fbpx
Wikipedia

Linearized gravity

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 edit

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

 

where   is the Ricci tensor,   is the Ricci scalar,   is the energy–momentum tensor, and   is the spacetime metric tensor that represents 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   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]   plus a small perturbation term  . In other words:

 

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

 

where   is the trace of the perturbation,   denotes the partial derivative with respect to the   coordinate of spacetime, and   is the d'Alembert operator.

Together with the Ricci scalar,

 

the left side of the field equation reduces to

 

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

Gauge invariance edit

The process of decomposing the general spacetime   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  . 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   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   is represented as being a consequence of the diverse collection of diffeomorphisms on spacetime that leave   sufficiently small. Therefore to continue, it is required that   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   to denote an arbitrary diffeomorphism that maps the flat Minkowski spacetime to the more general spacetime represented by the metric  . With this, the perturbation metric may be defined as the difference between the pullback of   and the Minkowski metric:

 

The diffeomorphisms   may thus be chosen such that  .

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

 

Therefore, in the limit  ,

 

where   is the Lie derivative along the vector field  .

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

 

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 edit

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

Transverse gauge edit

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

 

(Note that the indices span only spatial components:  ). Thus, by using  , the spatial components of the perturbation can be decomposed as

 

where  .

The tensor   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   to satisfy the relation

 

then choosing the time component   to satisfy

 

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

 

with the additional property:

 

Synchronous gauge edit

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   are zero, namely

 

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

 

and requiring the spatial components to satisfy

 

Harmonic gauge edit

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

 

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

 

Consequently, by using the harmonic gauge, the Einstein tensor   reduces to

 

Therefore, by writing it in terms of a "trace-reversed" metric,  , the linearized field equations reduce to

 

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

See also edit

Notes edit

  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 edit

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

linearized, gravity, theory, general, relativity, linearized, gravity, application, perturbation, theory, metric, tensor, that, describes, geometry, spacetime, consequence, linearized, gravity, effective, method, modeling, effects, gravity, when, gravitational. 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 Contents 1 Weak field approximation 1 1 Gauge invariance 1 2 Choice of gauge 1 2 1 Transverse gauge 1 2 2 Synchronous gauge 1 2 3 Harmonic gauge 2 See also 3 Notes 4 Further readingWeak field approximation editThe Einstein field equation EFE describing the geometry of spacetime is given as using natural units R m n 1 2 R g m n 8 p G T m n displaystyle R mu nu frac 1 2 Rg mu nu 8 pi GT mu nu nbsp where R m n displaystyle R mu nu nbsp is the Ricci tensor R displaystyle R nbsp is the Ricci scalar T m n displaystyle T mu nu nbsp is the energy momentum tensor and g m n displaystyle g mu nu nbsp is the spacetime metric tensor that represents 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 g m n displaystyle g mu nu nbsp 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 h m n displaystyle eta mu nu nbsp plus a small perturbation term h m n displaystyle h mu nu nbsp In other words g m n h m n h m n h m n 1 displaystyle g mu nu eta mu nu h mu nu qquad h mu nu ll 1 nbsp In this regime substituting the general metric g m n displaystyle g mu nu nbsp for this perturbative approximation results in a simplified expression for the Ricci tensor R m n 1 2 s m h n s s n h m s m n h h m n displaystyle R mu nu frac 1 2 partial sigma partial mu h nu sigma partial sigma partial nu h mu sigma partial mu partial nu h square h mu nu nbsp where h h m n h m n displaystyle h eta mu nu h mu nu nbsp is the trace of the perturbation m displaystyle partial mu nbsp denotes the partial derivative with respect to the x m displaystyle x mu nbsp coordinate of spacetime and h m n m n displaystyle square eta mu nu partial mu partial nu nbsp is the d Alembert operator Together with the Ricci scalar R h m n R m n m n h m n h displaystyle R eta mu nu R mu nu partial mu partial nu h mu nu square h nbsp the left side of the field equation reduces to R m n 1 2 R g m n 1 2 s m h n s s n h m s m n h h m n h m n r l h r l h m n h displaystyle R mu nu frac 1 2 Rg mu nu frac 1 2 partial sigma partial mu h nu sigma partial sigma partial nu h mu sigma partial mu partial nu h square h mu nu eta mu nu partial rho partial lambda h rho lambda eta mu nu square h nbsp and thus the EFE is reduced to a linear second order partial differential equation in terms of h m n displaystyle h mu nu nbsp Gauge invariance edit The process of decomposing the general spacetime g m n displaystyle g mu nu nbsp 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 h m n displaystyle h mu nu nbsp 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 h m n displaystyle h mu nu nbsp 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 h m n displaystyle h mu nu nbsp is represented as being a consequence of the diverse collection of diffeomorphisms on spacetime that leave h m n displaystyle h mu nu nbsp sufficiently small Therefore to continue it is required that h m n displaystyle h mu nu nbsp 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 displaystyle phi nbsp to denote an arbitrary diffeomorphism that maps the flat Minkowski spacetime to the more general spacetime represented by the metric g m n displaystyle g mu nu nbsp With this the perturbation metric may be defined as the difference between the pullback of g m n displaystyle g mu nu nbsp and the Minkowski metric h m n ϕ g m n h m n displaystyle h mu nu phi g mu nu eta mu nu nbsp The diffeomorphisms ϕ displaystyle phi nbsp may thus be chosen such that h m n 1 displaystyle h mu nu ll 1 nbsp Given then a vector field 3 m displaystyle xi mu nbsp defined on the flat background spacetime an additional family of diffeomorphisms ps ϵ displaystyle psi epsilon nbsp may be defined as those generated by 3 m displaystyle xi mu nbsp and parameterized by ϵ gt 0 displaystyle epsilon gt 0 nbsp These new diffeomorphisms will be used to represent the coordinate transformations for infinitesimal shifts as discussed above Together with ϕ displaystyle phi nbsp a family of perturbations is given by h m n ϵ ϕ ps ϵ g m n h m n ps ϵ ϕ g m n h m n ps ϵ h h m n h m n ps ϵ h m n ϵ ps ϵ h m n h m n ϵ displaystyle begin aligned h mu nu epsilon amp phi circ psi epsilon g mu nu eta mu nu amp psi epsilon phi g mu nu eta mu nu amp psi epsilon h eta mu nu eta mu nu amp psi epsilon h mu nu epsilon left frac psi epsilon eta mu nu eta mu nu epsilon right end aligned nbsp Therefore in the limit ϵ 0 displaystyle epsilon rightarrow 0 nbsp h m n ϵ h m n ϵ L 3 h m n displaystyle h mu nu epsilon h mu nu epsilon mathcal L xi eta mu nu nbsp where L 3 displaystyle mathcal L xi nbsp is the Lie derivative along the vector field 3 m displaystyle xi mu nbsp The Lie derivative works out to yield the final gauge transformation of the perturbation metric h m n displaystyle h mu nu nbsp h m n ϵ h m n ϵ m 3 n n 3 m displaystyle h mu nu epsilon h mu nu epsilon partial mu xi nu partial nu xi mu nbsp 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 edit By exploiting gauge invariance certain properties of the perturbation metric can be guaranteed by choosing a suitable vector field 3 m displaystyle xi mu nbsp Transverse gauge edit To study how the perturbation h m n displaystyle h mu nu nbsp distorts measurements of length it is useful to define the following spatial tensor s i j h i j 1 3 d k l h k l d i j displaystyle s ij h ij frac 1 3 delta kl h kl delta ij nbsp Note that the indices span only spatial components i j 1 2 3 displaystyle i j in 1 2 3 nbsp Thus by using s i j displaystyle s ij nbsp the spatial components of the perturbation can be decomposed as h i j s i j PS d i j displaystyle h ij s ij Psi delta ij nbsp where PS 1 3 d k l h k l displaystyle Psi frac 1 3 delta kl h kl nbsp The tensor s i j displaystyle s ij nbsp 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 3 m displaystyle xi mu nbsp to satisfy the relation 2 3 j 1 3 j i 3 i i s i j displaystyle nabla 2 xi j frac 1 3 partial j partial i xi i partial i s ij nbsp then choosing the time component 3 0 displaystyle xi 0 nbsp to satisfy 2 3 0 i h 0 i 0 i 3 i displaystyle nabla 2 xi 0 partial i h 0i partial 0 partial i xi i nbsp After performing the gauge transformation using the formula in the previous section the strain becomes spatially transverse i s ϵ i j 0 displaystyle partial i s epsilon ij 0 nbsp with the additional property i h ϵ 0 i 0 displaystyle partial i h epsilon 0i 0 nbsp Synchronous gauge edit 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 h m n ϵ displaystyle h mu nu epsilon nbsp are zero namely h 0 n ϵ 0 displaystyle h 0 nu epsilon 0 nbsp This can be achieved by requiring the time component of 3 m displaystyle xi mu nbsp to satisfy 0 3 0 h 00 displaystyle partial 0 xi 0 h 00 nbsp and requiring the spatial components to satisfy 0 3 i i 3 0 h 0 i displaystyle partial 0 xi i partial i xi 0 h 0i nbsp Harmonic gauge edit 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 m h n m 1 2 n h displaystyle partial mu h nu mu frac 1 2 partial nu h nbsp is true To achieve this 3 m displaystyle xi mu nbsp is required to satisfy the relation 3 m n h m n 1 2 m h displaystyle square xi mu partial nu h mu nu frac 1 2 partial mu h nbsp Consequently by using the harmonic gauge the Einstein tensor G m n R m n 1 2 R g m n displaystyle G mu nu R mu nu frac 1 2 Rg mu nu nbsp reduces to G m n 1 2 h m n ϵ 1 2 h ϵ h m n displaystyle G mu nu frac 1 2 square left h mu nu epsilon frac 1 2 h epsilon eta mu nu right nbsp Therefore by writing it in terms of a trace reversed metric h m n ϵ h m n ϵ 1 2 h ϵ h m n displaystyle bar h mu nu epsilon h mu nu epsilon frac 1 2 h epsilon eta mu nu nbsp the linearized field equations reduce to h m n ϵ 16 p G T m n displaystyle square bar h mu nu epsilon 16 pi GT mu nu nbsp Which can be solved exactly using the wave solutions that define gravitational radiation See also editCorrespondence principle Gravitoelectromagnetism Lanczos tensor Parameterized post Newtonian formalism Post Newtonian expansion Quasinormal modeNotes edit 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 Not to be confused with Lorentz Further reading editSean M Carroll 2003 Spacetime and Geometry an Introduction to General Relativity Pearson ISBN 978 0805387322 Retrieved from https en wikipedia org w index php title Linearized gravity amp oldid 1208630731, wikipedia, wiki, book, books, library,

article

, read, download, free, free download, mp3, video, mp4, 3gp, jpg, jpeg, gif, png, picture, music, song, movie, book, game, games.