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Geodesics of the Kerr metric

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Therefore, once we have solved (4.97), we have <strong>the</strong> expressions <strong>of</strong><br />

<strong>the</strong> conjugate momenta (and <strong>the</strong>n <strong>of</strong> ẋ µ ) in terms <strong>of</strong> four constants,<br />

which allow to write <strong>the</strong> solutions <strong>of</strong> <strong>the</strong> geodesic equation in a<br />

closed form, in terms <strong>of</strong> integrals.<br />

In general, it is more difficult to solve (4.97), which is a partial<br />

differential equation, than to solve <strong>the</strong>geodesicequation,butinthis<br />

case we can find such a solution.<br />

First <strong>of</strong> all, we can use what we already know, i.e.<br />

These conditions require that<br />

H = 1 2 gµν p µ p ν = 1 2 κ<br />

p t = −E constant<br />

p φ = L constant . (4.99)<br />

S = − 1 2 κλ − Et + Lφ + S(rθ) (r, θ) (4.100)<br />

where S (rθ) is a function <strong>of</strong> r and θ to be determined.<br />

Fur<strong>the</strong>rmore, we look for a separable solution, by making <strong>the</strong><br />

ansatz<br />

S = − 1 2 κλ − Et + Lφ + S(r) (r)+S (θ) (θ) . (4.101)<br />

Substituting (4.101) into <strong>the</strong> Hamilton-Jacobi equation (4.97), and<br />

using <strong>the</strong> expression (3.16) for <strong>the</strong> inverse <strong>metric</strong>, we find<br />

−κ + ∆ ( ) dS<br />

(r) 2<br />

+ 1 ( ) dS<br />

(θ) 2<br />

Σ dr Σ dθ<br />

− 1 ]<br />

[r 2 + a 2 + 2Mra2<br />

∆<br />

Σ<br />

sin2 θ E 2 + 4Mra<br />

Σ∆ EL + ∆ − a2 sin 2 θ<br />

Σ∆ sin 2 θ L2 =0.<br />

(4.102)<br />

Using <strong>the</strong> relation (3.12)<br />

(r 2 + a 2 )+ 2Mra2<br />

Σ<br />

sin2 θ = 1 Σ<br />

and multiplying by Σ = r 2 + a 2 cos 2 θ,weget<br />

( ) dS<br />

−κ(r 2 + a 2 cos 2 (r) 2 ( dS<br />

(θ)<br />

θ)+∆ +<br />

dr dθ<br />

[<br />

(r 2 + a 2 ) 2 − a 2 sin 2 θ∆ ] (4.103)<br />

86<br />

) 2

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