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4.3 Scalar Green’s functions in curved spacetime

4.3.1 Green’s equation for a massless scalar field in curved spacetime

We consider a massless scalar field Φ(x) in a curved spacetime with metric gαβ. The field satisfies the wave equation

(□ − ξR )Φ (x ) = − 4π μ(x), (266 )
where □ = g αβ∇ α∇ β is the wave operator, R the Ricci scalar, ξ an arbitrary coupling constant, and μ (x ) is a prescribed source. We seek a Green’s function G (x,x′) such that a solution to Equation (266View Equation) can be expressed as
∫ ∘ ---- Φ (x) = G (x,x ′)μ(x ′) − g′d4x′, (267 )
where the integration is over the entire spacetime. The wave equation for the Green’s function is
′ ′ (□ − ξR )G (x, x ) = − 4π δ4(x, x), (268 )
where δ4(x, x′) is the invariant Dirac functional introduced in Section 4.2.1. It is easy to verify that the field defined by Equation (267View Equation) is truly a solution to Equation (266View Equation).

We let ′ G+ (x,x ) be the retarded solution to Equation (268View Equation), and ′ G− (x,x ) be the advanced solution; when viewed as functions of x, G+ (x, x′) is nonzero in the causal future of x ′, while G − (x, x′) is nonzero in its causal past. We assume that the retarded and advanced Green’s functions exist as distributions and can be defined globally in the entire spacetime.

4.3.2 Hadamard construction of the Green’s functions

Assuming throughout this section that x is restricted to the normal convex neighbourhood of x ′, we make the ansatz

′ ′ ′ G ±(x,x ) = U (x,x )δ±(σ) + V (x,x )θ±(− σ), (269 )
where U(x, x′) and V(x,x ′) are smooth biscalars; the fact that the spacetime is no longer homogeneous means that these functions cannot depend on σ alone.

Before we substitute the Green’s functions of Equation (269View Equation) into the differential equation of Equation (268View Equation), we proceed as in Section 4.1.6 and shift σ by the small positive quantity ε. We shall therefore consider the distributions

G ε (x, x′) = U (x,x ′)δ (σ + ε) + V (x,x′)θ (− θ − ε), ± ± ±

and later recover the Green’s functions by taking the limit ε → 0+. Differentiation of these objects is straightforward, and in the following manipulations we will repeatedly use the relation σασ α = 2σ satisfied by the world function. We will also use the distributional identities σδ (σ + ε) = − εδ (σ + ε) ± ±, ′ ′ σ δ±(σ + ε) = − δ± (σ + ε) − εδ± (σ + ε), and ′′ ′ ′′ σ δ±(σ + ε) = − 2δ(σ + ε) − εδ (σ + ε). After a routine calculation we obtain

(□ − ξR)G ε = − 2εδ′′(σ + ε)U + 2εδ′(σ + ε)V + δ ′(σ + ε){2U σ α + (σ α − 4 )U } ± ± ±α α ± ,α α + δ±(σ + ε){− 2V,ασ + (2 − σ α)V + (□ − ξR )U } + θ±(− σ − ε){(□ − ξR)V } ,
which becomes
(□ − ξR )G ± = − 4πδ4(x,x ′)U + δ′±(σ){2U, ασα + (σαα − 4)U } + δ (σ){− 2V σ α + (2 − σ α)V + (□ − ξR )U } + θ (− σ){(□ − ξR )V} (270 ) ± ,α α ±
in the limit ε → 0+, after using the identities of Equations (263View Equation, 264View Equation, 265View Equation).

According to Equation (268View Equation), the right-hand side of Equation (270View Equation) should be equal to − 4πδ4(x,x′). This immediately gives us the coincidence condition

[U ] = 1 (271 )
for the biscalar U (x, x′). To eliminate the δ′ ± term we make its coefficient vanish:
α α 2U,ασ + (σ α − 4)U = 0. (272 )
As we shall now prove, these two equations determine U (x, x′) uniquely.

Recall from Section 2.1.3 that σα is a vector at x that is tangent to the unique geodesic β that connects x to ′ x. This geodesic is affinely parameterized by λ and a displacement along β is described by α α dx = (σ ∕λ )d λ. The first term of Equation (272View Equation) therefore represents the rate of change of U (x,x′) along β, and this can be expressed as 2λ dU∕d λ. For the second term we recall from Section 2.5.1 the differential equation Δ− 1(Δ σ α);α = 4 satisfied by Δ (x,x′), the van Vleck determinant. This gives us σ α − 4 = Δ − 1Δ σα = Δ − 1λ dΔ ∕dλ α ,α, and Equation (272View Equation) becomes

d λ--- (2 ln U − ln Δ ) = 0. d λ

It follows that 2 U ∕Δ is constant on β, and it must therefore be equal to its value at the starting point x′: U2∕Δ = [U 2∕Δ ] = 1, by virtue of Equation (271View Equation) and the property [Δ ] = 1 of the van Vleck determinant. Since this statement must be true for all geodesics β that emanate from x′, we have found that the unique solution to Equations (271View Equation) and (272View Equation) is

′ 1∕2 ′ U (x,x ) = Δ (x,x ). (273 )

We must still consider the remaining terms in Equation (270View Equation). The δ± term can be eliminated by demanding that its coefficient vanish when σ = 0. This, however, does not constrain its value away from the light cone, and we thus obtain information about V |σ=0 only. Denoting this by ˇV (x,x′) – the restriction of V (x, x′) on the light cone σ(x,x ′) = 0 – we have

1 1 || ˇV,ασα + --(σαα − 2)Vˇ = --(□ − ξR )U || , (274 ) 2 2 σ=0
where we indicate that the right-hand side also must be restricted to the light cone. The first term of Equation (274View Equation) can be expressed as ˇ λdV ∕dλ, and this equation can be integrated along any null geodesic that generates the null cone ′ σ (x, x ) = 0. For these integrations to be well posed, however, we must provide initial values at x = x ′. As we shall now see, these can be inferred from Equation (274View Equation) and the fact that V(x,x ′) must be smooth at coincidence.

Equations (97View Equation) and (273View Equation) imply that near coincidence, U (x, x′) admits the expansion

-1- α′ β′ 3 U = 1 + 12R α′β′σ σ + 𝒪 (λ ), (275 )
where Rα′β′ is the Ricci tensor at ′ x and λ is the affine-parameter distance to x (which can be either on or off the light cone). Differentiation of this relation gives
U,α = − 1-gα′R α′β′σ β′ + 𝒪 (λ2), U,α′ = 1-Rα′β′σ β′ + 𝒪 (λ2), (276 ) 6 α 6
and eventually,
1- ′ [□U ] = 6 R(x ). (277 )
Using also α [σ α] = 4, we find that the coincidence limit of Equation (274View Equation) gives
-1- ′ [V ] = 12 (1 − 6ξ) R(x ), (278 )
and this provides the initial values required for the integration of Equation (274View Equation) on the null cone.

Equations (274View Equation) and (278View Equation) give us a means to construct ˇV(x,x ′), the restriction of V (x, x′) on the null cone σ(x,x ′) = 0. These values can then be used as characteristic data for the wave equation

′ (□ − ξR)V (x,x ) = 0, (279 )
which is obtained by elimination of the θ± term in Equation (270View Equation). While this certainly does not constitute a practical method to compute the biscalar ′ V(x,x ), these considerations show that ′ V (x,x ) exists and is unique.

To summarize: We have shown that with U (x,x′) given by Equation (273View Equation) and V (x,x′) determined uniquely by the wave equation of Equation (279View Equation) and the characteristic data constructed with Equations (274View Equation) and (278View Equation), the retarded and advanced Green’s functions of Equation (269View Equation) do indeed satisfy Equation (268View Equation). It should be emphasized that the construction provided in this section is restricted to 𝒩 (x ′), the normal convex neighbourhood of the reference point x ′.

4.3.3 Reciprocity

We shall now establish the following reciprocity relation between the (globally defined) retarded and advanced Green’s functions:

′ ′ G − (x ,x) = G+ (x,x ). (280 )
Before we get to the proof we observe that by virtue of Equation (280View Equation), the biscalar V (x,x ′) must be symmetric in its arguments,
′ ′ V(x ,x) = V (x,x ). (281 )
To go from Equation (280View Equation) to Equation (281View Equation) we need simply note that if x ∈ 𝒩 (x′) and belongs to I+ (x′), then G+ (x,x ′) = V (x,x′) and G − (x′,x) = V (x′,x ).

To prove the reciprocity relation we invoke the identities

′ ′′ ′ ′′ G+ (x,x )(□ − ξR )G − (x,x ) = − 4πG+ (x, x )δ4(x,x )


G − (x, x′′)(□ − ξR )G+ (x,x′) = − 4πG − (x,x ′′)δ4(x, x′),

and take their difference. On the left-hand side we have

′ ′′ ′′ ′ G+ (x,x )□G − (x,x ) − G − (x,x )□G+ (x,x ) = ∇ (G (x,x ′)∇ αG (x,x ′′) − G (x, x′′)∇ αG (x,x′)), α + − − +
while the right-hand side gives
′ ′′ ′′ ′ − 4π (G+ (x,x )δ4(x,x ) − G − (x,x )δ4(x,x )).

Integrating both sides over a large four-dimensional region V that contains both x′ and x′′, we obtain

∮ ′ α ′′ ′′ α ′ ′′ ′ ′ ′′ (G+ (x,x )∇ G − (x,x ) − G − (x,x )∇ G+ (x,x )) dΣ α = − 4π (G+ (x ,x ) − G − (x ,x )), ∂V

where ∂V is the boundary of V. Assuming that the Green’s functions fall off sufficiently rapidly at infinity (in the limit ∂V → ∞; this statement imposes some restriction on the spacetime’s asymptotic structure), we have that the left-hand side of the equation evaluates to zero in the limit. This gives us the statement ′′ ′ ′ ′′ G+ (x ,x ) = G− (x,x ), which is just Equation (280View Equation) with ′′ x replacing x.

4.3.4 Kirchhoff representation

Suppose that the values for a scalar field Φ(x′) and its normal derivative ′ nα ∇ α′Φ(x′) are known on a spacelike hypersurface Σ. Suppose also that the scalar field satisfies the homogeneous wave equation

(□ − ξR )Φ (x ) = 0. (282 )
Then the value of the field at a point x in the future of Σ is given by Kirchhoff’s formula,
∫ ( ) Φ(x) = − -1- G+ (x,x′)∇ α′Φ (x′) − Φ (x′)∇ α′G+ (x,x′) dΣ α′, (283 ) 4π Σ
where dΣ ′ α is the surface element on Σ. If n ′ α is the future-directed unit normal, then dΣ α′ = − n α′dV, with dV denoting the invariant volume element on Σ; notice that dΣ α′ is past directed.

To establish this result we start with the equations

G − (x′,x)(□ ′ − ξR ′)Φ (x′) = 0, Φ (x′)(□ ′ − ξR ′)G − (x ′,x) = − 4π δ4(x ′,x)Φ (x′),

in which x and x′ refer to arbitrary points in spacetime. Taking their difference gives

( ) ∇ ′ G (x′,x)∇ α′Φ(x′) − Φ(x′)∇ α′G (x′,x) = 4πδ (x′,x)Φ(x ′), α − − 4

and this we integrate over a four-dimensional region V that is bounded in the past by the hypersurface Σ. We suppose that V contains x and we obtain

∮ ( ′ ′ ) G− (x′,x )∇α Φ (x′) − Φ (x′)∇ α G − (x′,x) dΣ α′ = 4π Φ(x ), ∂V

where dΣα ′ is the outward-directed surface element on the boundary ∂V. Assuming that the Green’s function falls off sufficiently rapidly into the future, we have that the only contribution to the hypersurface integral is the one that comes from Σ. Since the surface element on Σ points in the direction opposite to the outward-directed surface element on ∂V, we must change the sign of the left-hand side to be consistent with the convention adopted previously. With this change we have

∮ ( ) 1-- ′ α′ ′ ′ α′ ′ ′ Φ (x ) = − 4π ∂V G − (x ,x)∇ Φ(x ) − Φ (x )∇ G − (x ,x) dΣ α ,

which is the same as Equation (283View Equation) if we take into account the reciprocity relation of Equation (280View Equation).

4.3.5 Singular and radiative Green’s functions

In Section 5 of this review we will compute the retarded field of a moving scalar charge, and we will analyze its singularity structure near the world line; this will be part of our effort to understand the effect of the field on the particle’s motion. The retarded solution to the scalar wave equation is the physically relevant solution because it properly incorporates outgoing-wave boundary conditions at infinity – the advanced solution would come instead with incoming-wave boundary conditions. The retarded field is singular on the world line because a point particle produces a Coulomb field that diverges at the particle’s position. In view of this singular behaviour, it is a subtle matter to describe the field’s action on the particle, and to formulate meaningful equations of motion.

When facing this problem in flat spacetime (recall the discussion of Section 1.3), it is convenient to decompose the retarded Green’s function ′ G+ (x, x) into a singular Green’s function GS (x,x′) ≡ 12[G+ (x,x′) + G − (x, x′)] and a radiative Green’s function GR (x,x ′) ≡ 12[G+ (x,x′) − G− (x,x′)]. The singular Green’s function takes its name from the fact that it produces a field with the same singularity structure as the retarded solution: The diverging field near the particle is insensitive to the boundary conditions imposed at infinity. We note also that ′ GS (x, x) satisfies the same wave equation as the retarded Green’s function (with a Dirac functional as a source), and that by virtue of the reciprocity relations, it is symmetric in its arguments. The radiative Green’s function, on the other hand, takes its name from the fact that it satisfies the homogeneous wave equation, without the Dirac functional on the right-hand side; it produces a field that is smooth on the world line of the moving scalar charge.

Because the singular Green’s function is symmetric in its argument, it does not distinguish between past and future, and it produces a field that contains equal amounts of outgoing and incoming radiation – the singular solution describes standing waves at infinity. Removing GS (x,x ′) from the retarded Green’s function will therefore have the effect of removing the singular behaviour of the field without affecting the motion of the particle. The motion is not affected because it is intimately tied to the boundary conditions: If the waves are outgoing, the particle loses energy to the radiation and its motion is affected; if the waves are incoming, the particle gains energy from the radiation and its motion is affected differently. With equal amounts of outgoing and incoming radiation, the particle neither loses nor gains energy and its interaction with the scalar field cannot affect its motion. Thus, subtracting GS (x,x ′) from the retarded Green’s function eliminates the singular part of the field without affecting the motion of the scalar charge. The subtraction leaves behind the radiative Green’s function, which produces a field that is smooth on the world line; it is this field that will govern the motion of the particle. The action of this field is well defined, and it properly encodes the outgoing-wave boundary conditions: The particle will lose energy to the radiation.

In this section we attempt a decomposition of the curved-spacetime retarded Green’s function into singular and radiative Green’s functions. The flat-spacetime relations will have to be amended, however, because of the fact that in a curved spacetime, the advanced Green’s function is generally nonzero when x ′ is in the chronological future of x. This implies that the value of the advanced field at x depends on events ′ x that will unfold in the future; this dependence would be inherited by the radiative field (which acts on the particle and determines its motion) if the naive definition GR (x,x ′) ≡ 12[G+ (x,x ′) − G − (x,x′)] were to be adopted.

We shall not adopt this definition. Instead, we shall follow Detweiler and Whiting [23Jump To The Next Citation Point] and introduce a singular Green’s function with the properties

  Sc.S1: GS (x,x′) satisfies the inhomogeneous scalar wave equation,

(□ − ξR)G (x,x′) = − 4πδ (x,x′); (284 ) S 4

  Sc.S2: ′ GS (x,x ) is symmetric in its arguments,

′ ′ GS (x ,x) = GS (x,x ); (285 )

  Sc.S3: ′ GS (x,x ) vanishes if x is in the chronological past or future of ′ x,

′ ± ′ GS (x,x ) = 0 when x ∈ I (x). (286 )

Properties Sc.S1 and Sc.S2 ensure that the singular Green’s function will properly reproduce the singular behaviour of the retarded solution without distinguishing between past and future; and as we shall see, Property Sc.S3 ensures that the support of the radiative Green’s function will not include the chronological future of x.

The radiative Green’s function is then defined by

′ ′ ′ GR (x, x) = G+ (x, x) − GS (x,x ), (287 )
where G+ (x,x′) is the retarded Green’s function. This comes with the properties

  Sc.R1: ′ GR (x, x) satisfies the homogeneous wave equation,

′ (□ − ξR )GR (x,x ) = 0; (288 )

  Sc.R2: GR (x,x ′) agrees with the retarded Green’s function if x is in the chronological future of x′,

′ ′ + ′ GR (x,x ) = G+ (x,x ) when x ∈ I (x ); (289 )

  Sc.R3: GR (x, x′) vanishes if x is in the chronological past of x′,

′ − ′ GR (x,x ) = 0 when x ∈ I (x ). (290 )

Property Sc.R1 follows directly from Equation (287View Equation) and Property Sc.S1 of the singular Green’s function. Properties Sc.R2 and Sc.R3 follow from Property Sc.S3 and the fact that the retarded Green’s function vanishes if x is in past of x′. The properties of the radiative Green’s function ensure that the corresponding radiative field will be smooth at the world line, and will depend only on the past history of the scalar charge.

We must still show that such singular and radiative Green’s functions can be constructed. This relies on the existence of a two-point function H (x,x′) that would possess the properties

  Sc.H1: ′ H (x, x) satisfies the homogeneous wave equation,

(□ − ξR )H (x,x ′) = 0; (291 )

  Sc.H2: ′ H (x, x) is symmetric in its arguments,

′ ′ H (x ,x) = H (x,x ); (292 )

  Sc.H3: H (x, x′) agrees with the retarded Green’s function if x is in the chronological future of x′,

′ ′ + ′ H (x, x) = G+ (x, x) when x ∈ I (x ); (293 )

  Sc.H4: H (x, x′) agrees with the advanced Green’s function if x is in the chronological past of x′,

′ ′ − ′ H (x, x ) = G − (x, x ) when x ∈ I (x ). (294 )

With a biscalar H (x,x ′) satisfying these relations, a singular Green’s function defined by

G (x, x′) = 1[G (x,x′) + G (x,x′) − H (x, x′)] (295 ) S 2 + −
will satisfy all the properties listed previously: Property Sc.S1 comes as a consequence of Property Sc.H1 and the fact that both the advanced and the retarded Green’s functions are solutions to the inhomogeneous wave equation, Property Sc.S2 follows directly from Property Sc.H2 and the definition of Equation (295View Equation), and Property Sc.S3 comes as a consequence of Properties Sc.H3, Property Sc.H4 and the properties of the retarded and advanced Green’s functions.

The question is now: Does such a function H (x, x′) exist? I will present a plausibility argument for an affirmative answer. Later in this section we will see that ′ H (x, x) is guaranteed to exist in the local convex neighbourhood of x′, where it is equal to V (x,x′). And in Section 4.3.6 we will see that there exist particular spacetimes for which H (x,x′) can be defined globally.

To satisfy all of Properties Sc.H4, Sc.H2, Sc.H3, and Sc.H4 might seem a tall order, but it should be possible. We first note that Property Sc.H4 is not independent from the rest: It follows from Property Sc.H2, Property Sc.H3, and the reciprocity relation (280View Equation) satisfied by the retarded and advanced Green’s functions. Let x ∈ I− (x′), so that x′ ∈ I+ (x). Then H (x,x ′) = H (x′,x) by Property Sc.H2, and by Property Sc.H3 this is equal to G+ (x′,x). But by the reciprocity relation this is also equal to G (x, x′) −, and we have obtained Property Sc.H4. Alternatively, and this shall be our point of view in the next paragraph, we can think of Property Sc.H3 as following from Properties Sc.H2 and Sc.H4.

Because H (x,x ′) satisfies the homogeneous wave equation (Property Sc.H1), it can be given the Kirkhoff representation of Equation (283View Equation): If Σ is a spacelike hypersurface in the past of both x and x ′, then

∫ ′ 1 ( ′′ α′′ ′′ ′ ′′ ′ α′′ ′′ ) H (x,x ) = − 4π- G+ (x, x )∇ H (x ,x ) − H (x ,x)∇ G+ (x,x ) dΣα′′, Σ

where dΣα′′ is a surface element on Σ. The hypersurface can be partitioned into two segments, Σ − (x ′) and Σ − Σ − (x′), with Σ − (x′) denoting the intersection of Σ with I− (x′). To enforce Property Sc.H4 it suffices to choose for ′ H (x, x) initial data on − ′ Σ (x ) that agree with the initial data for the advanced Green’s function; because both functions satisfy the homogeneous wave equation in I− (x ′), the agreement will be preserved in all of the domain of dependence of Σ − (x′). The data on Σ − Σ− (x′) is still free, and it should be possible to choose it so as to make ′ H (x,x ) symmetric. Assuming that this can be done, we see that Property Sc.H2 is enforced and we conclude that the Properties Sc.H1, Sc.H2, Sc.H3, and Sc.H4 can all be satisfied.

When x is restricted to the normal convex neighbourhood of x′, Properties Sc.H1, Sc.H2, Sc.H3, and Sc.H4 imply that

H (x,x ′) = V (x,x′); (296 )
it should be stressed here that while ′ H (x, x) is assumed to be defined globally in the entire spacetime, the existence of ′ V (x,x ) is limited to ′ 𝒩 (x ). With Equations (269View Equation) and (295View Equation) we find that the singular Green’s function is given explicitly by
1 1 GS (x,x ′) = --U(x, x′)δ(σ ) −--V (x, x′)θ(σ ) (297 ) 2 2
in the normal convex neighbourhood. Equation (297View Equation) shows very clearly that the singular Green’s function does not distinguish between past and future (Property Sc.S2), and that its support excludes I ±(x′), in which θ(σ) = 0 (Property Sc.S3). From Equation (287View Equation) we get an analogous expression for the radiative Green’s function:
[ ] ′ 1 ′ ′ 1 GR (x,x ) = 2U (x,x )[δ+(σ) − δ− (σ )] + V (x,x ) θ+ (− σ ) + 2-θ(σ) . (298 )
This reveals directly that the radiative Green’s function coincides with G+ (x,x ′) in I+(x′), in which θ(σ ) = 0 and θ+(− σ) = 1 (Property Sc.R2), and that its support does not include I− (x′), in which θ(σ ) = θ (− σ) = 0 + (Property Sc.R3).

4.3.6 Example: Cosmological Green’s functions

To illustrate the general theory outlined in the previous Sections 4.3.1, 4.3.2, 4.3.3, 4.3.4, and 4.3.5, we consider here the specific case of a minimally-coupled (ξ = 0) scalar field in a cosmological spacetime with metric

2 2 2 2 2 2 ds = a (η)(− dη + dx + dy + dz ), (299 )
where a(η) is the scale factor expressed in terms of conformal time. For concreteness we take the universe to be matter dominated, so that a(η) = C η2, where C is a constant. This spacetime is one of the very few for which Green’s functions can be explicitly constructed. The calculation presented here was first carried out by Burko, Harte, and Poisson [15]; it can be extended to other cosmologies.

To solve Green’s equation □G (x,x ′) = − 4πδ4(x,x ′) we first introduce a reduced Green’s function ′ g(x, x) defined by

′ G (x, x′) = -g(x,x-)-. (300 ) a(η)a(η′)
Substitution yields
( ∂2 2 ) − ----+ ∇2 + --- g(x, x′) = − 4πδ (η − η ′)δ3(x − x ′), (301 ) ∂η2 η2
where x = (x,y, z) is a vector in three-dimensional flat space, and ∇2 is the Laplacian operator in this space. We next expand ′ g(x,x ) in terms of plane-wave solutions to Laplace’s equation,
1 ∫ ′ g(x,x ′) = ------ &tidle;g(η,η ′;k )eik⋅(x −x) d3k, (302 ) (2π )3
and we substitute this back into Equation (301View Equation). The result, after also Fourier transforming δ3(x − x′), is an ordinary differential equation for ′ &tidle;g(η,η ;k),
( 2 ) -d--+ k2 − -2- &tidle;g = 4πδ (η − η ′), (303 ) dη2 η2
where k2 = k ⋅ k. To generate the retarded Green’s function we set
′ ′ ′ &tidle;g+(η,η ;k) = θ(η − η )ˆg(η,η ;k), (304 )
in which we indicate that ˆg depends only on the modulus of the vector k. To generate the advanced Green’s function we would set instead ′ ′ ′ &tidle;g− (η,η ;k ) = θ (η − η)ˆg (η, η;k ). The following manipulations will refer specifically to the retarded Green’s function; they are easily adapted to the case of the advanced Green’s function.

Substitution of Equation (304View Equation) into Equation (303View Equation) reveals that gˆ must satisfy the homogeneous equation

( 2 ) -d--+ k2 − -2- ˆg = 0, (305 ) dη2 η2
together with the boundary conditions
dˆg ˆg(η = η′;k) = 0, ---(η = η′;k) = 4π. (306 ) dη
Inserting Equation (304View Equation) into Equation (302View Equation) and integrating over the angular variables associated with the vector k yields
∫ ′ θ(Δ η) ∞ ′ g+ (x,x ) = 2π2R-- gˆ(η,η;k )k sin(kR )dk, (307 ) 0
where Δ η ≡ η − η′ and R ≡ |x − x′|.

Equation (305View Equation) has cos(k Δ η) − (kη )−1sin(kΔ η) and sin(kΔ η) + (kη)−1cos(k Δη ) as linearly independent solutions, and ˆg(η,η ′;k) must be given by a linear superposition. The coefficients can be functions of ′ η, and after imposing Equations (306View Equation) we find that the appropriate combination is

[( ) ] ˆg(η,η′;k) = 4π- 1 + --1--- sin (kΔ η) − Δ-η--cos(kΔ η) . (308 ) k k2ηη′ kηη′
Substituting this into Equation (307View Equation) and using the identity ∫ ∞ ′ ′ ′ (2∕π) 0 sin (ωx) sin(ωx ) dω = δ(x − x ) − δ(x + x ) yields
∫ ∞ g (x,x′) = δ(Δ-η-−-R-)+ θ(Δη-)2- 1-sin(kΔ η)cos(kR )dk + R ηη′ π 0 k

after integration by parts. The integral evaluates to θ(Δ η − R ).

We have arrived at

′ δ(η − η′ − |x − x ′|) θ(η − η′ − |x − x′|) g+(x,x ) = ------------′-------+ -----------′-------- (309 ) |x − x | η η
for our final expression for the retarded Green’s function. The advanced Green’s function is given instead by
′ ′ ′ ′ g (x,x′) = δ(η −-η-+-|x-−-x-|)-+ θ(−-η +-η-−-|x-−-x-|). (310 ) − |x − x ′| ηη′
The distributions ′ g±(x,x ) are solutions to the reduced Green’s equation of Equation (301View Equation). The actual Green’s functions are obtained by substituting Equations (309View Equation) and (310View Equation) into Equation (300View Equation). We note that the support of the retarded Green’s function is given by η − η′ ≥ |x − x ′|, while the support of the advanced Green’s function is given by η − η′ ≤ − |x − x′|.

It may be verified that the symmetric two-point function

h (x, x′) = -1- (311 ) ηη′
satisfies all of the Properties Sc.H1, Sc.H2, Sc.H3, and Sc.H4 listed in Section 4.3.5; it may thus be used to define singular and radiative Green’s functions. According to Equation (295View Equation) the singular Green’s function is given by
1 gS(x,x ′) = --------′ [δ(η − η′ − |x − x′|) + δ(η − η′ + |x − x ′|)] 2|x − x | -1--- ′ ′ ′ ′ + 2ηη′ [θ(η − η − |x − x |) − θ(η − η + |x − x |)], (312 )
and its support is limited to the interval ′ ′ ′ − |x − x | ≤ η − η ≤ |x − x |. According to Equation (287View Equation) the radiative Green’s function is given by
′ ----1---- ′ ′ ′ ′ gR(x,x ) = 2 |x − x ′| [δ (η − η − |x − x |) − δ(η − η + |x − x |)] + -1--[θ(η − η′ − |x − x ′|) + θ(η − η′ + |x − x ′|)]; (313 ) 2ηη′
its support is given by η − η′ ≥ − |x − x ′|, and for η − η ′ ≥ |x − x ′| the radiative Green’s function agrees with the retarded Green’s function.

As a final observation we note that for this cosmological spacetime, the normal convex neighbourhood of any point x consists of the whole spacetime manifold (which excludes the cosmological singularity at a = 0). The Hadamard construction of the Green’s functions is therefore valid globally, a fact that is immediately revealed by Equations (309View Equation) and (310View Equation).

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