Astronomy:Gibbons–Hawking–York boundary term

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In general relativity, the Gibbons–Hawking–York boundary term is a term that needs to be added to the Einstein–Hilbert action when the underlying spacetime manifold has a boundary. The Einstein–Hilbert action is the basis for the most elementary variational principle from which the field equations of general relativity can be defined. However, the use of the Einstein–Hilbert action is appropriate only when the underlying spacetime manifold is closed, i.e., a manifold which is both compact and without boundary. In the event that the manifold has a boundary , the action should be supplemented by a boundary term so that the variational principle is well-defined.

The necessity of such a boundary term was first realised by James W. York and later refined in a minor way by Gary Gibbons and Stephen Hawking.

For a manifold that is not closed, the appropriate action is

𝒮EH+𝒮GHY=116πd4xgR+18πd3yϵhK,

where 𝒮EH is the Einstein–Hilbert action, 𝒮GHY is the Gibbons–Hawking–York boundary term, hab is the induced metric (see section below on definitions) on the boundary, h its determinant, K is the trace of the second fundamental form, ϵ is equal to +1 where the normal to is spacelike and 1 where the normal to is timelike, and ya are the coordinates on the boundary. Varying the action with respect to the metric gαβ, subject to the condition

δgαβ|=0,

gives the Einstein equations; the addition of the boundary term means that in performing the variation, the geometry of the boundary encoded in the transverse metric hab is fixed (see section below). There remains ambiguity in the action up to an arbitrary functional of the induced metric hab.

That a boundary term is needed in the gravitational case is because R, the gravitational Lagrangian density, contains second derivatives of the metric tensor. This is a non-typical feature of field theories, which are usually formulated in terms of Lagrangians that involve first derivatives of fields to be varied over only.

The GHY term is desirable, as it possesses a number of other key features. When passing to the Hamiltonian formalism, it is necessary to include the GHY term in order to reproduce the correct Arnowitt–Deser–Misner energy (ADM energy). The term is required to ensure the path integral (a la Hawking) for quantum gravity has the correct composition properties. When calculating black hole entropy using the Euclidean semiclassical approach, the entire contribution comes from the GHY term. This term has had more recent applications in loop quantum gravity in calculating transition amplitudes and background-independent scattering amplitudes.

In order to determine a finite value for the action, one may have to subtract off a surface term for flat spacetime:

SEH+SGHY,0=116πd4xgR+18πd3yϵhK18πd3yϵhK0,

where K0 is the extrinsic curvature of the boundary imbedded flat spacetime. As h is invariant under variations of gαβ, this addition term does not affect the field equations; as such, this is referred to as the non-dynamical term.

Introduction to hyper-surfaces

Defining hyper-surfaces

In a four-dimensional spacetime manifold, a hypersurface is a three-dimensional submanifold that can be either timelike, spacelike, or null.

A particular hyper-surface Σ can be selected either by imposing a constraint on the coordinates

f(xα)=0,

or by giving parametric equations,

xα=xα(ya),

where ya(a=1,2,3) are coordinates intrinsic to the hyper-surface.

For example, a two-sphere in three-dimensional Euclidean space can be described either by

f(xα)=x2+y2+z2r2=0,

where r is the radius of the sphere, or by

x=rsinθcosϕ,y=rsinθsinϕ,z=rcosθ,

where θ and ϕ are intrinsic coordinates.

Hyper-surface orthogonal vector fields

We take the metric convention (-,+,...,+). We start with the family of hyper-surfaces given by

f(xα)=C

where different members of the family correspond to different values of the constant C. Consider two neighbouring points P and Q with coordinates xα and xα+dxα, respectively, lying in the same hyper-surface. We then have to first order

C=f(xα+dxα)=f(xα)+fxαdxα.

Subtracting off C=f(xα) from this equation gives

fxαdxα=0

at P. This implies that f,α is normal to the hyper-surface. A unit normal nα can be introduced in the case where the hyper-surface is not null. This is defined by

nαnαϵ={1if Σ is spacelike+1if Σ is timelike

and we require that nα point in the direction of increasing f:nαf,α>0. It can then easily be checked that nα is given by

nα=ϵf,α(ϵgαβf,αf,β)12

if the hyper-surface either spacelike or timelike.

Induced and transverse metric

The three vectors

eaα=(xαya)a=1,2,3

are tangential to the hyper-surface.

The induced metric is the three-tensor hab defined by

hab=gαβeaαebβ.

This acts as a metric tensor on the hyper-surface in the ya coordinates. For displacements confined to the hyper-surface (so that xα=xα(ya))

ds2=gαβdxαdxβ=gαβ(xαyadya)(xβybdyb)=(gαβeaαebβ)dyadyb=habdyadyb

Because the three vectors e1α,e2α,e3α are tangential to the hyper-surface,

nαeaα=0

where nα is the unit vector (nαnα=±1) normal to the hyper-surface.

We introduce what is called the transverse metric

hαβ=gαβϵnαnβ.

It isolates the part of the metric that is transverse to the normal nα.

It is easily seen that this four-tensor

hαβ=δαβϵnαnβ

projects out the part of a four-vector transverse to the normal nα as

hαβnβ=(δαβϵnαnβ)nβ=(nαϵ2nα)=0and ifwαnα=0thenhαβwβ=wα.

We have

hab=hαβeaαebβ.

If we define hab to be the inverse of hab, it is easy to check

hαβ=habeaαebβ

where

hαβ=gαβϵnαnβ.

Note that variation subject to the condition

δgαβ|=0,

implies that hab=gαβeaαebβ, the induced metric on , is held fixed during the variation. See also [1] for clarification on δhαβ and δnα etc.

On proving the main result

In the following subsections we will first compute the variation of the Einstein–Hilbert term and then the variation of the boundary term, and show that their sum results in

δSTOTAL=δSEH+δSGHY=116πGαβδgαβgd4x

where Gαβ=Rαβ12gαβR is the Einstein tensor, which produces the correct left-hand side to the Einstein field equations, without the cosmological term, which however is trivial to include by replacing SEH with

116π(R2Λ)gd4x

where Λ is the cosmological constant.

In the third subsection we elaborate on the meaning of the non-dynamical term.

Variation of the Einstein–Hilbert term

We will use the identity

δg12ggαβδgαβ,

and the Palatini identity:

δRαβμ(δΓαβμ)β(δΓαμμ),

which are both obtained in the article Einstein–Hilbert action.

We consider the variation of the Einstein–Hilbert term:

(16π)δSEH=δ(gαβRαβg)d4x=(Rαβgδgαβ+gαβRαβδg+ggαβδRαβ)d4x=(Rαβ12gαβR)δgαβgd4x+gαβδRαβgd4x.

The first term gives us what we need for the left-hand side of the Einstein field equations. We must account for the second term.

By the Palatini identity

gαβδRαβ=δVμ;μ,δVμ=gαβδΓαβμgαμδΓαββ.

We will need Stokes theorem in the form:

Aμ;μgd4x=(gAμ),μd4x=AμdΣμ=ϵAμnμ|h|d3y

where nμ is the unit normal to and ϵnμnμ=±1, and ya are coordinates on the boundary. And dΣμ=ϵnμdΣ where dΣ=|h|12d3y where h=det[hab], is an invariant three-dimensional volume element on the hyper-surface. In our particular case we take Aμ=δVμ.

We now evaluate δVμnμ on the boundary , keeping in mind that on ,δgαβ=0=δgαβ. Taking this into account we have

δΓαβμ|=12gμν(δgνα,β+δgνβ,αδgαβ,ν).

It is useful to note that

gαμδΓαββ|=12gαμgβν(δgνα,β+δgνβ,αδgαβ,ν)=12gμνgαβ(δgνα,β+δgαβ,νδgνβ,α)

where in the second line we have swapped around α and ν and used that the metric is symmetric. It is then not difficult to work out δVμ=gμνgαβ(δgνβ,αδgαβ,ν).

So now

δVμnμ|=nμgαβ(δgμβ,αδgαβ,μ)=nμ(ϵnαnβ+hαβ)(δgμβ,αδgαβ,μ)=nμhαβ(δgμβ,αδgαβ,μ)

where in the second line we used the identity gαβ=ϵnαnβ+hαβ, and in the third line we have used the anti-symmetry in α and μ. As δgαβ vanishes everywhere on the boundary , its tangential derivatives must also vanish: δgαβ,γecγ=0. It follows that hαβδgμβ,α=habeaαebβδgμβ,α=0. So finally we have

nμδVμ|=hαβδgαβ,μnμ.

Gathering the results we obtain

(16π)δSEH=Gαβδgαβgd4xϵhαβδgαβ,μnμhd3yEq1.

We next show that the above boundary term will be cancelled by the variation of SGHY.

Variation of the boundary term

We now turn to the variation of the SGHY term. Because the induced metric is fixed on , the only quantity to be varied is K is the trace of the extrinsic curvature.

We have

K=nα;α=gαβnα;β=(ϵnαnβ+hαβ)nα;β=hαβnα;β=hαβ(nα,βΓαβγnγ)

where we have used that 0=(nαnα);β implies nαnα;β=0. So the variation of K is

δK=hαβδΓαβγnγ=hαβnγ12gγσ(δgσα,β+δgσβ,αδgαβ,σ)=12hαβ(δgμα,β+δgμβ,αδgαβ,μ)nμ=12hαβδgαβ,μnμ

where we have use the fact that the tangential derivatives of δgαβ vanish on . We have obtained

(16π)δSGHY=ϵhαβδgαβ,μnμhd3y

which cancels the second integral on the right-hand side of Eq. 1. The total variation of the gravitational action is:

δSTOTAL=116πGαβδgαβgd4x.

This produces the correct left-hand side of the Einstein equations. This proves the main result.

This result was generalised to fourth-order theories of gravity on manifolds with boundaries in 1983[2] and published in 1985.[3]

The non-dynamical term

We elaborate on the role of

S0=18πϵK0|h|12d3y

in the gravitational action. As already mentioned above, because this term only depends on hab, its variation with respect to gαβ gives zero and so does not effect the field equations, its purpose is to change the numerical value of the action. As such we will refer to it as the non-dynamical term.

Let us assume that gαβ is a solution of the vacuum field equations, in which case the Ricci scalar R vanishes. The numerical value of the gravitational action is then

S=18πϵK|h|12d3y,

where we are ignoring the non-dynamical term for the moment. Let us evaluate this for flat spacetime. Choose the boundary to consist of two hyper-surfaces of constant time value t=t1,t2 and a large three-cylinder at r=r0 (that is, the product of a finite interval and a three-sphere of radius r0). We have K=0 on the hyper-surfaces of constant time. On the three cylinder, in coordinates intrinsic to the hyper-surface, the line element is

ds2=dt2+r02dΩ2=dt2+r02(dθ2+sin2θdϕ2)

meaning the induced metric is

hab=[1000r02000r02sin2θ].

so that |h|12=r02sinθ. The unit normal is nα=αr, so K=nα;α=2/r0. Then

ϵK|h|12d3y=t1t2dt02πdφ0πdθ(2r0)(r02sinθ)=8πr0(t2t1)

and diverges as r0, that is, when the spatial boundary is pushed to infinity, even when the is bounded by two hyper-surfaces of constant time. One would expect the same problem for curved spacetimes that are asymptotically flat (there is no problem if the spacetime is compact). This problem is remedied by the non-dynamical term. The difference SGHYS0 will be well defined in the limit r0.

Variation of modified gravity terms

Main page: Physics:Alternatives to general relativity

There are many theories which attempt to modify General Relativity in different ways, for example f(R) gravity replaces R, the Ricci scalar in the Einstein–Hilbert action with a function f(R). Guarnizo et al. found the boundary term for a general f(R) theory.[4] They found that the "modified action in the metric formalism of f(R) gravity plus a Gibbons–York–Hawking like boundary term must be written as:"

Smod=12κVd4xgf(R)+2Vd3yϵ|h|f(R)K

where f(R)df(R)dR.

By using the ADM decomposition and introducing extra auxiliary fields, in 2009 Deruelle et al. found a method to find the boundary term for "gravity theories whose Lagrangian is an arbitrary function of the Riemann tensor."[5] This method can be used to find the GHY boundary terms for Infinite derivative gravity.[6]

A path-integral approach to quantum gravity

As mentioned at the beginning, the GHY term is required to ensure the path integral (a la Hawking et al.) for quantum gravity has the correct composition properties.

This older approach to path-integral quantum gravity had a number of difficulties and unsolved problems. The starting point in this approach is Feynman's idea that one can represent the amplitude

g2,ϕ2,Σ2|g1,ϕ1,Σ1

to go from the state with metric g1 and matter fields ϕ1 on a surface Σ1 to a state with metric g2 and matter fields ϕ2 on a surface Σ2, as a sum over all field configurations g and ϕ which take the boundary values of the fields on the surfaces Σ1 and Σ2. We write

g2,ϕ2,Σ2|g1,ϕ1,Σ1=𝒟[g,ϕ]exp(iS[g,ϕ])

where 𝒟[g,ϕ] is a measure on the space of all field configurations g and ϕ, S[g,ϕ] is the action of the fields, and the integral is taken over all fields which have the given values on Σ1 and Σ2.

It is argued that one need only specify the three-dimensional induced metric h on the boundary.

Now consider the situation where one makes the transition from metric h1, on a surface Σ1, to a metric h2, on a surface Σ2 and then on to a metric h3 on a later surface Σ3

One would like to have the usual composition rule

h3,Σ3|h1,Σ1=h2h3,Σ3|h2,Σ2h2,Σ2|h1,Σ1

expressing that the amplitude to go from the initial to final state to be obtained by summing over all states on the intermediate surface Σ2.

Let g1 be the metric between Σ1 and Σ2 and g2 be the metric between Σ2 and Σ3. Although the induced metric of g1 and g2 will agree on Σ2, the normal derivative of g1 at Σ2 will not in general be equal to that of g2 at Σ2. Taking the implications of this into account, it can then be shown that the composition rule will hold if and only if we include the GHY boundary term.[7]

In the next section it is demonstrated how this path integral approach to quantum gravity leads to the concept of black hole temperature and intrinsic quantum mechanical entropy.

Calculating black-hole entropy using the Euclidean semi-classical approach

Main page: Physics:Euclidean quantum gravity


Application in loop quantum gravity

Main page: Physics:Loop quantum gravity

Transition amplitudes and the Hamilton's principal function

In the quantum theory, the object that corresponds to the Hamilton's principal function is the transition amplitude. Consider gravity defined on a compact region of spacetime, with the topology of a four dimensional ball. The boundary of this region is a three-dimensional space with the topology of a three-sphere, which we call Σ. In pure gravity without cosmological constant, since the Ricci scalar vanishes on solutions of Einstein's equations, the bulk action vanishes and the Hamilton's principal function is given entirely in terms of the boundary term,

S[q]=ΣKab[q]qabqd3σ

where Kab is the extrinsic curvature of the boundary, qab is the three-metric induced on the boundary, and σ are coordinates on the boundary.

The functional S[q] is a highly non-trivial functional to compute; this is because the extrinsic curvature Kab[q] is determined by the bulk solution singled out by the boundary intrinsic geometry. As such Kab[q] is non-local. Knowing the general dependence of Kab from qab is equivalent to knowing the general solution of the Einstein equations.

Background-independent scattering amplitudes

Loop quantum gravity is formulated in a background-independent language. No spacetime is assumed a priori, but rather it is built up by the states of theory themselves – however scattering amplitudes are derived from n-point functions (Correlation function (quantum field theory)) and these, formulated in conventional quantum field theory, are functions of points of a background space-time. The relation between the background-independent formalism and the conventional formalism of quantum field theory on a given spacetime is far from obvious, and it is far from obvious how to recover low-energy quantities from the full background-independent theory. One would like to derive the n-point functions of the theory from the background-independent formalism, in order to compare them with the standard perturbative expansion of quantum general relativity and therefore check that loop quantum gravity yields the correct low-energy limit.

A strategy for addressing this problem has been suggested;[8] the idea is to study the boundary amplitude, or transition amplitude of a compact region of spacetime, namely a path integral over a finite space-time region, seen as a function of the boundary value of the field.[9][10] In conventional quantum field theory, this boundary amplitude is well-defined[11][12] and codes the physical information of the theory; it does so in quantum gravity as well, but in a fully background-independent manner.[13] A generally covariant definition of n-point functions can then be based on the idea that the distance between physical points – arguments of the n-point function is determined by the state of the gravitational field on the boundary of the spacetime region considered.

The key observation is that in gravity the boundary data include the gravitational field, hence the geometry of the boundary, hence all relevant relative distances and time separations. In other words, the boundary formulation realizes very elegantly in the quantum context the complete identification between spacetime geometry and dynamical fields.

See also

Notes

  1. Feng, J. C., Matzner R. A. The Weiss variation of the gravitational action. Theory Group, Department of Physics, University of Texas at Austin. arXiv:1708.04489v3 [gr-qc]. 24 July 2018 https://arxiv.org/pdf/1708.04489
  2. "Second and fourth order gravitational actions on manifolds with boundaries" (in en). https://www.researchgate.net/publication/34874539. 
  3. Barth, N H (1985-07-01). "The fourth-order gravitational action for manifolds with boundaries". Classical and Quantum Gravity (IOP Publishing) 2 (4): 497–513. doi:10.1088/0264-9381/2/4/015. ISSN 0264-9381. Bibcode1985CQGra...2..497B. https://www.researchgate.net/publication/230911526. 
  4. Guarnizo, Alejandro; Castaneda, Leonardo; Tejeiro, Juan M. (2010). "Boundary Term in Metric f(R) Gravity: Field Equations in the Metric Formalism". General Relativity and Gravitation 42 (11): 2713–2728. doi:10.1007/s10714-010-1012-6. Bibcode2010GReGr..42.2713G. 
  5. Deruelle, Nathalie; Sasaki, Misao; Sendouda, Yuuiti; Yamauchi, Daisuke (2010). "Hamiltonian formulation of f(Riemann) theories of gravity". Progress of Theoretical Physics 123 (1): 169–185. doi:10.1143/PTP.123.169. Bibcode2010PThPh.123..169D. 
  6. Teimouri, Ali; Talaganis, Spyridon; Edholm, James; Mazumdar, Anupam (2016). "Generalised Boundary Terms for Higher Derivative Theories of Gravity". Journal of High Energy Physics 2016 (8): 144. doi:10.1007/JHEP08(2016)144. Bibcode2016JHEP...08..144T. 
  7. For example see the book "Hawking on the big bang and black holes" by Stephen Hawking, chapter 15.
  8. Modesto, Leonardo; Rovelli, Carlo (2005-11-01). "Particle Scattering in Loop Quantum Gravity". Physical Review Letters 95 (19): 191301. doi:10.1103/physrevlett.95.191301. ISSN 0031-9007. PMID 16383970. Bibcode2005PhRvL..95s1301M. 
  9. Oeckl, Robert (2003). "A "general boundary" formulation for quantum mechanics and quantum gravity". Physics Letters B (Elsevier BV) 575 (3–4): 318–324. doi:10.1016/j.physletb.2003.08.043. ISSN 0370-2693. Bibcode2003PhLB..575..318O. 
  10. Oeckl, Robert (2003-11-03). "Schrödinger's cat and the clock: lessons for quantum gravity". Classical and Quantum Gravity 20 (24): 5371–5380. doi:10.1088/0264-9381/20/24/009. ISSN 0264-9381. Bibcode2003CQGra..20.5371O. 
  11. Conrady, Florian; Rovelli, Carlo (2004-09-30). "Generalized Schrödinger equation in Euclidean field theory". International Journal of Modern Physics A (World Scientific Pub Co Pte Lt) 19 (24): 4037–4068. doi:10.1142/s0217751x04019445. ISSN 0217-751X. Bibcode2004IJMPA..19.4037C. 
  12. Doplicher, Luisa (2004-09-24). "Generalized Tomonaga-Schwinger equation from the Hadamard formula". Physical Review D (American Physical Society (APS)) 70 (6): 064037. doi:10.1103/physrevd.70.064037. ISSN 1550-7998. Bibcode2004PhRvD..70f4037D. 
  13. Conrady, Florian; Doplicher, Luisa; Oeckl, Robert; Rovelli, Carlo; Testa, Massimo (2004-03-18). "Minkowski vacuum in background independent quantum gravity". Physical Review D (American Physical Society (APS)) 69 (6): 064019. doi:10.1103/physrevd.69.064019. ISSN 1550-7998. Bibcode2004PhRvD..69f4019C. 

References