g tµ u µ =<br />

g tφ = − 2Ma<br />

r<br />

g rr = r2<br />

∆<br />

g φφ = r 2 + a 2 + 2Ma2<br />

r<br />

(<br />

1 − 2M r<br />

L = g φµ u µ = − 2Ma ṫ +<br />

r<br />

(4.16)<br />

)<br />

ṫ + 2Ma ˙φ (4.17)<br />

r<br />

)<br />

(r 2 + a 2 + 2Ma2 ˙φ. (4.18)<br />

r<br />

To solve (4.17), (4.18) for ṫ, ˙φ we define<br />

A ≡ 1 − 2M r<br />

70

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