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Gravity and Strings

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6.1 The traditional approach 175<br />

Having the total conserved energy–momentum pseudotensor obeying the local continuity<br />

equation, we go on to define the conserved charges (momentum <strong>and</strong> angular momentum)<br />

by the volume integrals7 P µ <br />

=<br />

M µα <br />

=<br />

<br />

<br />

dd−1 √<br />

ν |g|(Tmatter µν + tLL µν ),<br />

dd−1 √ <br />

[α<br />

ν |g| 2x Tmatter µ]ν + tLL µ]ν ,<br />

(6.11)<br />

where it is assumed that one integrates over a timelike hypersurface .<br />

One of the shortcomings of this approach is that it is not clear why these are the (only)<br />

conserved charges <strong>and</strong> how we can generalize it to other spacetimes in which these are not<br />

necessarily the conserved charges. The Abbott–Deser approach will solve this problem.<br />

A second shortcoming is the large number of terms that have to be calculated in order<br />

to find the conserved quantities. In practice, though, one uses Eq. (6.8) to rewrite, using<br />

Stokes’ theorem,<br />

P µ = 1<br />

<br />

2<br />

∂<br />

d d−2 η<br />

νρ<br />

µνρ<br />

√ |g| , (6.12)<br />

<strong>and</strong> similarly for M µα . This is an interesting expression that has to be evaluated at the<br />

boundary of the hypersurface , which is, typically, for asymptotically flat spacetimes a<br />

(d − 2)-sphere at spatial infinity Sd−2 ∞ .Wecould integrate over the boundary of smaller<br />

regions of the spacetime. However, the integr<strong>and</strong> is not a general-covariant tensor <strong>and</strong> the<br />

result of the integral would be coordinate-dependent <strong>and</strong> the momentum would not be well<br />

defined. Only when we integrate over Sd−2 ∞ in asymptotically flat spacetimes does the integral<br />

transform as a Poincaré tensor. This is the common behavior of most superpotentials<br />

used to defined conserved quantities in GR, except for Møller’s [702], which is a true tensor.<br />

For asymptotically flat spaces, we can use the weak-field expansion8 gµν = ηµν + hµν.<br />

In this limit, we see that<br />

g µσ,νρ = K µσ νρ + O(h 2 ), (6.13)<br />

<strong>and</strong><br />

η µνρ = 2η µνρ<br />

LL + O(h2 ), 2∂ρη µνρ<br />

LL = Dµν (h), (6.14)<br />

where η µνρ<br />

LL was defined in Eq. (3.90) <strong>and</strong> Dµν (h) is the Fierz–Pauli wave operator.<br />

Thus, in practice, all we have to do is to integrate the Fierz–Pauli wave operator over<br />

the volume or ηLL over the boundary ∂,ifthe asymptotic weak-field expansion of<br />

the metric is well defined. Many different gravity energy–momentum pseudotensors have<br />

been proposed in the literature but, in the end, one never uses them directly. Instead one<br />

integrates over , using the equations of motion, an expression that, in the weak-field<br />

limit, is equivalent to the Fierz–Pauli wave operator. Usually this expression is rewritten as<br />

an integral over the boundary using Stokes’ theorem. This can be done in many different<br />

ways, as we discussed in Chapter 3, <strong>and</strong> here is where the differences arise. 9<br />

7 Observe the “extra” factors of √ |g|.<br />

8 Observe that the hµν that we are using in this chapter is χhµν of Chapter 3.<br />

9 Some expressions may be better suited for certain boundary conditions. When we compare the weak-field<br />

limits of the various expressions proposed in the literature, we have to bear in mind that the expansions used<br />

are valid only under certain asymptotic conditions.

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