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3.5 Geodesics of the Kerr Metric

55

where

 

gpp(r, Ω) = gtt + 2Ωg+ Ω2gφφ

(3.4.8)

If gpp(r, Ω) never changes sign (namely it is positive definite) then the effective 2- dimensional metric displays no horizon. If gpp(r, Ω) goes through zero, then in the p, r plane there is a horizon. However if there is a horizon for a certain time p(Ω) light can still escape to infinity along some other time p(Ω ) for which gpp(r, Ω ) is positive-definite. In other words we look for the norm of the Killing vectors χ (Ω):

χ (Ω), χ (Ω) = gtt + 2Ωg+ Ω2gφφ

(3.4.9)

If all the possible vectors χ (Ω) have negative norm then we are below the horizon. This implies that we are below the horizon when the discriminant of the quadratic form (3.4.8) is negative, so that the horizon is indeed given by the condition (3.4.3) as we claimed. On the horizon r = r+ the equation:

admits only one solution:

 

χ (Ω), χ (Ω) = 0

(3.4.10)

 

 

 

 

 

 

Ω

=

ΩH

 

 

α

 

 

α

(3.4.11)

 

 

 

 

 

 

 

 

 

 

 

 

 

 

r+2

+ α2

= α2 + (m + m2 q2 α2)2

 

 

 

The above quantity ΩH can be interpreted as the angular velocity of the eventhorizon in the sense that any physical test-body sitting on the horizon necessarily rotates with such a velocity with respect to the fixed stars.

The Horizon Area We can now easily calculate the area of the horizon. By definition we have:

AreaH =

 

dθ dφ = r

2

+ α2

 

sin θ dθ dφ

gθ θ gφφ

r=r+

 

+

 

 

 

= 4π r+2 + α2

 

 

 

(3.4.12)

and by comparison with (3.4.11) we obtain the following very interesting relation of the horizon area with the mass m and the angular momentum J of the black-hole:

J

AreaH = 4π (3.4.13)

ΩH m

3.5 Geodesics of the Kerr Metric

The Kerr metric was discovered at the beginning of the sixties of the XXth century but it took several years before the problem of integrating its geodesics equations

56

3 Rotating Black Holes and Thermodynamics

was solved. For the Schwarzschild field the geodesics equations are almost immediately reduced to quadratures by regarding them as Euler Lagrange equations of a mechanical problem with 4 Lagrangian coordinates qμ = (t, r, θ, φ) and exploiting two facts:

1.There are three first integrals of the motion respectively given by the energy E , the angular momentum L and the mass μ of the particle

2.One Lagrangian coordinate can be eliminated from start, since all orbits are pla-

nar and the declination angle θ can be conventionally fixed to the value θ = π2 without loss of generality.

In this way, after elimination of θ we have a number of conserved charges equal to the number of effective Lagrangian coordinates and the mechanical system is necessarily reduced to the quadratures. The really crucial point, therefore, is the elimination of θ which, in the Schwarzschild case might be seen as a consequence of the full-spherical symmetry, absent in the Kerr case. At α = 0 there is dynamics also in the declination angle θ , while at first glance, the integrals of motion seem to be just three as at α = 0. Hence integrability seem to be lost for the Kerr metric.

As Carter2 discovered, the truth is more subtle and the Kerr geodesic system is still fully integrable. The reason for that is the existence of a fourth hidden integral of motion, the Carter constant K, which exists at all values of α and is, in the limit α 0, the real source for the trivialization of the θ motion.

In order to discover the Carter constant one has to reformulate the geodesic problem within the framework of the Hamilton Jacobi approach to classical mechanics and this is what we shall do in the present section. As a preparation to this task let us first review the construction of the three integral of motion associated with manifest symmetries.

3.5.1 The Three Manifest Integrals, E , L and μ

The two first integrals E and L are associated with symmetries of the metric via Noether theorem (see Sect. 1.7 in Chap. 1 of Volume 1). They exist just because the two Lagrangian coordinates t and φ are cyclic. On its turn this cyclicity follows from

the existence of the two Killing vectors k = ∂/∂t and

˜

=

∂/∂φ

. These properties

 

k

 

 

are true for the Kerr metric as much as for the Schwarzschild one. Hence also the Kerr metric admits the first integrals E and L.

Defining the Lagrangian according to the conventions of used in Chaps. 3 and 4 of Volume 1 and using the form (3.2.10) of the Kerr metric in Boyes-Lindquist coordinates, namely:

L ≡ −

1

gμν (x)

dxμ dxν

 

 

 

 

2

dτ dτ

2Brandon Carter is an Australian born theoretical physicist working at Meudon (CNRS), France.

3.5 Geodesics of the Kerr Metric

 

 

 

 

 

 

 

 

˙

 

 

 

 

 

 

 

 

 

˙

 

 

 

57

 

 

 

ρ2r

 

 

ρ

θ

 

 

 

 

((r2

 

α2

 

 

 

 

 

 

 

 

 

 

 

 

αφ 2 θ )2

 

1

 

2

 

 

 

˙

 

+

 

+

 

 

 

αt)2 sin2 θ

 

 

 

 

 

 

= − 2

˙

+

 

2

2

 

 

 

 

ρ2

 

 

 

 

 

 

 

Δ(t

 

ρ2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

˙

 

 

 

 

 

 

 

 

 

 

 

 

 

 

˙ sin

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

(3.5.1)

we find the Kerr definition of the first integrals of motion E and L. Explicitly:

 

 

 

 

E =

 

t

 

∂t

=

1 ρ

2

t˙ + α ρ2

sin

 

 

θ

 

˙

 

 

 

 

 

 

 

 

p

 

 

 

∂L

 

 

 

2m

 

 

 

 

 

2mr

 

2

 

 

φ

(3.5.2)

 

 

 

 

 

 

 

 

 

 

 

˙

 

 

 

 

 

 

 

 

 

t˙ − ρ

 

 

 

 

 

 

 

 

 

 

L = pφ

 

 

=

 

 

 

 

 

 

 

 

 

 

 

 

 

θ ˙

 

 

 

 

 

 

 

φ

ρ2

 

sin

 

θ

2

 

sin

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

∂L

 

α

 

2mr

 

 

2

 

 

Σ2

 

 

2

 

φ

 

(3.5.3)

 

 

 

 

 

 

 

 

 

 

 

˙

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

where, adding the new shorthand Σ2 to the already introduced ones ρ2 and

 

, we

have:

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

ρ2 = r2 + α2 cos2 θ

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

= r2 2mr + α2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

(3.5.4)

 

 

 

 

Σ2 = r2 + α2 2 α2 r2 2mr + α2 sin2 θ

 

 

 

 

Equation (3.5.3) replace the homologous ones of the Schwarzschild case (see Chap. 3 of Volume One). In the limit α 0 the Kerr metric degenerates into the Schwarzschild metric and the definitions (3.5.3) of the energy and angular momen-

tum of a test particle flow to the Schwarzschild ones. This is easily checked, noting that at α = 0 we have ρ2 = = r2 and Σ2 = r4.

Equation (3.5.3) can be effectively interpreted in the following matrix form:

E

L = M(r, θ )

where the key point is that the 2 × 2 matrix:

M(r, θ )

 

1 ρ2

2

 

=

2m

 

 

2mr ρ2

 

 

 

α sin θ

t˙

˙

φ

2mrα sin2 θ ρ2

Σρ22

(3.5.5)

(3.5.6)

is function only of the coordinates r and θ . The same, obviously is true also of the inverse matrix.

 

 

 

ρ2Σ2

 

 

 

2mrαρ2 sin2 θ

 

 

M1(r, θ )

=

4m2r2α2 sin4 θ +22m)Σ2

 

4m2r2

α2 sin4(θ )+22m)Σ2

(3.5.7)

 

 

4m2r2α2 sin4 θ +2

2m)Σ2

4m2r2

α2 sin4 θ +22m)Σ2

 

 

 

 

2mrαρ2 sin2

θ

 

 

22ρ4

 

 

Hence if the geodesic flow of the coordinates r, θ has already been determined in terms of the first integral of motion, namely if we have the two proper-time functions:

r = r(τ, E, L);

θ = θ (τ, E, λ)

(3.5.8)

58 3 Rotating Black Holes and Thermodynamics

then the matrix M1 is reduced to a known function of τ and the inverse relation:

φ

= M

 

 

L

 

t˙

 

1(τ )

E

(3.5.9)

˙

 

 

 

 

reduces also the integration of the cyclic variables t and φ to quadratures.

The constant of motion μ2 is associated with fixing the reparameterization invariance of the geodesics equation. Indeed, in order for the Euler-Lagrange equations obtained from the Lagrangian (3.5.1) to be equivalent to the original geodesics equations it is necessary that the Lagrangian time τ should coincide with the proper time defined by the metric. This implies that we have to enforce the constraint:

 

 

1

2

 

time-like geodesics

 

L

=

μ2 where μ2

= 1;

(3.5.10)

2

 

 

μ

= 0;

light-like geodesics

 

 

 

 

 

This condition yields the third manifest integral of motion:

 

2

 

ρ2r

2

 

2

 

2

 

((r2

α2

 

αt)2 sin2 θ

 

Δ(t

αφ

2 θ )2

 

=

 

 

 

+

˙

+

 

˙

 

 

˙ sin

 

 

μ

 

 

 

˙

 

 

ρ

θ

 

 

+

 

˙

 

˙ −

 

(3.5.11)

3.5.2 The Hamilton-Jacobi Equation and the Carter Constant

Let us recall the essential points of the Hamilton Jacobi method of integration of a Hamiltonian system.

Given the Hamiltonian:

H (p, q) = pi q˙i L (q, q)˙

(3.5.12)

where the canonical momenta pi Lq˙i are defined as usual, the Hamilton Jacobi method consists of constructing the generating function S(τ, p, q) of a canonical transformation which reduces the new Hamiltonian H to an identically vanishing function of the new canonical variables (P , Q). In this way we will be guaranteed that both the new canonical coordinates Qi and the new canonical momenta Pi are constant, since:

0

Qi

 

∂H

P

∂H

(3.5.13)

 

 

 

 

= ∂Pi ;

 

 

= ˙

0 = ˙i = −

∂Qi

 

Calling S(q, P , τ ) the generating function of such a canonical transformation, where qi are the old coordinates and Pi the new momenta, by definition we have the relations:

pi =

∂S(τ, q, P )

 

 

∂qi

 

(3.5.14)

Qi =

∂S(τ, q, P )

 

 

∂P i

3.5 Geodesics of the Kerr Metric

59

which, provided that S(τ, q, P ) is known, yields the explicit solution of the mechanical problem under consideration. Such solution is the complete integral since it involves exactly 2n integration constants that are nothing else but the new canonical momenta and coordinates (P , Q). The function S is named the Jacobi principal function and, as a consequence of its definition, it satisfies the Hamilton Jacobi equation:

∂S

+ H

qi ,

∂S

= 0

(3.5.15)

 

 

∂τ

∂qi

The question is whether the Hamilton-Jacobi equation can be integrated more easily than the original Hamiltonian equations. This happens when (3.5.15) is such that it allows for a separation of the variables. By this we mean that it is consistent to write the following ansatz for the function S(τ, q, P ):

n

 

 

i 1

S(τ, q, P ) = E τ + Wi qi , Pi

(3.5.16)

=

where each function Wi depends only on the corresponding old canonical variable qi . When this is the case the integration of the Hamilton Jacobi equation can be reduced to the quadratures.

Applying the Hamilton-Jacobi method to the problem of geodesics, the first thing that we note is one of a general character, common to any metric. Since the Lagrangian is a quadratic form in the velocities, with coordinate dependent coefficients, the Hamiltonian will be a quadratic form in the canonical momenta with coordinate dependent coefficients. Indeed in full generality we obtain:

pμ ≡ −gμν (q)q˙ν

 

 

 

 

1

gμν (q)pμpν

 

H (q, p) = −

 

(3.5.17)

2

where gμν is the controvariant metric with upper indices.

 

 

 

 

In the case of the Kerr-metric we have:

 

 

 

 

 

 

 

 

 

 

 

 

Σ2

0

 

0

 

2mrα

 

 

 

 

 

 

 

Δρ2

 

 

 

Δρ2

 

 

 

 

 

 

0

 

 

0

 

0

 

 

 

 

 

 

g

μν

 

ρ2

1

 

 

 

 

(3.5.18)

 

0

 

0

 

 

0

 

 

 

 

 

 

=

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

ρ2

 

 

 

 

 

 

 

 

 

 

2mrα

0

 

 

csc2 θ (α2 sin2 θ

Δ)

 

 

 

 

 

 

 

0

 

 

 

 

 

 

 

 

 

 

 

Δρ2

 

 

 

 

 

 

Δρ2

 

 

 

 

where the chosen order of the coordinates is (t, r, θ, φ). Correspondingly the Hamiltonian takes the explicit form:

H (p, q) =

2pr2

+ Σ2pt2 Δpθ2 + α2pφ2 csc2(θ )pφ2 + 4mrαpt pφ

 

2Δρ2

(3.5.19) which provides the explicit form of the Hamilton-Jacobi equation. Recalling the first integrals (3.5.3) we try the following factorized ansatz for the principal Jacobi

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