1. Introduction and Summary
Gravitational waves (GWs) offer a unique window into the most energetic events in the cosmos, such as colliding black holes, neutron stars and interactions in the early universe. The recent rise in gravitational wave astronomy highlighted the need for better models of gravitational wave sources. Due to the large distances involved from the source, it is reasonable to make the approximation that the size of gravitational wave sources are significantly smaller than this distance. One may use an approximation where the source is considered point-like, but with additional structure contained in the moments. These moments can be represented as Schwartz distributional [
1] (e.g.,
–function) stress–energy tensors
, over the worldline of a chosen centre of the source. By imposing symmetry,
, and the divergence-free condition,
, one obtains ordinary differential equations (ODEs) for the moments. These ODEs are given in Equations (
7)–(
10) and (
20)–(
23), below. By solving these, one may predict the gravitational waves that the system will produce [
2,
3]. The distributional source approximation has several advantages. Solving a system of ODEs is much easier to solve than a system of partial differential equations (PDEs). In addition, there is an algebraic formula for the gravitational waves in terms of the components, given below in (
30). Another advantage is that, in principle, one can use this formula to directly measure the components of the multipole. This would require significant improvement in the sensitivity of gravitational wave detection, as one would need to measure the individual components of the gravitational wave perturbation tensor, and how they change when one changed the detectors’ position in space. In contrast, for a continuous stress–energy source, one can only measure the integrated contributions. These measured moments may provide physical insights into the source of the gravitational waves, especially when there is no model, or competing models for the dynamics of the source. This would then provide a direct comparison to the quadrupole, or higher multipole, model.
In the case of the monopole, the divergence-free condition implies that the point source undergoes geodesic motion, whereas for the dipole, this condition implies the Mathisson–Papapetrou–Tulczyjew–Dixon equations. The quadrupole is particularly interesting, as it is the quadrupole terms which give rise to gravitational waves. However, for the quadrupole, there are 60 moments (after imposing symmetries) but only 40 ODEs [
2,
3]. This implies that one requires additional ODEs or algebraic equations to determine the remaining 20 free components. We call additional equations
constitutive relations, because they will depend on the underlying material which we are approximating with the quadrupole. One would expect “dust” to have different constitutive relations from a neutron star, or two orbiting neutron stars. To date, there are no models at all for these constitutive relations, although in [
2], a suggestion is made. The freedom in the componets corresponds to the idea that a blob of matter can spread out and then recombine without breaking any conservation laws; see
Figure 1. The divergencelessness of the stress–energy tensor, Equation (
6), below, is not affected by certain internal dynamics of the multipole, as these internal dynamics are completely determined by the free components.
A similar situation, which requires constitutive relations, occurs when the worldline of the source is not specified. This is called the Pole–Dipole problem [
4,
5,
6,
7,
8,
9,
10,
11,
12]. In this case, the Mathisson–Papapetrou–Tulczyjew–Dixon equations, which are the only equations arising from the divergencelessness of the stress–energy tensor, are insufficient to determine both the dynamics of the worldline and the dynamics of the dipole moments. In this work, by contrast, we assume the worldline is specified, and hence the Mathisson–Papapetrou–Tulczyjew–Dixon equations completely specify the dynamics of the dipole.
Quadrupoles, and general multipoles, are abstract geometric objects, but it is useful to represent them using coordinates. There are two representations, the
Dixon representation [
13,
14,
15,
16,
17] and the
Ellis representation [
18], which are defined below. Both these representations consist of components defined only over a worldline, which is usually a path within, or close to, the extended body. The components correspond to the moments of the extended body. However, in order to calculate the moments, all the stress–energy tensors at the same “time” must be transported to the same point on the worldline, such that one can integrate them. This gives rise to two choices that one must make. The first is to decide which points in the extended object are at the same “time”. The other choice is how to transport the tensors. Dixon and Ellis make two different choices; this corresponds to how the multipoles are represented.
For the spatial timeslice, Dixon chose the orthogonal hypersurface. For a point on the worldline, take all the geodesics which emanate from this point and are orthogonal to the worldline. Then, use parallel transport to transport the tensors on this timeslice, along the geodesics, to the worldline to be integrated [
15]. These choices give rise to the Dixon representation. However, this representation is a little more general since one does not have to choose the tangent to the worldline to define the orthogonal hypersurface. Instead, one can use another arbitrary 4–vector along the worldline. This vector is called the
Dixon vector ; see
Figure 2. In this case, one chooses all the geodesics which are orthogonal to
. There are cases where using a Dixon vector which is not the 4–velocity of the worldline would be advantageous. One example is when there is a global timelike Killing vector, such as when considering matter near a black hole. Another is when considering ultra-relativistic particles expanded around a lightlike worldline, in which case the orthogonal hypersurfaces would not be transverse to the worldline.
There are many advantages to using the Dixon representation. One, the components are tensor fields along the worldline. Two, these components are unique, in that given a particular quadrupole, there is a formula for the corresponding components. This is distinct from the Ellis representation. Three, the quadrupole is written as a sum of the monopole, dipole and quadrupole terms and there is no freedom in this splitting. This monopole can be used to define the mass of the quadrupole, but in general, this mass is not conserved. The disadvantage is that there is a non-tensorial dependency of the components on the Dixon vector. Furthermore, this change of Dixon vector will mix the various orders so that the quadrupole will contribute to the dipole and visa-versa. In fact an explicit formula for that transformation of the components, arising from changing the Dixon vector, is not currently known.
For the Ellis representation, one simply chooses a coordinate system and then transports the vectors using Lie-transport with respect to this coordinate system. This results in taking the components of the tensors, with respect to this coordinate system, and simply integrating these values. Since no timeslice is chosen, the corresponding components are not unique (they possess a gauge-like freedom). Although the transformation of the components is given below, it is not tensorial. Indeed, for the quadrupole, it involves second derivatives and integrals of the coordinate transformations. In addition, there is no formula for the monopole and dipole terms of the quadrupole. From a mathematical point of view, an advantage is that this representation does not require an additional structure, such as the connection, on the manifold. Thus, it can be generalised to manifolds, such as phase spaces [
19], which do not possess a connection.
For the Ellis representation, the situation can be improved if one chooses a coordinate system which is adapted to the worldline. In this case, the timelike coordinate defines the timeslices and one uses Lie-transport with respect to spatial coordinates. In addition, the components are unique and one can separate out the monopole, dipole and quadrupole terms. However, this split is dependent on the coordinate system.
In both representations, the dipole can be written consistently with the Mathisson–Papapetrou–Tulczyjew–Dixon equations. Also, in both representations, one can formulate a regular tensor field whose moments, up to
k, are the components of the distribution. If all the moments are known, and satisfy Carleman’s conditions, then one can reconstitute the original distribution. As stated, both Ellis and Dixon are representations of an abstract geometric object, which can be formulated in a coordinate-free way, employing the de Rham pushforward [
2,
20].
2. Existing Literature on the Derivation of the Dynamics of the Quadrupole Moments
As stated in the introduction, the dynamics of the components of the dipole are given by the Mathisson–Papapetrou–Tulczyjew–Dixon equation. Thus, given the worldline and the initial values for the moments, they completely specify the moments. One may expect that the same would happen for the components of the quadrupole, and there have been several attempts, particularly by Dixon, to specify these ordinary differential equations for these moments. In his work, Dixon [
16,
17] makes two conjectures for the dynamics of the components of a quadrupole.
In [
15] (7.34)–(7.37), Dixon postulates simple rotational dynamics. Here, he introduces a connection [
15] (7.18),
defined by
where
is described as the body’s dynamical velocity,
and
. He writes
as
. Using this connection, we can formulate a rotation tensor
; [
15] (7.34) where,
From this, the dynamical equation for a non-rotating quadrupole
is given by [
15] (7.36)
As an alternative, Dixon also posits a non-dynamical equation based on symmetry [
16] (4.11).
We observe in
Section 6 below, that neither of these approaches correspond to the divergence-free condition (
6). Thus, they are not the generalisation of the Mathisson–Papapetrou–Tulczyjew–Dixon equations for the quadrupole.
In [
4], Steinhoff and Puetzfeld obtain the equations of motion of an extended test body in the framework of Einstein’s theory of gravitation. The equations of motion were derived via Tulczyjew’s multipolar approximation method, up to the quadrupole order. The canonical form of the energy-momentum density was explicitly constructed. The set of gravitational multipolar moments and the corresponding equations of motion were compared to alternative multipolar approximation schemes. They introduced the classification of two different types of equations, named “constraint” and “evolution”. The same type of pattern of equations replicates at each multipolar order. More than two equations of the evolution-type are not to be expected in the context of Tulczyjew’s approximation scheme. Moreover, in Tulczyjew’s method, which is used in [
4], the orthogonal decomposition of the moments is employed to facilitate the derivation of the canonical form. In particular, higher-order moments are recursively transferred to lower differential orders in the canonical form. For the quadrupole system, they take a similar approach to ours and we conjecture that our results (
7)–(
10) are equivalent to theirs. However, since they have used a different decomposition, it would require significant work to establish a direct comparison.
4. Distributional Quadrupole Sources of Gravitational Waves
Einstein’s equations
are non-linear. Recall that the distributional stress–energy tensor is an approximation to a regular stress–energy tensor, for which (
24) can be directly applied. In linear theories like electromagnetism, one often uses distributional sources. For example, an arbitrary moving point charge yields the Liénard–Wiechard fields. For a distributional matter, the stress–energy tensor can be written as (
4), (
13) or (
18). However, solutions of the Einstein Equation (
24) will diverge along the worldline
C, and the meaning of Equation (
24) requires interpretation. Indeed, according to Geroch [
21],
“There have been attempts to introduce into general relativity sources to represent gravitating point particles, i.e., sources concentrated on one-dimensional surfaces in space-time. One goal of this work was to find equations of motion for such point particles. To this end, there was introduced a class of metrics, specified by their behavior on approaching a singular worldline, to describe the near-field of such a particle. It now appears, however, that the metrics in this class may not be physically realistic, for one expects that such a concentration of matter would result in collapse through a horizon, and that inside this horizon there will be further structure. Indeed, it now seems likely that there is in general relativity no mathematical framework whatever for matter sources concentrated on one-dimensional surfaces in space-time.”
There have been several attempts to have a non-linear theory of distributions, the most successful being Colombeau, the algebra of generalised functions [
22]. An alternative approach is to consider a set of regular stress–energy tensors
, for which (
24) is valid. Dixon [
16] uses an exponential map, to connect points off the worldline to points on the worldline, to identify the distributional stress–energy
with the regular
tensor. Geroch and Weatherall [
23] consider an infinite set of regular stress–energy tensors fulfilling the dominant energy condition. They find a sequence which tends to the monopole stress–energy tensor. This is similar to use of squeezed tensors we consider in
Section 5, below.
Since we are primarily interested in sources of gravitational waves, we imply solve the linearlised Einstein’s equations. Expanding the gravitational metric,
is a pertubation about a background
,
where
is the small perturbation parameter and
is the perturbation term, and inserting the expansion into the Einstein Equation (
24), one has
Hence, the background metric
satisfies
. The linearised equations are then given by
In the case when the background metric
is the Minkowski metric
, then (
26) becomes [
24]
where
,
, and we have employed the Lorenz gauge, also called the de Donder gauge, (
). We can provide
in terms of an integral over the retarded Green’s functions:
Let us choose a one-parameter family of regular stress–energy tensors
, where
is the parameter. Let these tensors tend to the distributional tensor
in the limit
. An example of such a one-parameter family is provided in
Section 5. Then, the gravitational waves arising from
are the limit of the gravitational waves emanating from
, i.e.,
Let
be provided by the right-hand side of (
4); then, we have an explicit formula for
on a flat background (
28). Both the retarded Green’s function, and hence (
29) and the distribution
, are coordinate independent objects. Thus, the corresponding field
is a tensor. However, in order to express
in terms of components, it is necessary either to use the Dixon representation and choose
or use the Ellis representation and choose adapted coordinate systems. We will choose Cartesian coordinates and set
to be timelike and parallel. Thus, the components
are constant. In this case, we have an explicit expression given by
where
is the retarded time,
,
, and
.
Proof. Choose the Cartesian coordinates so that
. Thus, we have
. Let
be a vector field given by
and
, and let
. Then, from (
29), we have
which gives (
30) since
. □
6. Comparison of Dixon’s Equations for the Moments, with Those Presented Here
In order to compare Dixon’s equations for the moment with ours, it is necessary to relate the components. In [
17] (10.17), we see the term
when we expand the right-hand side. To understand this, we use, in turn [
17] (10.9), [
17] (10.6), [
16] (4.5), [
16] (7.4) to give
since from [
17] (10.17)
. Here, the moments
fulfil the symmetry conditions [
17] (10.3), and orthogonality condition [
17] (10.4). Thus, the first term in the last expression corresponds to the right-hand side of (
5) if we set
. However, the orthogonality condition does not completely correspond. Thus, we can identify
,
and
. Using [
17] (1.37) and [
14] (2.4), we can write
. Since this, by default, has the symmetries of the Riemann curvature tensor, it has 20 independent components. Most of these symmetries are necessitated because it is contracted with the Riemann curvature tensor [
17] (1.28) and (1.29). However, the 20 free components presented in this work do not correspond to 20 independent components of the quadrupole moment
.
The main dissimilarity is the necessity of the divergenceless condition. In [
17], this is realised by putting the divergence operator into the argument of
I, as observed in the term
in [
17] (10.16). As stated by comment (vii) in [
17] (p. 109), this does not yield any additional algebraic or differential equations for the
. It solely impacts the dynamics of the dipole [
17] (1.28) and (1.29). Contrarily, in our approach, we obtain the ODEs and free components of the
or
, by applying the divergence operator directly to the distribution. Therefore, a non-rotating quadrupole would not fulfill (
7)–(
10) and therefore does not correspond to a divergenceless stress–energy tensor.
Dixon’s alternative approach, [
16] Equation (4.11), becomes, in our language
This resembles the constraint (
10), but without the projections. Thus, it will not satisfy the divergenceless condition. Intriguingly, (
43) also yields 20 free components.