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Coordinates are messy
— not only in General Relativity

Carla Cederbaum
Mathematics Department
Eberhard Karls Universität Tübingen

Melanie Graf
Mathematics Department
Eberhard Karls Universität Tübingen/
now Universität Hamburg
[email protected]@uni-hamburg.de
Abstract

The coordinate freedom of General Relativity makes it challenging to find mathematically rigorous and physically sound definitions for physical quantities such as the center of mass of an isolated gravitating system. We will argue that a similar phenomenon occurs in Newtonian Gravity once one ahistorically drops the restriction that one should only work in Cartesian coordinates when studying Newtonian Gravity. This will also shed light on the nature of the challenge of defining the center of mass in General Relativity. Relatedly, we will give explicit examples of asymptotically Euclidean relativistic initial data sets which do not satisfy the Regge–Teitelboim parity conditions often used to achieve a satisfactory definition of center of mass. These originate in our joint work [4] with Jan Metzger. This will require appealing to Bartnik’s asymptotic harmonic coordinates.

1 Preferred Systems of Coordinates (or not)

As we all know, Euclidean space — the stage of Newtonian Gravity — knows preferred systems of coordinates, called Cartesian coordinates. In such coordinates, the Euclidean metric δ\delta takes its canonical form. Similarly, the Minkowski spacetime — the setting of Special Relativity — carries preferred systems of coordinates in which the Minkowski metric η\eta takes its canonical form. In contrast, curved spacetimes — the mathematical framework of General Relativity — and initial data sets therein are well-known not to admit any ’canonical’ or ’preferred’ coordinates in general. This freedom in the choice of coordinates makes it challenging to find mathematically rigorous and physically sound definitions for physical quantities such as the center of mass of an isolated gravitating system in General Relativity as is well-known and will be discussed in this article. We will argue that a similar phenomenon occurs in Newtonian Gravity once one ahistorically and somewhat unnecessarily drops the restriction that one should only work in Cartesian coordinates when studying Newtonian Gravity. This will also shed light on the nature of the challenge of defining the center of mass in General Relativity. Relatedly, we will give explicit examples of asymptotically Euclidean relativistic initial data sets which do not satisfy the “Regge–Teitelboim (parity) conditions” often used to achieve a satisfactory definition of center of mass. These originate in our joint work [4] with Jan Metzger.

2 Isolated Systems at a Given Instant of Time

Let’s begin by recalling the standard definitions of an “isolated system at a given instant of time” in both Newtonian Gravity and General Relativity. We will also recall the standard definitions of (total) mass of such systems along the way and discuss the convergence of the involved integrals.

2.1 Isolated Systems at a Given Instant of Time in Newtonian Gravity

In Newtonian Gravity, we can think of an “isolated system at a given instant of time” as given by a matter density function ρ:3[0,)\rho\colon\mathbb{R}^{3}\to[0,\infty) which has compact support or at least decays suitably fast towards infinity. For example, one could ask that ρ=O(r3ε)\rho=O(r^{-3-\varepsilon}) as rr\to\infty for some (small) ε>0\varepsilon>0, that is, ρ\rho decays to zero at least as fast as r3+εr^{-3+\varepsilon}, where rr denotes the radial coordinate on 3\mathbb{R}^{3}. Alternatively but not equivalently, one could ask that ρL1(3)\rho\in L^{1}(\mathbb{R}^{3}). Both assumptions are independent of the chosen Cartesian coordinates because any two systems of Cartesian coordinates on 3\mathbb{R}^{3} differ only by a rigid motion. Either of these decay assumptions is sufficient for the total mass

m=3ρ(x)𝑑x\displaystyle m=\iiint_{\mathbb{R}^{3}}\rho(\vec{x})\,d\vec{x} (2.1)

to be well-defined and finite. Anticipating the discussion below, let us point out that the OO-assumption suggests computing the integral in (2.1) as an improper Riemann integral in polar coordinates, while the L1L^{1}-assumption suggests treating it as a Lebesgue integral. Of course, the resulting mass mm will be the same whatever notion of integral one refers to, as long as it converges. However, taking the former viewpoint, we can take advantage of cancellations in the spherical integrals. Also note that the decay assumptions are of course not independent of arbitrary coordinate changes.

2.2 Isolated Systems at a Given Instant of Time in General Relativity

In General Relativity, an “isolated system at a given instant of time” is modelled as an asymptotically Euclidean (or asymptotically flat) relativistic initial data set (or time-slice): As usual, an initial data set (M,g,K)(M,g,K) consists of a 33-dimensional Riemannian manifold (M,g)(M,g) carrying a symmetric (0,2)(0,2)-tensor field KK playing the role of second fundamental form (or extrinsic curvature) of the initial data set in the spacetime modelling the system.

In addition, a relativistic initial data set carries an energy density μ:M\mu\colon M\to\mathbb{R} and a momentum density one-form JJ related to gg and KK via the well-known Einstein constraint equations

R|K|2+(trK)2\displaystyle\operatorname{R}-|K|^{2}+(\operatorname{tr}K)^{2} =2μ\displaystyle=2\mu (2.2)
div(K(trK)g)\displaystyle\operatorname{div}(K-(\operatorname{tr}K)g) =J.\displaystyle=-J. (2.3)

and derived from the energy-momentum tensor TT of the spacetime. Here, R\operatorname{R} denotes the scalar curvature of (M,g)(M,g), and |||\cdot|, tr\operatorname{tr}, and div\operatorname{div} denote the tensor norm, trace, and divergence with respect to gg, respectively. We will adopt the following standard definition, see also Figure 1.

Def 2.1 (Asymptotically Euclidean Relativistic Initial Data Set).

A relativistic initial data set (M,g,K)(M,g,K) with energy density μ\mu and momentum density JJ is called asymptotically Euclidean if there exists a compact set CMC\subset M, a radius R>0R>0, and an asymptotic coordinate chart x:MC3BR(0)\vec{x}\colon M\setminus C\to\mathbb{R}^{3}\setminus B_{R}(0) such that

gijδij\displaystyle g_{ij}-\delta_{ij} =O2(r12ε)\displaystyle=O_{2}(r^{-\frac{1}{2}-\varepsilon}) (2.4)
Kij\displaystyle K_{ij} =O1(r32ε)\displaystyle=O_{1}(r^{-\frac{3}{2}-\varepsilon}) (2.5)
μ,Ji\displaystyle\mu,J_{i} =O0(r3ε)\displaystyle=O_{0}(r^{-3-\varepsilon}) (2.6)

as r=|x|r=|\vec{x}\,|\to\infty for some decay parameter ε>0\varepsilon>0, where gijg_{ij}, KijK_{ij}, and JiJ_{i} denote the components of gg, KK, and JJ in the coordinates x\vec{x}, respectively. Alternatively but not equivalently, one can replace Assumption (2.6) by asking that μ,JiL1(3BR(0))\mu,J_{i}\in L^{1}(\mathbb{R}^{3}\setminus B_{R}(0)).

Here, the index k0{}k\in\mathbb{N}_{0}\cup\{\infty\} in Ok(rα)O_{k}(r^{\alpha}) for some α<0\alpha<0 is a shorthand for asking that derivatives of order up to kk decay ’accordingly’ as rr\to\infty, that is, first derivatives decay to zero at least as fast as rα1r^{\alpha-1}, second derivatives decay to zero at least as fast as rα2r^{\alpha-2}, etc. In what follows, we will slightly abuse notation and extend this to the ’decay rate’ α=0\alpha=0, so that f=Ok(r0)f=O_{k}(r^{0}) will mean that the function ff stays bounded as rr\to\infty, while its order ll derivatives decay to zero at least as fast as rlr^{-l} as rr\to\infty whenever lkl\leq k.

The (total) mass mADMm_{\text{ADM}} of an asymptotically Euclidean relativistic initial data set (M,g,K)(M,g,K) was defined by Arnowitt, Deser, and Misner in [1] via the (total) energy EADME_{\text{ADM}} and (total) linear momentum PADM\vec{P}_{\text{ADM}} and has become the standard definition, satisfying many desirable properties such as for example positivity ([12, 13]):

EADM\displaystyle E_{\text{ADM}} :=116πlimRSR(0)i,j=13(igijjgii)xjRdAδ,\displaystyle\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\frac{1}{16\pi}\lim_{R\to\infty}\iint_{S_{R}(0)}\sum_{i,j=1}^{3}(\partial_{i}g_{ij}-\partial_{j}g_{ii})\frac{x^{j}}{R}dA_{\delta}, (2.7)
PADMj\displaystyle P_{\text{ADM}}^{j} :=18πlimRSR(0)i=13((trK)gijKij)xiRdAδ,\displaystyle\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\frac{1}{8\pi}\lim_{R\to\infty}\iint_{S_{R}(0)}\sum_{i=1}^{3}\left((\operatorname{tr}K)g_{ij}-K_{ij}\right)\frac{x^{i}}{R}dA_{\delta}, (2.8)
mADM\displaystyle m_{\text{ADM}} :=EADM2|PADM|2,\displaystyle\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\sqrt{E_{\text{ADM}}^{2}-\left|\vec{P}_{\text{ADM}}\right|^{2}}, (2.9)

where dAδdA_{\delta} denotes the Euclidean area measure on SR(0)S_{R}(0). In [2], Bartnik uses harmonic asymptotically Euclidean coordinate charts to prove that EADME_{\text{ADM}} is well-defined and independent of the choice of asymptotically Euclidean coordinate charts, see Section 3. Note that Bartnik uses the weaker L1L^{1}-decay condition on μ\mu. From this, (2.8), (2.5) and (2.6), it follows directly that mADMm_{\text{ADM}} is also well-defined and independent of the choice of asymptotically Euclidean coordinate chart via the Divergence Theorem. Again, this argument only uses the weaker L1L^{1}-condition on JJ.

Refer to caption
Figure 1: An asymptotically Euclidean relativistic initial data set (M,g,K)(M,g,K) and the image of its asymptotic end MCM\setminus C in 3\mathbb{R}^{3} under the asymptotic coordinate chart x\vec{x}.

You may wonder why one asks for such general decay rates in (2.4)–(2.6), and not just for, say,

gijδij=O2(r1)\displaystyle g_{ij}-\delta_{ij}=O_{2}(r^{-1}) (2.10)

etc.. This has two reasons: First, the theory of asymptotically Euclidean relativistic initial data sets does not become more complicated if one does so. Second, it actually becomes richer, i.e., allows for more examples, see [4] and the references cited therein.

Next, let us discuss how a single relativistic initial data set can carry different asymptotic coordinate charts and discuss the relationship between different such charts.

3 Comparing Different Asymptotic Coordinate Systems

Clearly, if a relativistic initial data set is asymptotically Euclidean for some asymptotic coordinate chart x\vec{x}, it will also be asymptotically Euclidean for any asymptotic coordinate chart y\vec{y} arising from x\vec{x} by a rigid motion111The careful reader may note that one may need to change the compact set CC and the radius RR from 2.1 for the coordinate chart y\vec{y}; we will ignore such subtleties in this article for the sake of readability., for the same decay parameter ε\varepsilon. Moreover, the class of possible transformations between two asymptotic coordinate charts x\vec{x} and y\vec{y} with respect to which a given relativistic initial data set (M,g,K)(M,g,K) is asymptotically Euclidean is much richer than just rigid motions, even when fixing the decay parameter ε\varepsilon. Here is an example: Let (M,g,K)(M,g,K) be a relativistic initial data set with energy and momentum densities μ\mu and JJ which is asymptotically Euclidean with respect to some asymptotic coordinate chart x\vec{x} and for some decay parameter ε>0\varepsilon>0. Then (M,g,K)(M,g,K) will also be asymptotically Euclidean with decay parameter ε\varepsilon with respect to the asymptotic coordinate chart

y:=x+sin(lnr)a\displaystyle\vec{y}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\vec{x}+\sin(\ln r)\,\vec{a} (3.1)

for some non-vanishing a3\vec{a}\in\mathbb{R}^{3}, with r=|x|r=|\vec{x}| as before. This can be seen by a straightforward computation. In particular, note that Equation 3.1 is very similar to a mere translation, differing only in the bounded factor sin(lnr)=O(r0)\sin(\ln r)=O_{\infty}(r^{0}) as rr\to\infty.

On the other hand, it crucially depends on the choice of asymptotic coordinate chart whether a given relativistic initial data set “is” asymptotically Euclidean: For example, any relativistic initial data set which is asymptotically Euclidean with respect to an asymptotic coordinate chart x\vec{x} will not be asymptotically Euclidean with respect to the chart y:=2x\vec{y}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}2\vec{x} as one easily computes. We will hence refer to an asymptotic coordinate chart x\vec{x} as an asymptotically Euclidean coordinate chart for a given relativistic initial data set (M,g,K)(M,g,K) (with energy and momentum densities μ\mu and JJ) if (M,g,K)(M,g,K) is asymptotically Euclidean with respect to x\vec{x}.

Summarizing, the class of asymptotically Euclidean coordinate charts for a given relativistic initial data set is much richer than the class of Cartesian coordinate systems on Euclidean space. This applies in particular to the Euclidean relativistic initial data set (M=3,g=δ,K=0)(M=\mathbb{R}^{3},g=\delta,K=0) sitting inside the Minkowski spacetime. Here, one sees that the Cartesian coordinate systems are asymptotically Euclidean coordinate charts, but by far not the only asymptotically Euclidean coordinate charts.

3.1 Divergence of Mass

At this point, it is instructive to recall that the decay condition (2.4) cannot be relaxed as was shown by a counter-example by Denissov and Solovyev [7]: Inspired by their example, let us consider the Euclidean relativistic initial data set (M=3,g=δ,K=0)(M=\mathbb{R}^{3},g=\delta,K=0) in the coordinates

y:=(1+ar)x\displaystyle\vec{y}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\left(1+\frac{a}{\sqrt{r}}\right)\,\vec{x} (3.2)

for some non-zero aa\in\mathbb{R} which leads to (2.4) with ε=0\varepsilon=0 and the unphysical result mADM=a28m_{\text{ADM}}=\frac{a^{2}}{8}. One can argue similarly for (2.5) as we will discuss elsewhere; alternatively, one can compute in a lengthy but straightforward way that the decay conditions (2.4) and (2.5) transform equivariantly under coordinate boosts in the ambient spacetime. From this and the example by Denissov and Solovyev, one can conclude that (2.5) is necessary for physicality of the definition of mADMm_{\text{ADM}}.

In summary, (convergence and coordinate independence of) mass is very well understood in both Newtonian Gravity and General Relativity and depends crucially on the decay of the matter variables, as well as, in General Relativity, on the asymptotics of the relativistic initial data set itself.

One of the main tools introduced by Bartnik for the study of mass and energy are the “harmonic asymptotically Euclidean coordinates” we will now explain.

4 A Canonical Choice: Harmonic Coordinates

Cartesian coordinates are not only canonical for the Euclidean metric, they are also harmonic, that is, they satisfy the system of partial differential equations

δx=0,\displaystyle\triangle_{\delta}\vec{x}=0, (4.1)

a shorthand for the system of equations

δxi=0 for i=1,2,3,\displaystyle\triangle_{\delta}x^{i}=0\text{ for }i=1,2,3, (4.2)

where δ\triangle_{\delta} denotes the Euclidean Laplacian.

Exploiting this insight, Bartnik showed in [2] that asymptotically Euclidean relativistic initial data sets (M,g,K)(M,g,K) always possess harmonic asymptotically Euclidean coordinate charts, that is, asymptotically Euclidean coordinate charts satisfying the geometric system of partial differential equations

x=0,\displaystyle\triangle\vec{x}=0, (4.3)

where \triangle denotes the Laplacian with respect to gg. Here, “geometric” means that the partial differential equations themselves do not depend on a choice of (local or asymptotic) coordinate chart.

Furthermore, Bartnik showed [2, Theorem 3.1] that two such harmonic asymptotically Euclidean coordinate charts x\vec{x}, y\vec{y} are related by a rigid motion up to suitably lower order terms,

y=Qx+a+O0(r12ε),\displaystyle\vec{y}=Q\vec{x}+\vec{a}+O_{0}(r^{\frac{1}{2}-\varepsilon}), (4.4)

for a special orthogonal matrix Q3×3Q\in\mathbb{R}^{3\times 3} and a vector a3\vec{a}\in\mathbb{R}^{3}. In particular, there are more harmonic asymptotically Euclidean coordinate charts on Euclidean space than just the Cartesian coordinate systems: for example, the coordinates y:=x+br\vec{y}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\vec{x}+\frac{\vec{b}}{r} for some non-trivial vector b3\vec{b}\in\mathbb{R}^{3} are also harmonic.

5 On the Center of Mass of Isolated Systems at a Given Instant of Time

Let us now move on to the definition of (total) center of mass, where the situation is somewhat drastically different than for energy, linear momentum, and mass. Again, we will first take a look at the (total) center of mass of an isolated system at a given instant of time in Newtonian Gravity.

5.1 On the Center of Mass in Newtonian Gravity

Provided m0m\neq 0, the center of mass in Newtonian Gravity is naturally defined as the averaged weighted integral of the position vector x\vec{x},

C:=1m3ρ(x)x𝑑x.\displaystyle\vec{C}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\frac{1}{m}\iiint_{\mathbb{R}^{3}}\rho(\vec{x})\,\vec{x}\,d\vec{x}. (5.1)

Looking at (5.1) as a Lebesgue integral, it suggests itself that one should ask that ρrL1(3)\rho r\in L^{1}(\mathbb{R}^{3}). Instead, for this to be well-defined and finite as an improper Riemann integral,

C=limR0RSr(0)ρ(x)x𝑑Aδ𝑑r,\displaystyle\vec{C}=\lim_{R\to\infty}\int_{0}^{R}\iint_{S_{r}(0)}\rho(\vec{x})\,\vec{x}\,dA_{\delta}\,dr, (5.2)

it suggests itself to assume ρ=O0(r4ε)\rho=O_{0}(r^{-4-\varepsilon}) for some ε>0\varepsilon>0, in analogy with the choice of decay rate used for ensuring that the mass is well-defined; this of course settles the convergence issue for Newtonian gravitating systems.

However, let us — ahistorically — take a different approach in analogy with the standard approach taken to resolve the corresponding issue in General Relativity. To this end, let us instead make a further parity-based decay assumption, namely

ρodd=O0(r4ε),\displaystyle\rho^{\mathrm{odd}}=O_{0}(r^{-4-\varepsilon}), (5.3)

where

ρodd(x):=12(ρ(x)ρ(x))\displaystyle\rho^{\mathrm{odd}}(\vec{x})\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\frac{1}{2}(\rho(\vec{x})-\rho(-\vec{x})) (5.4)

is the odd part of ρ\rho. This approach relies on the insight that the contribution to (5.2) of the even part

ρeven:=ρρodd\displaystyle\rho^{\mathrm{even}}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\rho-\rho^{\mathrm{odd}} (5.5)

vanishes by parity on each sphere Sr(0)S_{r}(0).

In view of the analogous approach taken in General Relativity, let us take the time to consider the parity condition

ρodd=O0(r4ε)\displaystyle\rho^{\mathrm{odd}}=O_{0}(r^{-4-\varepsilon}) (5.6)

and its properties in more detail. Importantly, we would like to bring to the reader’s attention that the parity condition is not independent of the choice of Cartesian coordinate systems because the reflection xx\vec{x}\mapsto-\vec{x} involved in the definition of ρodd\rho^{\mathrm{odd}} does not interact well with translations. However, the desirable invariance under choice of Cartesian coordinate systems can be restored if one assumes that in some, and hence all, Cartesian coordinate systems, one has ρ=O1(r3ε)\rho=O_{1}(r^{-3-\varepsilon}), by appealing to the Mean Value Theorem.

5.1.1 Transformation Behavior of the Center of Mass in Newtonian Gravity

Of course, when well-defined by asking that ρL1(3)\rho\in L^{1}(\mathbb{R}^{3}) or ρ=O0(r4ε)\rho=O_{0}(r^{-4-\varepsilon}) for some ε>0\varepsilon>0, the center of mass C\vec{C} transforms as expected under changes of Cartesian coordinate systems, which can suggestively be written as

Cy=QCx+a.\displaystyle\vec{C}_{\vec{y}}=Q\vec{C}_{\vec{x}}+\vec{a}. (5.7)

But what happens if one — ahistorically — allows asymptotically Euclidean coordinate charts on the Euclidean stage of Newtonian Gravity? It will be instructive to study this in an explicit example similar to (3.1), i.e., y:=x+sin(lnr)a\vec{y}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\vec{x}+\sin(\ln r)\,\vec{a}, but modified to obtain a global coordinate chart z\vec{z} on 3\mathbb{R}^{3},

z:=x+σ(r)sin(lnr)a,\displaystyle\vec{z}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=}\vec{x}+\sigma(r)\sin(\ln r)\,\vec{a}, (5.8)

where σ:[0,)\sigma\colon[0,\infty)\to\mathbb{R} is a strictly increasing cut-off function satisfying σ(r)=0\sigma(r)=0 for r<2r<2 and σ(r)=1\sigma(r)=1 for r>3r>3. Computing the center of mass Cz\vec{C}_{\vec{z}} according to (5.1) with respect to the asymptotically Euclidean coordinate chart z\vec{z}, for a point particle matter density ρ(x)=mδ(x)\rho(\vec{x})=m\delta(\vec{x}), one finds Cx=0\vec{C}_{\vec{x}}=\vec{0} but Cz\vec{C}_{\vec{z}} diverges like sin(lns)a\sin(\ln s)\vec{a} for s=|z|s=|\vec{z}|\to\infty.

This can be made mathematically more precise by using a surface integral approach via the Divergence Theorem and the Poisson equation for the Newtonian potential as elaborated by Cederbaum and Nerz [5].

Briefly put, once one ahistorically allows more general asymptotically Euclidean coordinate charts in Newtonian Gravity, the center of mass is not generically a well-defined quantity even if ρ=O0(r4ε)\rho=O_{0}(r^{-4-\varepsilon}) as rr\to\infty. From the perspective of Newtonian Gravity arising as the Newtonian limit of General Relativity for slow speeds and small masses, it thus becomes reasonable to expect a similar phenomenon to occur in General Relativity. We will now turn to this.

5.2 On the Center of Mass in General Relativity

In General Relativity, a (total) notion of center of mass CBÓRT\vec{C}_{\text{B\'{O}RT}} of an isolated system at a given instant of time was put forward by Beig and Ó Murchadha in [3], based on previous work by Regge and Teitelboim [11] and similar in spirit and derivation to the ADM-quantities. For an asymptotically Euclidean relativistic initial data set (M,g,K)(M,g,K) with EADM0E_{\text{ADM}}\neq 0, its components are formally defined by

CBOM:=\displaystyle C_{\text{BOM}}^{\ell}\mathrel{\raise 0.40903pt\hbox{\rm:}\mkern-5.2mu=} 116πEADMlimR{SR(0)xi,j=13(igijjgii)xjRdAδSR(0)i=13(gixiRgiixR)dAδ}\displaystyle\frac{1}{16\pi E_{ADM}}\lim_{R\to\infty}\left\{\iint_{S_{R}(0)}x^{\ell}\sum_{i,j=1}^{3}(\partial_{i}g_{ij}-\partial_{j}g_{ii})\frac{x^{j}}{R}\right.dA_{\delta}-\left.\iint_{S_{R}(0)}\sum_{i=1}^{3}\big{(}g_{i\ell}\frac{x^{i}}{R}-g_{ii}\frac{x^{\ell}}{R}\big{)}dA_{\delta}\right\} (5.9)

with respect to the given asymptotically Euclidean coordinate chart x\vec{x}. Just as in the Newtonian case, this is a formal definition in the sense that it need not and does not always converge.

One instance where it diverges222For further examples of divergence of the center of mass, see [5] and the references cited therein. is the canonical Schwarzschild relativistic initial data set (3B2m(0)¯,112mrdr2+r2dΩ2,K=0)(\mathbb{R}^{3}\setminus\overline{B_{2m}(0)},\frac{1}{1-\frac{2m}{r}}dr^{2}+r^{2}d\Omega^{2},K=0) of mass m0m\neq 0, when considered with respect to the asymptotic coordinate chart y\vec{y} arising from the Cartesian coordinates x\vec{x} computed from the spherical polar Schwarzschild coordinates via (3.1). As in the Newtonian Gravity case discussed above, one finds via a lengthy computation that (CBÓRT)y\left(\vec{C}_{\text{B\'{O}RT}}\right)_{\vec{y}} diverges like sin(lns)a\sin(\ln s)\vec{a} for s=|y|s=|\vec{y}|\to\infty, while of course (CBÓRT)x\left(\vec{C}_{\text{B\'{O}RT}}\right)_{\vec{x}}=0 and EADM=mE_{\text{ADM}}=m. We would like to draw the reader’s attention to the fact that this initial data set has μ=0\mu=0, J=0J=0, so the divergence problem clearly does not arise from poor decay of the matter.

A first idea one might have to remedy the divergence problem of CBÓRT\vec{C}_{\text{B\'{O}RT}} could be to assume the stronger decay condition gijδij=O1(r2ε)g_{ij}-\delta_{ij}=O_{1}(r^{-2-\varepsilon}), thereby enforcing convergence in a way similar to remedying the convergence issue of EADME_{\text{ADM}} discovered by Denissov and Solovyev, see Section 3.1. However, this implies EADM=0E_{\text{ADM}}=0 which is undesirable when interested in the center of mass.

Instead, one usually resorts to parity assumptions. Before we do so in Section 5.2.2, let us briefly take a look at the transformation behavior of the center of mass under changes of asymptotic coordinates.

5.2.1 Transformation Behavior of the Center of Mass in General Relativity

As in the Newtonian case discussed in Section 5.1.1, when CBÓRT\vec{C}_{\text{B\'{O}RT}} is well-defined (see below), the center of mass CBÓRT\vec{C}_{\text{B\'{O}RT}} transforms as expected under “asymptotic Euclidean motions”, i.e., under changes of asymptotic coordinate systems that can be written as

y=Qx+a\displaystyle\vec{y}=Q\vec{x}+\vec{a} (5.10)

with QQ and a\vec{a} as before. That is to say that (5.7) holds also in the relativistic case.

5.2.2 Introducing the Regge–Teitelboim Parity Conditions

As hinted to in the Newtonian Gravity discussion above, the standard way out of the divergence dilemma is to assume parity conditions as suggested by Regge and Teitelboim in [11].

Def 5.1 (Regge–Teitelboim Conditions).

An initial data set (M,g,K)(M,g,K) with an asymptotically Euclidean coordinate chart x\vec{x} is said to satisfy the weak (strong) Regge–Teitelboim conditions if there exists ε>0\varepsilon>0 such that, for η=12\eta=\frac{1}{2} (η=1\eta=1) and

gijodd\displaystyle g_{ij}^{\mathrm{odd}} =O2(r12ηε)\displaystyle=O_{2}(r^{-\frac{1}{2}-\eta-\varepsilon}) (5.11)
Kijeven\displaystyle K_{ij}^{\mathrm{even}} =O1(r32ηε)\displaystyle=O_{1}(r^{-\frac{3}{2}-\eta-\varepsilon}) (5.12)
μodd,Jiodd\displaystyle\mu^{\mathrm{odd}},J_{i}^{\mathrm{odd}} =O0(r3ηε)\displaystyle=O_{0}(r^{-3-\eta-\varepsilon}) (5.13)

as r=|x|r=|\vec{x}|\to\infty, where the even and odd parts are taken with respect to x\vec{x}.

It was shown by Beig and Ó Murchadha in [3] that the strong Regge–Teitelboim conditions indeed suffice to ensure convergence of CBÓRT\vec{C}_{\text{B\'{O}RT}}. Consistently, the above Schwarzschild example does not satisfy any Regge–Teitelboim conditions in the asymptotically Euclidean coordinate chart y\vec{y} introduced in (3.1), as can be seen by a tedious computation for which we refer the interested reader to [4].

It is well-known (see [5] and the references cited therein) that the weak Regge–Teitelboim conditions do not suffice to ensure convergence of CBÓRT\vec{C}_{\text{B\'{O}RT}}; yet, as we will see at the end of this article, they are very relevant for analyzing CBÓRT\vec{C}_{\text{B\'{O}RT}}.

Moreover, as in the Newtonian Gravity case, neither the strong nor the weak Regge–Teitelboim conditions are invariant under changes between different asymptotically Euclidean coordinate charts because of the same conflict between reflections and translations. But they suffer from even more fundamental issues.

6 (In-)Existence of Coordinate Systems Satisfying the Regge–Teitelboim Conditions

We have just seen that the class of coordinate systems satisfying the Regge–Teitelboim conditions is not closed under translations. But, more fundamentally, do all asymptotically Euclidean relativistic initial data sets even possess any asymptotically Euclidean coordinate charts in which the (strong) Regge–Teitelboim conditions hold? As we have investigated with Jan Metzger in [4], this turns out not to be the case; indeed, we will soon give explicit counter-examples.

In order to prove inexistence of such asymptotically Euclidean coordinate charts on a given relativistic initial data set, we utilize Bartnik’s harmonic asymptotically Euclidean coordinate charts, see Section 4, and methods from [2, 9] as well as a bootstrapping argument to show the following result. We refer the interested reader to our joint work with Jan Metzger [4] for more details and the proofs of the following theorems.

Theorem 6.1.

Let (M,g,K)(M,g,K) be an asymptotically Euclidean relativistic initial data set and assume it satisfies the weak (strong) Regge–Teitelboim conditions with respect to an asymptotically Euclidean coordinate chart x\vec{x}. Then there exists a smooth harmonic asymptotically Euclidean coordinate chart y\vec{y} such that xy=O3(|x|12ε¯)\vec{x}-\vec{y}=O_{3}(|\vec{x}|^{\frac{1}{2}-\overline{\varepsilon}}) as |x||\vec{x}|\to\infty and

g¯ijodd\displaystyle\overline{g}_{ij}^{\,\mathrm{odd}} =O1(|y|12ηε¯)\displaystyle=O_{1}(|\vec{y}|^{-\frac{1}{2}-\eta-\overline{\varepsilon}}) (6.1)
K¯ijeven\displaystyle\overline{K}_{ij}^{\,\mathrm{even}} =O0(|y|32ηε¯)\displaystyle=O_{0}(|\vec{y}|^{-\frac{3}{2}-\eta-\overline{\varepsilon}}) (6.2)

as |y||\vec{y}|\to\infty for some ε¯>0\overline{\varepsilon}>0, where η=12\eta=\frac{1}{2} (respectively η=1\eta=1), and where the components g¯ij\overline{g}_{ij} and K¯ij\overline{K}_{ij} of gg and KK as well as their odd and even parts are computed with respect to y\vec{y}.

In other words, the Regge–Teitelboim conditions are inherited by harmonic asymptotically Euclidean coordinate charts up to a potential loss of derivatives. As a corollary of this analysis, the reduced derivative weak (respectively strong) Regge–Teitelboim conditions (6.1), (6.2) are satisfied for one set of harmonic asymptotically Euclidean coordinate charts if and only if they are satisfied for all such charts.

We also get the following “converses”, which readily follow from a more careful analysis of decay rates.

Theorem 6.2.

Let (M,g,K)(M,g,K) be an asymptotically Euclidean relativistic initial data set with respect to an asymptotically Euclidean coordinate chart x\vec{x}, but assume that

KijevenO0(|x|2ε)\displaystyle K_{ij}^{\mathrm{even}}\neq O_{0}(|\vec{x}|^{-2-\varepsilon}) (6.3)

as |x||\vec{x}|\to\infty for some decay parameter ε>0\varepsilon>0.

Then the harmonic coordinate chart constructed in 6.1 is asymptotically Euclidean but cannot satisfy the weak Regge–Teitelboim conditions. More precisely, we get

K¯ijevenO0(|y|2ε)\displaystyle\overline{K}_{ij}^{\,\mathrm{even}}\neq O_{0}(|\vec{y}|^{-2-\varepsilon}) (6.4)

as |y||\vec{y}|\to\infty. If, in addition, gg satisfies additional decay assumptions such as for example

gijodd=O2(|x|3/2ε),\displaystyle g^{\mathrm{odd}}_{ij}=O_{2}(|\vec{x}|^{-\nicefrac{{3}}{{2}}-\varepsilon}), (6.5)

while

KijevenO0(|x|52ε)\displaystyle K_{ij}^{\mathrm{even}}\neq O_{0}(|\vec{x}|^{-\frac{5}{2}-\varepsilon}) (6.6)

as |x||\vec{x}|\to\infty then the harmonic coordinate chart constructed in 6.1 is asymptotically Euclidean but cannot satisfy the strong Regge–Teitelboim conditions. More precisely, we get

K¯ijevenO0(|y|52ε)\displaystyle\overline{K}_{ij}^{\,\mathrm{even}}\neq O_{0}(|\vec{y}|^{-\frac{5}{2}-\varepsilon}) (6.7)

as |y||\vec{y}|\to\infty.

In a nutshell, we have seen that ruling out the existence of asymptotically Euclidean coordinate charts in which a given relativistic initial data set satisfies the strong or the weak Regge–Teitelboim conditions can be reduced to asking (almost) the same question only about harmonic asymptotically Euclidean coordinate charts.

This allows us to give a number of explicit examples of relativistic initial data sets not allowing for any asymptotically Euclidean coordinate charts satisfying the strong (respectively weak) Regge–Teitelboim conditions.

6.1 Graphical Counter-Examples to Existence of Regge–Teitelboim Coordinates

All examples discussed in this section originate from our joint work with Jan Metzger [4]. Following ideas by Cederbaum and Nerz [5], we focus on relativistic initial data sets in the Schwarzschild spacetime of mass mm\in\mathbb{R} in the Cartesian coordinates x\vec{x} associated with the Schwarzschild coordinates. These can and will be described as graphs over the canonical relativistic initial data set {t=0}\{t=0\} of suitable graph functions T:3CT\colon\mathbb{R}^{3}\setminus C\to\mathbb{R} for a suitable compact set C3C\subset\mathbb{R}^{3}. Writing the Schwarzschild spacetime as

N(r)\displaystyle N(r) =12mr,\displaystyle=\sqrt{1-\frac{2m}{r}}, (6.8)
h\displaystyle h =1N2dr2+r2dΩ2,\displaystyle=\frac{1}{N^{2}}dr^{2}+r^{2}d\Omega^{2}, (6.9)

on ×(rm,)×𝕊2\mathbb{R}\times(r_{m},\infty)\times\mathbb{S}^{2} with dΩ2d\Omega^{2} denoting the canonical metric on the sphere 𝕊2\mathbb{S}^{2}, one finds

gijT\displaystyle g^{T}_{ij} =hijN2iTjT\displaystyle=h_{ij}-N^{2}\partial_{i}T\partial_{j}T (6.10)
KijT\displaystyle K^{T}_{ij} =iTjN+jTiN+NHessh(T)ijN2iTjTdN(gradh(T))1N2|dT|h2\displaystyle=\frac{\partial_{i}T\partial_{j}N+\partial_{j}T\partial_{i}N+N\mathrm{Hess}_{h}(T)_{ij}-N^{2}\partial_{i}T\partial_{j}T\,dN(\mathrm{grad}_{h}(T))}{\sqrt{1-N^{2}|dT|^{2}_{h}}} (6.11)

on the graph MT={t=T(x):x3C}M_{T}=\{t=T(\vec{x}):\vec{x}\in\mathbb{R}^{3}\setminus C\}, see Figure 2.

Refer to caption
Figure 2: Graphical example in Schwarzschild spacetime for {t=T1}\{t=T_{1}\}, logarithmic plot.

Choosing

T1(x)=sin(lnr)+uxr\displaystyle T_{1}(\vec{x})=\sin(\ln r)+\frac{\vec{u}\cdot\vec{x}}{r} (6.12)

as in [5] for non-trivial u3\vec{u}\in\mathbb{R}^{3}, one obtains a relativistic initial data set (MT1,gT1,KT1)(M_{T_{1}},g^{T_{1}},K^{T_{1}}) which satisfies neither the weak nor the strong Regge–Teitelboim conditions with respect to x\vec{x}; in fact, CBÓRT\vec{C}_{\text{B\'{O}RT}} diverges like sin(lnr)u\sin(\ln r)\vec{u} in this example, see [5, 4]. It is worth noting that the metric gT1g^{T_{1}} in fact does satisfy the weak (but not the strong) Regge–Teitelboim conditions with respect to x\vec{x} (see [5]); they fail to hold only for KT1K^{T_{1}}.

Suitably exploiting Theorems 6.1 and 6.2 and the decay of T1T_{1}, NN, and hh, one can assert that (MT1,gT1,KT1)(M_{T_{1}},g^{T_{1}},K^{T_{1}}) does not satisfy the weak nor the strong Regge–Teitelboim conditions in any asymptotically Euclidean coordinate chart.

Similarly, choosing

T2(x)=sin(lnr)rβ\displaystyle T_{2}(\vec{x})=\frac{\sin(\ln r)}{r^{\beta}} (6.13)

for 0<β<120<\beta<\frac{1}{2}, one finds that (MT2,gT2,KT2)(M_{T_{2}},g^{T_{2}},K^{T_{2}}) does satisfy the weak Regge–Teitelboim conditions (for ε<12\varepsilon<\frac{1}{2}) but does not possess any asymptotically Euclidean coordinate chart in which the strong Regge–Teitelboim conditions hold. Again, the problematic (non-)decay occurs in KT2K^{T_{2}}.

6.2 Why the Weak Regge–Teitelboim Conditions are Relevant for the Center of Mass

Finally, we still owe the reader a justification of why the weak Regge–Teitelboim conditions are relevant for the study of the center of mass CBÓRT\vec{C}_{\text{B\'{O}RT}}: Indeed, Huisken and Yau in [8] developed an alternative definition of center of mass, called CCMC\vec{C}_{\text{CMC}}, via asymptotic Constant Mean Curvature (CMC) foliations. In a series of works culminating in a paper by Nerz [10], it was shown that, for asymptotically Euclidean relativistic initial data sets satisfying the weak Regge–Teitelboim conditions, one has

CBÓRT=CCMC\displaystyle\vec{C}_{\text{B\'{O}RT}}=\vec{C}_{\text{CMC}} (6.14)

in the sense that either both centers diverge or both converge to the same limit.

Refer to caption
Figure 3: The leaves of a foliation near infinity and their images in 3\mathbb{R}^{3} under the asymptotic coordinates x\vec{x}. The crossed positions indicate the Euclidean coordinate centers c(Σσ)\vec{c}\,(\Sigma_{\sigma}) of the surfaces Σσ\Sigma_{\sigma} of the same color (representing the same parameter σ\sigma).

Roughly, Huisken and Yau in [8] and Nerz in [10] prove existence and uniqueness of a foliation (that is, a smoothly parametrized partition into smooth 22-spheres parametrized by σ(0,σ0)\sigma\in(0,\sigma_{0})) of the asymptotic end of an asymptotically Euclidean relativistic initial data set, such that the leaves have constant mean (i.e., average extrinsic) curvature H(Σσ)=σH(\Sigma_{\sigma})=\sigma. The leaves (i.e., the 22-spheres) Σσ\Sigma_{\sigma} of this foliation are indicated as colored curves in Figure 3. Pushing forward the leaves via the asymptotic coordinates x\vec{x}, x(Σσ)\vec{x}(\Sigma_{\sigma}), gives rise to a foliation of a neighborhood of infinity in 3\mathbb{R}^{3} and one computes the average position of a point on x(Σσ)\vec{x}(\Sigma_{\sigma}) in 3\mathbb{R}^{3} as

c(Σσ)=1|x(Σσ)|x(Σσ)x𝑑Aδ,\displaystyle\vec{c}(\Sigma_{\sigma})=\frac{1}{|\vec{x}(\Sigma_{\sigma})|}\iint_{\vec{x}(\Sigma_{\sigma})}\vec{x}\,dA_{\delta}, (6.15)

where |x(Σσ)||\vec{x}(\Sigma_{\sigma})| denotes the surface area of x(Σσ)\vec{x}(\Sigma_{\sigma}) in 3\mathbb{R}^{3} with respect to the Euclidean metric δ\delta, see Figure 3. The center CCMC\vec{C}_{\text{CMC}} then arises as the limit

CCMC=limσ0c(Σσ)\displaystyle\vec{C}_{\text{CMC}}=\lim_{\sigma\to 0}\vec{c}(\Sigma_{\sigma}) (6.16)

outward along this foliation, provided this limit exists. We refer the interested reader to [5] for more information on this construction and its dependence on the choice of asymptotic coordinates.

6.2.1 Spacetime Equivariance

It was observed by Cederbaum and Sakovich in [6] that the divergence issue of both notions of center of mass for (MT1,gT1,KT1)(M_{T_{1}},g^{T_{1}},K^{T_{1}}) — i.e., the one defined via a Hamiltonian systems approached by Beig and Ó Murchadha in [3] and the one defined via foliations — is rooted in the lack of dependence on KK in both approaches. Generalizing the Constant Mean Curvature foliation approach, they construct asymptotic ”Spacetime Constant Mean Curvature (STCMC)” foliations in asymptotically Euclidean relativistic initial data sets, see below. These allow for the definition of a generally covariant center of mass CSTCMC\vec{C}_{\text{STCMC}} as well as a correction term Z\vec{Z} for CBÓRT\vec{C}_{\text{B\'{O}RT}} such that

CSTCMC=CBÓRT+Z\displaystyle\vec{C}_{\text{STCMC}}=\vec{C}_{\text{B\'{O}RT}}+\vec{Z} (6.17)

holds under the weak Regge–Teitelboim conditions in the sense that either both sides of the equation diverge or both converge to the same limit. The definition of CSTCMC\vec{C}_{\text{STCMC}} mimicks the definition of CCMC\vec{C}_{\text{CMC}}, see Figure 3, based on the Spacetime Constant Mean Curvature instead of on the (spatial) Constant Mean Curvature foliation. As expected from the spacetime symmetry, one finds CSTCMC=0\vec{C}_{\text{STCMC}}=\vec{0} in the graphical example for the graph function T1T_{1} in (6.12).

It is also proved in [6] that CSTCMC\vec{C}_{\text{STCMC}} evolves in time such that

ddtCSTCMC=PADMEADM\displaystyle\frac{d}{dt}\vec{C}_{\text{STCMC}}=\frac{\vec{P}_{\text{ADM}}}{E_{\text{ADM}}} (6.18)

under the Einstein Evolution Equations, just as a freely falling point particle in Special Relativity. This applies even when CSTCMC\vec{C}_{\text{STCMC}} does not converge.

Before we end this section, let us briefly address what it means that a surface Σ\Sigma has ”constant spacetime mean curvature”: If one considers a 22-surface Σ\Sigma not only as sitting inside the relativistic initial data set (M,g,K)(M,g,K) but also as sitting inside the spacetime generated from this relativistic initial data set via the Einstein Evolution Equations then it can be viewed as a co-dimension 22 surface in this spacetime. As such, it has co-dimension 22 extrinsic curvature, taking the form of a normal vector valued symmetric (0,2)(0,2)-tensor field. The trace (or average) of this normal vector valued symmetric (0,2)(0,2)-tensor field is called the spacetime mean curvature vector (field) \overrightarrow{\mathcal{H}} of Σ\Sigma. The Lorentzian length of \overrightarrow{\mathcal{H}}, \mathcal{H}, is called the spacetime mean curvature of Σ\Sigma. Then, a spacetime constant mean curvature surface is a surface with =const\mathcal{H}=\text{const}. It turns out that one can compute \mathcal{H} from the initial data alone, without any reference to the ambient spacetime, and one finds

=H2(trΣK)2,\displaystyle\mathcal{H}=\sqrt{H^{2}-(\operatorname{tr}_{\Sigma}K)^{2}}, (6.19)

where trΣK\operatorname{tr}_{\Sigma}K is the (partial) trace of KK over Σ\Sigma and HH denotes the (spatial) mean curvature of Σ\Sigma within the initial data set already considered in the Constant Mean Curvature foliation suggested by Huisken and Yau. On the other hand, taking a more physical perspective, one finds that

2=θ+θ,\displaystyle\mathcal{H}^{2}=\theta_{+}\theta_{-}, (6.20)

where θ±\theta_{\pm} denote the null expansions of Σ\Sigma in the ambient spacetime.

7 Lessons Learned and Current Research

We have seen that coordinates are messy in the following sense: In Newtonian Gravity, when ahistorically considering general asymptotically Euclidean coordinate charts on 3C\mathbb{R}^{3}\setminus C outside some compact set CC, convergence of the center of mass depends not only on suitable decay of the matter density but also on the choice of coordinate system. Accordingly, in General Relativity, where we generally do not have preferred systems of coordinates, one cannot hope to have convergence of any notion of center of mass in all asymptotically Euclidean coordinate charts. It was suggested to remedy such divergence issues by resorting to asymptotic parity conditions, however, as we showed, not all asymptotically Euclidean relativistic initial data sets have asymptotic parity.

It hence remains an open question whether, instead of asking for asymptotic parity, one can find a condition on asymptotic coordinate charts which is geometric (i.e., coordinate independent) just as Bartnik’s harmonic coordinates, compatible with translations (and reflections), and implies convergence of CSTCMC\vec{C}_{\text{STCMC}}, and of course such that every asymptotically Euclidean relativistic initial data set carries such a coordinate system. Coordinate charts satisfying such a condition could then legitimately be considered a natural analog of Cartesian coordinates in General Relativity. This question is currently studied by the authors and our coauthor Jan Metzger.

Acknowledgements.

This work was supported by the focus program on Geometry at Infinity (Deutsche Forschungsgemeinschaft, SPP 2026). MG also acknowledges support by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) under Germany’s Excellence Strategy – EXC 2121 “Quantum Universe” – 390833306. The authors would like to thank Axel Fehrenbach, Felix Salfelder, Oliver Schoen, Olivia Vičánek Martínez, and Giorgos Vretinaris for help with the graphics.

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