Physics:Linearized gravity

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Short description: Linear perturbations to solutions of nonlinear Einstein field equations

In the theory of general relativity, linearized gravity is the application of perturbation theory to the metric tensor that describes the geometry of spacetime. As a consequence, linearized gravity is an effective method for modeling the effects of gravity when the gravitational field is weak. The usage of linearized gravity is integral to the study of gravitational waves and weak-field gravitational lensing.

Weak-field approximation

The Einstein field equation (EFE) describing the geometry of spacetime is given as (using natural units)

Rμν12Rgμν=8πGTμν

where Rμν is the Ricci tensor, R is the Ricci scalar, Tμν is the energy–momentum tensor, and gμν is the spacetime metric tensor that represent the solutions of the equation.

Although succinct when written out using Einstein notation, hidden within the Ricci tensor and Ricci scalar are exceptionally nonlinear dependencies on the metric which render the prospect of finding exact solutions impractical in most systems. However, when describing particular systems for which the curvature of spacetime is small (meaning that terms in the EFE that are quadratic in gμν do not significantly contribute to the equations of motion), one can model the solution of the field equations as being the Minkowski metric[note 1] ημν plus a small perturbation term hμν. In other words:

gμν=ημν+hμν,|hμν|1.

In this regime, substituting the general metric gμν for this perturbative approximation results in a simplified expression for the Ricci tensor:

Rμν=12(σμhνσ+σνhμσμνhhμν),

where h=ημνhμν is the trace of the perturbation, μ denotes the partial derivative with respect to the xμ coordinate of spacetime, and =ημνμν is the d'Alembert operator.

Together with the Ricci scalar,

R=ημνRμν=μνhμνh,

the left side of the field equation reduces to

Rμν12Rgμν=12(σμhνσ+σνhμσμνhhμνημνρλhρλ+ημνh).

and thus the EFE is reduced to a linear, second order partial differential equation in terms of hμν.

Gauge invariance

The process of decomposing the general spacetime gμν into the Minkowski metric plus a perturbation term is not unique. This is due to the fact that different choices for coordinates may give different forms for hμν. In order to capture this phenomenon, the application of gauge symmetry is introduced.

Gauge symmetries are a mathematical device for describing a system that does not change when the underlying coordinate system is "shifted" by an infinitesimal amount. So although the perturbation metric hμν is not consistently defined between different coordinate systems, the overall system which it describes is.

To capture this formally, the non-uniqueness of the perturbation hμν is represented as being a consequence of the diverse collection of diffeomorphisms on spacetime that leave hμν sufficiently small. Therefore to continue, it is required that hμν be defined in terms of a general set of diffeomorphisms then select the subset of these that preserve the small scale that is required by the weak-field approximation. One may thus define ϕ to denote an arbitrary diffeomorphism that maps the flat Minkowski spacetime to the more general spacetime represented by the metric gμν. With this, the perturbation metric may be defined as the difference between the pullback of gμν and the Minkowski metric:

hμν=(ϕ*g)μνημν.

The diffeomorphisms ϕ may thus be chosen such that |hμν|1.

Given then a vector field ξμ defined on the flat, background spacetime, an additional family of diffeomorphisms ψϵ may be defined as those generated by ξμ and parameterized by ϵ>0. These new diffeomorphisms will be used to represent the coordinate transformations for "infinitesimal shifts" as discussed above. Together with ϕ, a family of perturbations is given by

hμν(ϵ)=[(ϕψϵ)*g]μνημν=[ψϵ*(ϕ*g)]μνημν=ψϵ*(h+η)μνημν=(ψϵ*h)μν+ϵ[(ψϵ*η)μνημνϵ].

Therefore, in the limit ϵ0,

hμν(ϵ)=hμν+ϵξημν

where ξ is the Lie derivative along the vector field ξμ.

The Lie derivative works out to yield the final gauge transformation of the perturbation metric hμν:

hμν(ϵ)=hμν+ϵ(μξν+νξμ),

which precisely define the set of perturbation metrics that describe the same physical system. In other words, it characterizes the gauge symmetry of the linearized field equations.

Choice of gauge

By exploiting gauge invariance, certain properties of the perturbation metric can be guaranteed by choosing a suitable vector field ξμ.

Transverse gauge

To study how the perturbation hμν distorts measurements of length, it is useful to define the following spatial tensor:

sij=hij13δklhklδij

(Note that the indices span only spatial components: i,j{1,2,3}). Thus, by using sij, the spatial components of the perturbation can be decomposed as

hij=sijΨδij

where Ψ=13δklhkl.

The tensor sij is, by construction, traceless and is referred to as the strain since it represents the amount by which the perturbation stretches and contracts measurements of space. In the context of studying gravitational radiation, the strain is particularly useful when utilized with the transverse gauge. This gauge is defined by choosing the spatial components of ξμ to satisfy the relation

2ξj+13jiξi=isij,

then choosing the time component ξ0 to satisfy

2ξ0=ih0i+0iξi.

After performing the gauge transformation using the formula in the previous section, the strain becomes spatially transverse:

is(ϵ)ij=0,

with the additional property:

ih(ϵ)0i=0.

Synchronous gauge

The synchronous gauge simplifies the perturbation metric by requiring that the metric not distort measurements of time. More precisely, the synchronous gauge is chosen such that the non-spatial components of hμν(ϵ) are zero, namely

h0ν(ϵ)=0.

This can be achieved by requiring the time component of ξμ to satisfy

0ξ0=h00

and requiring the spatial components to satisfy

0ξi=iξ0h0i.

Harmonic gauge

The harmonic gauge (also referred to as the Lorenz gauge[note 2]) is selected whenever it is necessary to reduce the linearized field equations as much as possible. This can be done if the condition

μhνμ=12νh

is true. To achieve this, ξμ is required to satisfy the relation

ξμ=νhμν+12μh.

Consequently, by using the harmonic gauge, the Einstein tensor Gμν=Rμν12Rgμν reduces to

Gμν=12(hμν(ϵ)12h(ϵ)ημν).

Therefore, by writing it in terms of a "trace-reversed" metric, h¯μν(ϵ)=hμν(ϵ)12h(ϵ)ημν, the linearized field equations reduce to

h¯μν(ϵ)=16πGTμν.

Which can be solved exactly using the wave solutions that define gravitational radiation.

See also


Notes

  1. This is assuming that the background spacetime is flat. Perturbation theory applied in spacetime that is already curved can work just as well by replacing this term with the metric representing the curved background.
  2. Not to be confused with Lorentz.

Further reading

  • Sean M. Carroll (2003). Spacetime and Geometry, an Introduction to General Relativity. Pearson. ISBN 978-0805387322.