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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