A Classical Proof of the Classical Soft Graviton Theorem in D>4
Alok Laddha, Ashoke Sen

TL;DR
This paper provides a direct classical proof of the soft graviton theorem in higher-dimensional gravity theories, linking low-frequency gravitational radiation to scattering trajectories without relying on quantum limits.
Contribution
It offers a novel, direct classical derivation of the soft graviton theorem in D>4, extending understanding beyond quantum or subleading order proofs.
Findings
Validated the classical soft graviton theorem in higher dimensions.
Connected gravitational radiation spectra to particle trajectories and spins.
Extended the theorem's applicability to generic gravity-matter systems.
Abstract
Classical soft graviton theorem gives an expression for the spectrum of low frequency gravitational radiation, emitted during a classical scattering process, in terms of the trajectories and spin angular momenta of ingoing and outgoing objects, including hard radiation. This has been proved to subleading order in the expansion in powers of frequency by taking the classical limit of the quantum soft graviton theorem. In this paper we give a direct proof of this result by analyzing the classical equations of motion of a generic theory of gravity coupled to interacting matter in space-time dimensions larger than four.
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A Classical Proof of the Classical Soft Graviton Theorem in D4
Alok Laddhaa and Ashoke Senb
* aChennai Mathematical Institute, Siruseri, Chennai, India*
* bHarish-Chandra Research Institute, HBNI*
Chhatnag Road, Jhusi, Allahabad 211019, India
E-mail: [email protected], [email protected]
Abstract
Classical soft graviton theorem gives an expression for the spectrum of low frequency gravitational radiation, emitted during a classical scattering process, in terms of the trajectories and spin angular momenta of ingoing and outgoing objects, including hard radiation. This has been proved to subleading order in the expansion in powers of frequency by taking the classical limit of the quantum soft graviton theorem. In this paper we give a direct proof of this result by analyzing the classical equations of motion of a generic theory of gravity coupled to interacting matter in space-time dimensions larger than four.
Contents
1 Introduction
Classical soft graviton theorem[1] describes the spectrum of low frequency gravitational radiation emitted during a classical scattering process, including decay in which a single bound system explodes into a set of outgoing objects. Up to subleading order in the expansion in powers of the soft graviton frequency, the result depends solely on the trajectories and the spin angular momenta of incoming and outgoing objects (which may also include radiation), without requiring any detailed knowledge of how the objects travelled during the scattering process or what kind of forces acted between the objects during the scattering. In space-time dimensions larger than four, this was proved in [1] by taking the classical limit of the quantum multiple soft graviton theorem[2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15]. Our goal in this paper will be to show that classical soft graviton theorem can be derived directly using the equations of motion of general relativity coupled to matter. Our results will be valid in any general coordinate invariant theory of gravity coupled to interacting matter, possibly including higher derivative terms in the action.
The strategy we follow will be to take all but the linearized terms in the Einstein’s equation to the right hand side and regard the right hand side as the total energy momentum tensor of the system. This includes the energy momentum tensor of the gravitational field as defined in [16]. We can then ‘solve’ the equations by taking the convolution of the flat space retarded Green’s function with the energy momentum tensor. The domain of integration is then divided into two parts: a large but finite spatial volume around the region where the scattering takes place, and the region outside this volume. In the outer region we approximate the energy momentum tensor by that of free particles corresponding to the asymptotic incoming and outgoing particles and radiation. In the inner region the energy momentum tensor, including the non-linear terms in the Einstein’s equation, are complicated, but we determine the low frequency gravitational radiation from this region simply by using local conservation laws. As we show below, the sum of the two contributions is independent of the precise division of the space-time regions we choose, and is given solely by the asymptotic trajectories and spin angular momenta of the incoming and the outgoing particles.
We now summarize our main results. In the following we shall refer to the incoming and outgoing objects involved in the scattering as particles, even though we do not assume that they are structureless objects – even black holes, stars and bound binary systems will be counted as particles. This is justified by the fact that while describing the coupling of a gravitational field of wavelength much larger then the characteristic size of the objects, we can approximate the stress tensor for any finite size gravitating object by the stress tensor of a point particle with (generically) infinitely many multipole moments. We denote the asymptotic trajectory of the -th particle by
[TABLE]
where and are constant -dimensional vectors and is an appropriately normalized affine parameter. We also denote by the momentum of the -th particle, and by the spin angular momentum carried by the -th particle, both counted with + sign if ingoing and sign if outgoing. Operationally, , , and can be defined through the energy momentum tensor carried by the particle as given in (2.11). If denotes metric fluctuation, then we define111Even though we express the metric as , we do not assume that is small, except in the asymptotic region.
[TABLE]
[TABLE]
[TABLE]
We show that for large , the small expansion of is given by (up to gauge transformations):
[TABLE]
where
[TABLE]
denotes the total angular momentum carried by the -th particle, with the first two terms giving the orbital contribution and the last term giving the spin contribution. In (1.5) we have set . Here, and in the rest of the paper, all indices are raised and lowered by the Minkowski metric and all scalar products are also defined using the Minkowski metric. As indicated in the last line of (1.5), the order of the error is larger of and . An important feature of (1.5) is that the result does not depend on any details of the actual scattering process or the nature of the interactions involved during the scattering. The leading term in (1.5), associated with the first term inside the square bracket, agrees with the results obtained in [17, 18].
If a significant amount of momentum and / or angular momentum is carried away by the outgoing scalar, electromagnetic and / or gravitational radiation, then the sum over in (1.5) also includes the contribution due to radiation. An explicit form of this contribution may be written as:
[TABLE]
where denotes angular integration, and
[TABLE]
is the contribution to the symmetric energy-momentum tensor due to massless fields. Note that there is no ambiguity regarding the definition of for the gravitational field – it is what we get by taking the non-linear terms in the Einstein’s equation to the right hand side[16]. Explicit form of for massless scalar, vector and gravitational field to the required order has been given in appendix B. Physically and represent respectively the total flux of outgoing momentum and angular momentum[19] of radiation along the direction . The overall minus sign in (1.7) reflects that in (1.5) the momenta and angular momenta are counted as positive if ingoing, whereas and represent outgoing flux.
With (1.7) present on the right hand side of (1.5), both sides of the equation contain the gravitational field . However one can easily check that the contribution to (1.7) from of frequency of order or less is suppressed by higher powers of and therefore does not produce any order terms. Therefore (1.5) with (1.7) included can be regarded as an equation that determines the low frequency component of the gravitational radiation in terms of its finite frequency component and other asymptotic data. Our result is similar in spirit to the memory effect in four dimensions (see [20] for a review) where the memory term is determined in terms of finite frequency gravitational radiation and other asymptotic data.
With some work, this approach to deriving classical soft theorem may be extended to one higher order in expansion in the soft frequency , by including the next order terms in the expansion (2.11) of the energy momentum tensor of matter in the far region. However the corresponding coefficients of expansion will not be universal, – they will depend on the detailed properties of the incoming and the outgoing objects. Based on the quantum results of [9], we expect the corrections to at the next order to be of the form:
[TABLE]
where is some tensor that depends on the properties of the -th external state, but does not depend on the details of the scattering process.222Results of [21, 22] in four dimensions suggest that the coefficient vanishes if the -th external state represents a rotating black hole. is anii-symmetric under and also under , and symmetric under . This approach will break down at the next order due to the ambiguity described in (2.28) in determining the contribution to from the near region. This is in agreement with the corresponding results in quantum soft graviton theorem described in [9].
A generalization of (1.5), including the contribution from massless particles, exists in four space-time dimensions as well[23, 24], but due to the existence of long range electromagnetic and gravitational forces, the actual formula takes a different form (see eq.(2.2) and (2.6) of [24] for the general formula). In particular the subleading terms now have contribution proportional to . As in the case of , the four dimensional formula has been obtained by taking the classical limit of quantum soft graviton theorem. This has also been verified in explicit examples where independent computation of soft gravitational radiation during classical scattering has been performed[25, 26, 27]. We expect that a direct classical derivation of this formula should be possible along the lines discussed in the paper, but the analysis will have to be more complicated due to the reasons described below eq.(2.16).
The rest of the paper is organized as follows. In §2 we prove the classical soft theorem (1.5), assuming that the contribution due to the radiation can be treated as a flux of massless particles. In §3 we derive the radiation contribution (1.7) explicitly by analyzing the soft radiation sourced by the energy momentum tensor of massless fields. The two appendices provide some technical results on the asymptotic growth of massless fields that is used in computing the contribution to due to radiation.
2 Classical soft theorem
We consider the situation in which a set of objects enter a given region in space, interact among themselves, and then disperse. Our goal will be to compute the spectrum of low frequency gravitational waves emitted during this process. Decomposing the metric as , we express the Einstein’s equation as
[TABLE]
where we have set . contains contribution from the matter energy momentum tensor as well as all the non-linear terms in the Einstein’s equation. Bianchi identity ensures that satisfies the conservation law (see e.g. [16]):
[TABLE]
Choosing de Donder gauge,
[TABLE]
and defining through the equation
[TABLE]
a ‘solution’ to (2.1) may be written as
[TABLE]
where denotes the flat space retarded Green’s function
[TABLE]
We should note however that (2.5) should be regarded as an identity involving instead of a solution, since the right hand side of the equation also involves through .
If we define
[TABLE]
then using (2.5), (2.6) we get
[TABLE]
We now decompose into its component along and transverse to . For large , we can evaluate the integration over by closing the integration contour in the upper half plane and picking up the residue from the pole at . After this the integration over can be done using saddle point method, with the saddle point occurring at . The result takes the simple form[1]:
[TABLE]
where
[TABLE]
and the boundary terms at infinity have to be adjusted to make this integral well-defined. denotes equality up to terms containing higher powers of .
Let us now suppose that we have a classical scattering process in which the interaction takes place mainly around the origin of the spatial coordinates . We shall evaluate (2.9) by dividing the domain of integration over the spatial coordinates into two parts: and , and call the corresponding contributions and respectively. Here is a large but finite number so that the interaction takes place mainly in the region . We do not need to assume anything about the kind of interactions that take place in this region, except that they must be consistent with the conservation laws. Outside this region we only need to take into account the effect of long range gravitational and electromagnetic fields, and even these can be treated perturbatively. We shall assume that all initial and final particles move with finite non-zero velocity so that in the far past and far future the region is nearly empty. This can always be achieved by choosing an appropriate Lorentz frame. However, since our final formula will be written in a Lorentz covariant form, it will also be valid in the frame where some of the initial or final state particles are at rest.
In the region , we do not make any assumption about except its conservation laws. We shall see that this is sufficient to extract the relevant contribution to the integral from this region. On the other hand in the interval , will be taken to be the energy momentum tensor of free particles whose quantum numbers are the same as those of the incoming and the outgoing particles. We do not however assume that the particles are structureless: the effect of the internal structure of the particle is encoded in the fact that the energy momentum tensor of the particles is allowed to have derivatives of delta functions localized on the trajectory besides the leading term proportional to the delta function[28, 29, 30, 31, 32, 33, 21, 22]. In this case the Fourier transform of the energy momentum tensor will have an expansion in powers of , with the expansion coefficients encoding the internal structure of the particle. As long as we consider wavelengths large compared to the sizes of the particles, this expansion will be valid even for big objects like neutron stars, black holes or binary systems. For our analysis we shall only need the first two coefficients in the expansion, which are determined in terms of the momentum and spin of the particle. The precise expression will be given shortly.
We begin our analysis in the region. In this region we have, to first order in the expansion in derivatives of delta function,333For the trajectory , the right hand side of (2.11) can be shown to be invariant under the transformation , , for any constant vector . Therefore neither nor are unambiguously defined. We can fix this ambiguity by imposing some conditions on , e.g. . In any case, defined in (1.6) is unambiguous. (see e.g. [34]):
[TABLE]
where the sum over runs over all the incoming and outgoing particles, denotes the trajectory of the ’th particle with labelling an appropriately normalized affine parameter along the trajectory up to a sign, and are respectively the -momentum and the spin angular momentum of the ’th particle, both counted with positive sign for ingoing particles and negative sign for outgoing particles, and . Since in our notation the ingoing momenta are positive, we take to increase from at the outer end to [math] on the surface . In this notation for some positive constant and the trajectory begins at some cut-off point at the outer end and ends at a point on the surface . This has been illustrated in Fig. 1. Therefore by definition . denotes symmetrization, with the convention:
[TABLE]
In the sum over in (2.11), we include the effect of outgoing radiation (gravitational or electromagnetic) by regarding them as a flux of massless particles.444This will be justified in detail in §3. Therefore the sum over includes an angular integration over outgoing finite frequency radiation. In the special case where the total energy carried away by radiation is small compared to the energies of the massive objects involved in the scattering, the contribution due to radiation in the sum in (2.11) can be ignored.
There are of course higher order terms in the expansion (2.11) containing more derivatives of , but they will not contribute to the soft theorem to subleading order. This can be seen as follows. First we see that when we substitute (2.11) into (2.9), the integral in the first term gets localized at , but the integration produces a linearly divergent term from the large region in the limit. This divergence is regulated by the term in (2.9), producing an inverse power of . This gives the leading term. Since the second term in (2.11) contains a derivative of , we can first integrate by parts, bringing down a factor of and then repeat the previous argument. As a result this term is of order unity and begins contributing at the subleading order. Terms involving higher derivatives of will bring down more powers of . Therefore they will not contribute at the subleading order.
Using (2.11), the contribution is given by:
[TABLE]
where we define,
[TABLE]
The term in the penultimate line of (2.13) is a boundary term at that arises from having to integrate by parts the term involving in (2.11). This can be seen as follows. First we represent the boundary term as
[TABLE]
We now carry out the integration over using the factor. This replaces by . We then carry out the integration using this delta function, which has support at since . This generates a factor of , with the minus sign reflecting the fact that is counted as positive if ingoing.
There are similar terms from the outer boundary where takes value , but these terms are absorbed into the boundary terms at in the last line of (2.13). Using the trajectory equation , we can carry out the integration over in (2.13). If we now use the relation for some positive constant , we can express (2.13) as:
[TABLE]
In arriving at this expression we have cancelled all terms proportional to by appropriate choice of the boundary terms at .
Let us estimate the error we made in the above calculation by taking to be the energy momentum tensor produced by free particles. Since we are computing the result to subleading order , we shall estimate the error to this order. First error stems from the fact that the particles are not free, but are under the influence of each other’s long range gravitational (and possibly electromagnetic) fields. These forces fall off as when the distance between the particles is of order – with all distances being measured with respect to the flat metric. Integrating this once we see that the correction to (and hence also ) fall off as . Therefore the integral of the error over part of the trajectory from to will fall off as . Since in the integration region for evaluating , the net error in the computation of is bounded by . For , this error vanishes in the large limit.
There may also be contributions to from stored in the long range fields (gravitational and electromagnetic). We shall show in §3 that this contribution can be included in the sum over in (2.16) by regarding the radiative field contribution as a sum over the flux of massless particles. In the final expression, the additional contribution to due to radiation will be given by (1.7).
We now turn to the contribution to (2.9) from the region. We have:
[TABLE]
This gives:
[TABLE]
Using integration by parts and the conservation law (2.2), this can be expressed as
[TABLE]
We can evaluate the right hand side by noting that on the boundaries the energy momentum tensor may be approximated by those of the free particles entering and leaving the region . We now use (2.11) to express (LABEL:econd1.1) as,
[TABLE]
We manipulate this expression using the following steps.
Replace by . 2. 2.
Integrate the term by parts. This acts on and brings down a factor of . It also acts on the and gives . 3. 3.
Once the factor has been removed from , we can use this delta function to perform the integration. This sets in all the expressions, including in the term and in the term. 4. 4.
We now use the fact that the solution to relations is to write
[TABLE]
The minus sign reflects the fact that is counted as positive if ingoing. 5. 5.
We can now perform the integration over using these delta functions. In particular the term will generate a derivative of , producing a term proportional to . 6. 6.
We now replace all factors of by with being a positive constant.
The net outcome of these manipulations is the relation:
[TABLE]
Expanding the factor in powers of and using the momentum conservation law
[TABLE]
we can express (2.22) as
[TABLE]
Since in the definition (2.17) of the integration over is confined to a finite region (which also effectively makes the integration over bounded since by assumption the region becomes empty for large ), is an analytic function of near and should admit a Taylor series expansion in . We propose the following solution for :
[TABLE]
It satisfies (2.24) up to terms of order . We also need to check that this is symmetric under exchange of and . For this we note that angular momentum conservation implies:
[TABLE]
Adding (2.26) multiplied by to (2.25), we get:
[TABLE]
which is manifestly symmetric under .
We can also argue that the solution (2.25) is unique. To see this we assume the contrary, that there is another solution. Then the difference between the two solutions will be analytic function of near and will satisfy the constraint . It is easy to check that there is no function that satisfies this requirement, is analytic at and does not vanish at . The first term in the power series expansion in that satisfies this constraint is proportional to
[TABLE]
Adding (2.16) and (2.27), and expanding in powers of , we get
[TABLE]
where
[TABLE]
This is the classical soft graviton theorem to subleading order. We emphasis that the sum over in (2.29) includes integration over the flux of gravitational (and electromagnetic if any) radiation, with representing the flux of angular momentum carried by the radiation. Explicit expression for these contributions has been given in (1.7). In §3 we shall derive (1.7) by directly working with massless fields instead of regarding them as flux of massless particles.
We conclude this section by exploring the possibility of extending the analysis to higher orders in the frequency of the soft graviton:
In order to extend our computation of to higher order in , we need to keep terms in the expression (2.11) involving higher number of derivatives of the delta function. However the coefficients of these terms are not expected to be universal. Instead they will depend on the internal structures of the objects involved in the scattering. Nevertheless, these contributions will still be independent of the details of the scattering process, being sensitive only to the properties of the incoming and the outgoing objects. For Kerr black holes in four dimensions, some of the coefficients of higher derivatives of the delta function have been computed in [21, 22]. 2. 2.
Presence of the term (2.28) in the expression for begin affecting the soft radiation at the sub-sub-subleading order. These contributions are expected to depend on the details of the scattering process and not just on the properties of the incoming and the outgoing objects. Therefore our approach cannot unambiguously determine the low frequency gravitational radiation in terms of the properties of the incoming and outgoing objects beyond the sub-subleading order and further details of the theory are required to determine the metric.
We have described in (1.9) the expected correction to at the subsubleading order in the expansion in powers of . We hasten to add however that this expectation is based on the quantum soft graviton theorem derived in [9], and we have not derived (1.9) from a classical analysis.
3 Soft radiation from fields
Our goal in this section will be to compute soft radiation sourced by fields. We shall use (2.9) for this computation, by dividing the integration region into the and parts as in §2. We shall divide the analysis into two parts. In the first part we shall derive the analog of (2.11) for radiation. In the second part we shall use this result to compute soft radiation from the radiative stress tensor.
3.1 General form of the stress tensor of radiation
We begin by introducing some notations. Let us first define:
[TABLE]
where in (3.1), and are to be regarded as contravariant vectors. We shall denote by the derivative . We also define the transverse derivative as follows. If denotes an infinitesimal vector orthogonal to , so that is still a unit vector to first order, then we define for any function via the relation:
[TABLE]
It is easy to verify the following identities,
[TABLE]
where
[TABLE]
is the projection operator into the space transverse to and . This gives, for any function :
[TABLE]
We shall now derive the analog of (2.11) – the asymptotic form of the stress tensor associated with massless fields, including gravitational and electromagnetic field. As in §2, the stress tensor of the gravitational field will be defined to be whatever appears on the right hand side of the Einstein’s equation if the left hand side contains only the linear terms. We claim that the relevant part of the stress tensor produced by radiation has the following expansion to order :
[TABLE]
where is a vector with only transverse components:
[TABLE]
Furthermore, we show below that for large , and fall off at least as fast as and respectively.
The justification for (3.6) can be given as follows. We begin with the leading term555This result is well known (see e.g. [35]), but we include the argument for completeness. . Any component of a massless field, irrespective of its spin, has a leading behaviour of the form for large . Furthermore, as reviewed in appendix A, falls off at large [36, 17, 18]. Using (3.5) we now see that the leading term in is given by . Since the relevant term in the stress tensor in the asymptotic region comes from the square of the first derivative of the field, we see that in order to get a term of the form in the stress tensor we must take the term and appropriately contract the indices. Since cannot contract with itself or the transverse indices, by taking the leading order term in the fields to carry only transverse polarization – which is possible for – we can ensure that and remain uncontracted and only the transverse indices are contracted with each other. This shows that the term in must be proportional to , i.e. it takes the form given in the first term in (3.6). Using (3.3), (3.5) one can show that this term satisfies the energy momentum conservation law by itself.
We now turn to the subleading terms in (3.6). We begin by writing down the most general expression for the order term in :
[TABLE]
where , and are scalars, , are transverse vectors and is a transverse symmetric tensor, all the quantities being functions of and . We now demand and use (3.3). We get, at order :
[TABLE]
Since for fixed the stress tensor must vanish for , this gives:
[TABLE]
Vanishing of the term proportional to in give
[TABLE]
The right hand sides of these equations could actually have terms proportional to -derivatives of higher order coefficients of expansion, but since such terms can be absorbed into a redefinition of in (3.6), we ignore them. This brings the result almost to the desired form (3.6) with the identification , except that we need to show that the transverse tensor has the form of the term proportional to in (3.6). This can be seen as follows:
Since we have chosen the polarization tensors of the fields to be transverse (and also traceless for the radiative part of the metric), neither the nor the derivative can contract with an index of the polarization tensor. One way to get rid of the free index from is to pick the other derivative to be and contract with – we see from (3.5) that this is possible since . This leaves behind the indices from the polarization tensors, which could supply the indices of the transverse tensor (and, for the gravitational field, the left-over transverse indices can contract with each other). Since and , such contributions to will have the structure with the polarizations appropriately contracted. It is easy to see that these terms are total derivatives in and therefore can be absorbed into the term proportional to in (3.6). For example for gauge fields we shall have and for the gravitational field we have . 2. 2.
For the gravitational field we need to also consider a possible contribution to proportional to , where are transverse directions and the two indices coming from are contracted with the two indices of . Even if by a choice of gauge we take the order term in to have only transverse components, could have a term of order . Therefore, could give a contribution to of order . However, as shown in eq.(LABEL:eb36) in appendix B, equations of motion forces the leading term in to be of order . Therefore we cannot get a contribution of order to with transverse from the term.
This establishes (3.6).
In appendix B we shall verify (3.6) explicitly for massless scalar, vector and tensor fields, where we also express (3.6) in Bondi coordinates. From this analysis it will also be clear that and contain two powers of , with having two derivative acting on these factors and having one derivative acting on one of the factors. On the other hand, it follows from the analysis of [36, 17, 18] – rederived in appendix A – that falls off at least as fast as for large . Therefore falls off at least as fast as and falls off at least as fast as for large .
Before concluding this section we shall discuss a subtle point. In odd dimensions, the expansion of a massless field in inverse powers of also contains integer powers of the form . In five dimensions this could upset the expansion (3.6), by producing a term of order from the product of the leading term in of order and the subleading term of order . This is larger than the subleading term of order given in (3.6). It was shown however in [37] that the order term in the expansion of is -independent, and therefore when we try to construct the stress tensor from the field, we must necessarily act either a radial derivative or a transverse derivative on this component.666Since in our set up the sources of the gravitational field travel with finite velocity at late time, we expect the Coulomb part to be not independent, but it should fall off for since the sources move away to a distance further than for . Nevertheless the important point is that the derivative is of the same order as derivative and therefore does not produce any contribution to of order . This produces an extra power of , making the contribution to the stress tensor of order . This is smaller than the subleading term in (3.6) which falls off as .
3.2 Computation of
We shall now substitute (3.6) into (2.9) to compute . As usual we divide the integration range into two parts, and , to compute the contributions to and . We begin with the contribution to , given by
[TABLE]
First we note that the contribution from the last term in (3.6) proportional to may be analyzed by integration by parts. There are no boundary terms since for fixed , integration over runs from to and the integrand falls off at the two ends. Acting on the factor at fixed , , the term brings down a factor proportional to . The integrand multiplying it falls off as for large , and the factor renders the integral finite, with at most a divergence for small . Since terms are subsubleading in the soft expansion, we can ignore this term in our computation.
Similarly one can show that higher order terms in the expansion of , beyond those given in (3.6), do not contribute to (3.12) to subleading order. For this let us consider a term in of order for any positive number . We substitute this into (3.12) and evaluate it in the limit. First let us assume that the integrand falls off sufficiently fast for large so that the integral gives a finite result. Then the integration over the spatial coordinates is proportional to . This goes as and is therefore suppressed in the large limit. Exceptions to this are terms coming from products of Coulomb components of the fields, which remain independent[37] over a time scale of order . After this period the sources producing the Coulomb field will move away to a distance farther than and the field will begin to decrease. Therefore for the contribution to the stress tensor from the product of these terms, the integration can give terms of order . However since the Coulomb component appears at order and its derivatives are of order , its contribution to the stress tensor will be of order . Therefore even if the integral produces a factor of , the spatial integral will be of the form . For , this is suppressed for large .
Therefore we need to evaluate (3.12) with given by (3.6), ignoring the term proportional to . For this we first make a change of variables:
[TABLE]
This induces the transformations:
[TABLE]
where we have ignored terms that are suppressed by two powers of . Using this in (3.12) we get
[TABLE]
In particular the order terms in (3.6) get cancelled (except for the term, which we have argued does not contribute to to subleading order). We now express as , and then integrate by parts over , arriving at
[TABLE]
where denotes integration over the angular variables and we have used:
[TABLE]
The first term on the right hand side of (3.16) represents the boundary contribution from . As usual, we have ignored boundary terms at infinity. The term in the second line has integrand of order , and even when we expand the exponential factor to order to pick the subleading term, the integrand will be of order . Therefore the integral goes as and can be ignored. This gives, to subleading order in the expansion in powers of ,
[TABLE]
We now turn to the computation of
[TABLE]
The calculation will follow the same steps as the ones described below (2.17). We have
[TABLE]
where in the second step we have carried out an integration by parts, picking up the boundary term at and using the conservation law777Actually it is the sum of the stress tensor of the radiation and matter that is conserved. So we really need to combine (3.20) with (2.18) and set to zero the total contribution to . Similarly neither (2.23) nor (3.21) is true individually, but their sum is true, and one should analyze the contribution to from matter and radiation together. A similar remark holds for the angular momentum conservation laws (2.26) and (3.24). . Since the total ingoing momentum flux is equal to the total outgoing momentum flux, we have
[TABLE]
Using this we can express (3.20) as
[TABLE]
We can take the solution to (3.22) to be
[TABLE]
This does not look symmetric under , but using the conservation of total angular momentum (see footnote 7):
[TABLE]
we can rewrite (3.23) as a manifestly symmetric tensor:
[TABLE]
Adding (3.18) and (3.25), and dropping terms containing inverse powers of , we now get, up to subleading order in the expansion in powers of ,
[TABLE]
We now use the expression for given in (3.6) to evaluate this expression, ignoring terms containing inverse powers of . Using the result at , and after an integration by parts in the angular variables for the term proportional to , we get the result:
[TABLE]
where
[TABLE]
It is straightforward to verify that if we substitute the expression for given in (3.6) into (LABEL:eabexpint), and substitute the resulting expressions for , into (1.7), we get back the same expression for as given in (3.27).888In the computation we have not included the contribution from the term proportional to in (3.6). This gives a contribution to proportional to . Being a total derivative in. (and hence ), its contribution to the soft theorem via (LABEL:eabexpint) vanishes.
This establishes (1.7), (LABEL:eabexpint).
From the analysis in the penultimate paragraph of §3.1 we know that falls off as and fall off as for large . Using these results in (3.27), (3.28) we see that the integrand in (3.27) falls off at least as fast as for large . Therefore its integral over yields finite result for . This observation is particularly relevant for odd since the retarded Green’s function has support for lying inside the future light-cone of , instead of on the future light-cone of .
Acknowledgement: We would like to thank Miguel Campiglia, Arnab Priya Saha and Biswajit Sahoo for useful discussions. The work of A.S. was supported in part by the J. C. Bose fellowship of the Department of Science and Technology, India and the Infosys chair professorship.
Appendix A Radiative fields at large retarded time
In this appendix we shall study the asymptotic fall-off of massless fields in the scattering process at large retarded time. We shall assume that we have chosen a gauge such that the field equation of a massless field takes the form:
[TABLE]
for some source term . In this case the solution is given by:
[TABLE]
where is the retarded Green’s function. It was shown in [1] (and reviewed in §2) that for large , (A.2) takes the form:
[TABLE]
with,
[TABLE]
Now we know from the analysis of §2 that for small :
[TABLE]
for some function . Since small behaviour of controls the large time behaviour of , we get, from (A.2)-(A.4),
[TABLE]
In even dimensions the integral gives or its derivatives[36, 17], and therefore the expression is localized around . In odd dimensions, changing integration variable from to , we get:
[TABLE]
This shows that for , falls off as for large . This agrees with the results of [18] and is one of the results used in our analysis in §3 for computing the contribution to due to stress tensor of massless fields.
Appendix B Stress tensor of radiation at large distance
In this appendix we shall verify the general form (3.6) of the stress tensor associated with massless fields by explicitly constructing the stress tensor of massless scalar, vector and tensor fields. The asymptotic form of various massless fields that we shall use for this computation can be found in [38, 37], but we also review their derivation. To simplify notation, we shall drop the subscript from and drop the primes from the coordinate labels used in (3.6).
We shall work with Bondi coordinates defined as
[TABLE]
For a given vector , we get, using (3.3)
[TABLE]
so that we have
[TABLE]
In this coordinate system, the expected form of given in (3.6) takes the form:
[TABLE]
up to terms that are either of order and total derivative in or of order . is related to in (3.6) via the relation,
[TABLE]
The metric in this coordinate system is given by
[TABLE]
where is the metric on the unit sphere. The inverse metric has the form:
[TABLE]
The non-vanishing Christoffel symbols of the Minkowski metric in Bondi coordinate system are:
[TABLE]
where is the Christoffel symbol on the unit sphere labelled by the coordinates . We shall denote by the covariant derivative on the unit sphere computed with the metric and the Christoffel symbol , and by the combination .
Our goal will be to verify (LABEL:etform) for massless fields. Let us first consider the case of a massless scalar field with stress tensor:
[TABLE]
In the Bondi coordinates the Laplace equation takes the form:
[TABLE]
The asymptotic form of the scalar field produced during a classical scattering process has the form:999In standard notation in general relativity, e.g. in [37], and would be denoted as and respectively. We shall avoid using this notation for brevity, but the translation is straightforward. The same translation can be made for the other fields introduced below, e.g. and will stand for and respectively, and and will stand for and respectively.
[TABLE]
Here is some function that falls off for large according to the results of appendix A, and will be determined shortly. In (B.11) we have ignored a possible Coulomb term of order in , since we have argued in §3 that these terms do not contribute to to the required order. Substituting (B.11) into (B.10) we find that the order term automatically vanishes and the order term gives:
[TABLE]
This gives, to order ,
[TABLE]
and therefore
[TABLE]
Since this is a total derivative in , we can ignore its contribution to given in (B.9). From (LABEL:ephder), (B.9) we now get:
[TABLE]
up to terms that are either of order or of order and total derivative in . This matches (LABEL:etform) up to terms of the form if we choose:
[TABLE]
Next we shall analyze the stress tensor corresponding to the asymptotic electromagnetic field. We shall use Lorentz gauge. In the Bondi coordinates, the equations of motion take the form[38, 37]:
[TABLE]
We now express the radiative part of the gauge field in the far region as
[TABLE]
where the function falls off for large . As described in §3, there are also Coulombic modes[37], but their contribution to the stress tensor can be ignored at this order. The Lorentz gauge condition gives . Since falls off at large , we get . We can use the residual gauge freedom with to also set . In the coordinate system this gives, from (B.3),
[TABLE]
up to corrections of order . Substituting (B.19) into (LABEL:elaplaceA) we get equations analogous to (B.12):
[TABLE]
The first equation, together with the fact that vanishes in the far past, allows us to set to 0.
In the coordinate system, different components of the field strength up to order are given by:
[TABLE]
From this we can calculate the energy momentum tensor:
[TABLE]
ignoring corrections of order and total derivatives in in terms of order . We first note that to this order
[TABLE]
Since this is a total derivative we can ignore its contribution to . Therefore we get, ignoring terms of order and total -derivative terms of order :
[TABLE]
This has the same form as (LABEL:etform) if we identify:
[TABLE]
It is easy to check that the last two equations are consistent with each other for suitable choice of .
Finally we shall analyze the stress tensor associated with asymptotic gravitational field. We shall use the de Donder gauge:
[TABLE]
so that the linearized equations of motion take the form . We expand the radiative part of in the far region as
[TABLE]
ignoring the Coulombic modes as usual. The gauge condition (B.26) gives, at leading order,
[TABLE]
In this gauge we still have residual gauge symmetry
[TABLE]
which induces a transformation
[TABLE]
for any function . By adjusting we can set
[TABLE]
In Bondi coordinates this corresponds to the following expansion of the various components of up to order :
[TABLE]
We can now write down the equations in the Bondi coordinate system, and substitute (LABEL:ehhexp) into these equations to determine ’s in terms of ’s as in the case of scalar fields and gauge fields. Explicit form of these equations can be found in [38, 37]. For the sake of brevity we shall not describe the full set of equations for , but give one example. The component of the equations of motion takes the form:
[TABLE]
Upon substituting (LABEL:ehhexp) into this equation we find that the order terms in the equation gives
[TABLE]
where in the last step we have used the last equation of (LABEL:ehhexp). Vanishing of is an important ingredient that was used in §3 to show that at order , the transverse component of the gravitational stress tensor is a total derivative in – we shall also see this explicitly in (LABEL:etmetric). Similar analysis with the other components of the equation leads to the following set of equations for the ’s in the Bondi coordinates:
[TABLE]
We can now use this to compute the energy-momentum tensor of gravitational radiation. In the asymptotic region we only need to take the terms quadratic in . This is given by[16]:101010Even if the action contains higher derivative terms, their contribution to the stress tensor in the asymptotic region will be suppressed. Therefore we do not include these terms.
[TABLE]
where and represent contributions to the Ricci tensor linear and quadratic in respectively:
[TABLE]
[TABLE]
In the Bondi coordinates, will have the same form, except that the derivatives will have to be replaced by – covariant derivatives computed with the metric (B.6) and connection (B.8), and will have to be replaced by the form of the metric given in (B.6). The calculation is straightforward, yielding the result:
[TABLE]
with all the other components vanishing to this order. This has the form given in (LABEL:etform) with:
[TABLE]
In particular the last two equations are compatible for suitable choice of . The expression for given in (LABEL:etmetric) also agrees with the result of [39] in .
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