Institute of planetary geodesy, Lohrmann-Observatory, Dresden, Germany
(2)
Shanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai, China
5.1 General Relativity
Special Relativity can be described as physics in a 4-dimensional space-time manifold with metric tensor gμν that reduces to ημν = diag(−1, +1, +1, +1) in any global inertial coordinate system. Such selected global coordinates exist because the geometry of Minkowskian space-time is flat, i.e., the curvature and Ricci tensor vanish. Einstein’s theory of gravity is also a structure , but space-time geometry in the presence of gravitational fields is not longer flat, the curvature tensor describing the tidal actions. For vanishing gravitational fields the structure reduces to the Minkowskian space-time; it is fully in accordance with all experiments from Special Relativity.
In General Relativity (GR) all aspects of gravitational fields are contained in the space-time metric tensor. A necessary prerequisite this is the Equivalence principle, that also shows the role of Special Relativity in Einstein’s GT. The weak form of the equivalence principle (the universality of free-fall) has already been discussed. The Einstein equivalence principle (EEP) generalizes this to all non-gravitational laws of physics: in any freely falling system all non-gravitational laws of physics take their form from Special Relativity. In some sense certain aspects of gravity disappear in a freely falling reference frame. Such aspects are related with the affine connections of space-time geometry that are not tensors and can be transformed to zero at any point by a suitable coordinate transformation. This, however, by no means implies that some existing gravitational field inside such a freely-falling system is zero; if the curvature tensor has non-vanishing components in one coordinate system then there is no coordinate system where it completely vanishes at any point . This means that the EEP simply says that at each point p of the space-time manifold there are local coordinates such that the metric tensor reduces to the Minkowskian tensor where effects from gravity do not appear.
Einstein’s equivalence principle implies that a reasonable theory of gravity should be a metric theory with as basic structure and possible additional fields ψi, taking part in the gravitational interaction. General Relativity is the simplest of all such metric theories, where all additional fields ψi = 0. Sources of the gravitational field, i.e., all forms of energy and momentum as well as gravity fields itself, produce curvature of space-time which again determines the dynamical behavior of the sources.
5.2 Einstein’s Equivalence Principle
Einstein’s theory of gravity generalizes the results from Minkowski space-time theory by considering also gravitational fields. A hint of how to incorporate gravity into the space-time structure comes from the phenomenon of gravitational redshift. Let us consider two identical clocks at rest in some gravitational potential U(x). Clock 1 is assumed to be located a distance H above clock 1. Then, because of the gravitational redshift the natural frequencies of the two clocks, f1 and f2, are related by
(5.2.1)
It is not difficult to see that the gravitational redshift
of electromagnetic waves is a consequence of a certain form of the equivalence principle. This will also make it clear why clocks in a gravitational field are running slower (Fig. 5.1).
Fig. 5.1
Three static clocks in some gravitational field. The larger the gravitational potential the slower the clock runs
Einstein’s Equivalence Principle
Everywhere in the universe and for all times in sufficiently small freely falling laboratories all non-gravitational laws of physics take their form from Special Relativity.
In other words: such freely falling systems are locally inertial. Let us now consider two clocks at rest in some external gravitational field (Fig. 5.2). Obviously the two clocks are not freely falling; instead they are at rest in some system that is accelerated upwards, i.e., away from the center of gravitational attraction. With respect to some freely falling local inertial coordinate system xμ = (ct, xi) the world-lines of the two clocks are depicted in Fig. 5.2. We now consider a light-pulse being emitted from clock 1 in the direction of clock 2. In a first approximation z1 = gt2∕2 + H and z2 = gt2∕2 and the velocities are given by v = gt. Since in the accelerated system where the two clocks are at rest the situation is stationary and we might choose for simplicity t = 0 for the emission event. Neglecting (v∕c)2-terms t will agree with the proper times indicated by the two clocks. Then for gH∕c2 ≪ 1 the signal will arrive at clock 2 at t−≃ H∕c. The crucial point is that at the point of reception the second clock has a finite velocity v = gt = gH∕c in the direction of the first clock. Let the first clock emit a second pulse at t = δt1 immediately after the first one. The arrival time at clock 2 then is
since during the interval δt1 it has moved a distance vδt1 in the direction of clock 1, i.e., the effective distance is only H − vδt1 instead of H. Hence the time that has elapsed during the reception of the two pulses at clock 2 is
in accordance with the gravitational redshift formula (5.2.1). Thus from the standpoint of Einstein’s Equivalence Principle the gravitational redshift results from the first-order Doppler shift of frequencies. Einstein’s form of the equivalence principle has the consequence that gravity can be described by a metric theory, i.e., (see e.g., Will 1993 for more details)
by at least a gμν-field and possibly by “other g-fields”;
these “other g-fields” only couple to the gμν-field but not to matter-fields directly;
at each point in space-time there is a local freely falling system (Einstein’s elevator) where the space-time metric gμν reduces to the flat space-time metric ημν;
the world-lines of uncharged test particles are geodesics of gμν.
Fig. 5.2
Two accelerated clocks as seen from a local freely falling system. The distance between the clocks is H. The first clock emits a first signal, a second one follows after a time interval δt1. The observer at z2 receives these two signal at times t− and t+
The last point follows from the fact that these world-lines are straight lines in a freely falling system, i.e., geodesics with respect to the flat space-time metric. Hence, they must be geodesics with respect to the space-time metric gμν.
Metric Property 3
Sufficiently small (uncharged) test bodies move along geodesics of the metric tensor.
The gravitational redshift can then be described in a very elegant manner: we incorporate the gravitational potential U into the metric and write in suitable coordinates
(5.2.2)
or
(5.2.3)
Assuming again metric property 2 (Eq. (4.3.10)) for two clocks at rest (dx = 0) we get for each of the two clocks i:
Let us consider the geometry that is determined by the metric (5.2.3) in more detail where we restrict our discussion to terms of order c−2. The inverse metric tensor in this approximation is given by
(5.3.1)
From this we derive the non-vanishing Christoffel-symbols:
(5.3.2)
We now come to the geodesic equation
Here λ is an affine parameter that might be replaced by the time coordinate t (which is not an affine parameter) in the μ = i equation:
(5.3.3)
(5.3.4)
In more detail this reads (vi ≡ dxi∕dt)
(5.3.5)
Considering the Christoffel-symbols from (5.3.2) we see that the right hand side of this equation has a term of order c0 resulting from . Keeping only this c-independent term the geodesic equation reads
(5.3.6)
This, however, is precisely the equation of free-fall of a sufficiently small test body in Newton’s theory of gravity in Galilean coordinates (Cartesian and inertial).
5.4 Einstein’s Theory of Gravity
Einstein’s theory of gravity is the ‘simplest’ of all reasonable metric theories of gravity. In Einstein’s theory there are no other g-fields but only one space-time metric that also describes gravity.
Metric property 3 indicates an intimate relation between Newton’s theory of gravity and a relativistic one. In both theories test particles move along geodesics of the space-time geometry. As we have seen the Newtonian field equation for the potential U relates the Ricci-tensor of space-time with the field generating source. Now in relativity the source of the gravitational field obviously must be the energy-momentum tensor Tμν and Einstein’s field equations for the metric tensor take the form
where is a function of gμν and its first and second partial derivatives with respect to the coordinates xμ. Because of the conservation laws for energy and momentum, Eq. (4.6.14) we have to require
The most general tensorthat is divergenceless, i.e., obeys Eq.(5.4.1) is of the form
(5.4.2)
where Gμνare the components of the Einstein-tensor.
The usual Einstein’s field equations
are obtained with a = 1 and b = 0:
(5.4.3)
or
(5.4.4)
Another important form of the field equations is obtained by contracting equation (5.4.4) with gμν (i.e., by taking its trace):
where
(5.4.5)
is the trace of the energy-momentum tensor. Inserting this result for the curvature scalar R into Einstein’s field equations leads to the alternative form
(5.4.6)
Finally we have to determine the coupling constant κ. To this end we consider the ‘Newtonian limit’ of these field equations. In Newton’s theory only the matter density ρ acts as source of the gravitational field. This density to lowest order is contained in the time-time component of the energy-momentum tensor, considering a continuous distribution of energy and momentum. From (4.6.7) we see that
(5.4.7)
and for that reason the Newtonian field equation must be contained in the time-time component of (5.4.6):
The left hand side to order c−2 can be taken from Eq. (3.2.21) keeping in mind that now x0 = ct and the dimension of the Einstein tensor is (length)−2:
Hence to lowest order the Einstein field equations lead to
and a comparison with the Poisson equation
(3.2.19) shows that
Einstein’s field equations form a complicated set of ten partial differential equations of second order. Because of the Bianchi identities these ten equations are not independent from each other but only six of them. Hence, the equations determine six out of ten degrees of freedom of the metric tensor gμν. Four degrees of freedom for the metric tensor remain, expressing the freedom in the choice of the four space-time coordinates. Of course the field equations cannot tell what coordinates should be used; instead the coordinates can be fixed by four (more or less) arbitrary conditions for the metric tensor. This is the coordinate or “gauge” freedom of the theory. This gauge freedom is one of the most important differences to the classical Newtonian case. In Newton’s theory time is absolute, so there is a preferred time coordinate which is fixed uniquely up to origin and unit. Out of the many possible spatial coordinates the inertial (Cartesian) ones which in Newton’s theory exist globally are preferred. They are determined uniquely up to origin, unit and orientation in space (determined e.g., by three Euler angles). All these preferred coordinates, however, do not exist in Einstein’s theory of gravity. However, the situation is not too bad for isolated systems with an asymptotically flat space-time. E.g., the solar system might be idealized in this manner: we forget about distant masses and think of the solar system as being isolated. Then far from the solar system the gravitational field will become very small and space-time will approach flat space-time from Special Relativity Theory in this idealized picture. Then in the asymptotic region preferred (inertial and Cartesian) coordinates exist such that there
(5.4.8)
If, however, we get closer to the gravitating masses preferred coordinates cease to exist; i.e., many different coordinates have equal rights.
If we choose a = 1 and b = Λ in Lovelock’s Theorem then we end up with field equations of the form with a Λ term
(5.4.9)
In this case the constant Λ is called the cosmological constant. It is obvious that the Λ-term can be absorbed in the energy-momentum tensor by replacing Tμν by
(5.4.10)
Usually it is assumed that Λ is related with the energy density of the quantum vacuum pervading the whole universe and might have a value of about 10−52 m−2 (Peebles and Ratra 2003). Metric (5.4.9) plays an important role in modern cosmology.
5.5 The Problem of Observables
Since in Einstein’s theory of gravity the coordinates usually have no direct physical meaning the problem of observables
is a serious one. It should be clear that observables are independent of any set of coordinates used by some theorist to describe the system of interest. In other words: observables have to be described by scalars, coordinate independent quantities. First one chooses some appropriate coordinate system and draws a coordinate picture of the system of interest. Then one constructs the observables as scalars from such a coordinate picture.
5.5.1 The Ranging Observable
Let us consider a typical astronomical measurement in the solar system: lunar laser ranging (LLR). Here laser pulses are emitted from LLR-stations on the Earth to retroreflectors on the lunar surface. A few photons per pulse find their way back into the receiving telescope of the station and one measures the total travel time of a pulse from the station to the Moon and back. This situation is depicted in Fig. 5.3. In the right part of the figure we see the world-line of the clock with the two events E: emission of the pulse and R: reception of the pulse. The observed time interval between E and R is then given by
(5.5.1)
with
In practise this indicated time interval Δτ can then be related with a corresponding interval of some other time scale.
Fig. 5.3
Left: A central observable for celestial mechanics, the ranging observable, is a propagation time interval between emission and reception of some electromagnetic pulse. In Lunar Laser Ranging it is a laser pulse that travels from some LLR-station on the Earth to some retro-reflector on the lunar surface and back to the ground station. Right: the observable is the proper time interval that has elapsed between the instant of emission and the instant of reception of an electromagnetic pulse
5.5.2 The Spectroscopic Observable
We now consider the following problem: one observer emits some monochromatic electromagnetic wave of frequency fE. Another observer receives this signal and measures the frequency fR and we ask about the relation between the two frequencies. If we concentrate upon one single light-ray propagating from the emitter to the receiver the situation is shown in Fig. 5.4. Here γE is the world-line of the emitter, γR that of the receiver, γ∗ that of the light ray. Let be the 4-velocity of the emitter at the point of emission, that of the receiver at the point of reception. Let kμ be the tangent vector onto γ∗ then according to (4.3.7) the frequency ratio is given by
(5.5.2)
Let us analyze this situation in Minkowski space in the absence of gravitational fields. Let us choose a Minkowskian coordinate system such that the receiver is at rest in the event of reception, i.e.,
If the emitter has coordinate velocity v at the point of emission then
Since kμ is a null-vector we can write in Minkowskian coordinates
(5.5.3)
with
The normalization constant in kμ will not play a role if only frequency ratios are considered. With
(5.5.4)
we then get
or
(5.5.5)
This is the well-known formula for the Doppler-effect in electromagnetism.
Fig. 5.4
The spectroscopic observable is the frequency ratio fR∕fE. Some observer (emitter) emits some electromagnetic signal of frequency fE. This signal is observed by another observer (receiver) who measures the frequency fR
5.5.3 The Astrometric Observable
In astrometry the principle observable is the observed angle between two incident light-rays. This situation is depicted in Fig. 5.5. Here γ(λ) is the worldline of the observer, and are two light-rays from two different astronomical sources that are simultaneously observed by the observer in some event O. Let uμ be the 4-velocity of the observer in O, and be the wave vectors of the two incident light-rays. Then
(5.5.6)
is a projection tensor that projects vectors into their components perpendicular to uμ, i.e.,
(5.5.7)
since uνuν = −c2. In some sense uμ points into the time-direction of the observer and the projection operator points into the space ‘experienced’ by the observer. Now are null-vectors but
(5.5.8)
is a spacelike vector of non-vanishing length. For
we find
(5.5.9)
and therefore
(5.5.10)
From this it is not difficult to see that
(5.5.11)
The observed angle θ between two incident light-rays and is generally given by
(5.5.12)
In the absence of gravity fields from (5.5.12) we get
(5.5.13)
This is the aberration
formula if gravity fields play no role. A Taylor expansion in terms of c−1 yields
(5.5.14)
Fig. 5.5
The astrometric observable: the observed angle θ between two incident light-rays and . The observer’s worldline is γ(λ) and are tangent vectors to the light-rays
5.6 Tetrads and Tetrad Induced Coordinates
Consider some massless observer E that moves through empty space with a space capsule and wants to perform some local experiment inside of his spacecraft. Let us describe the motion of E in some coordinate system xμ by some timelike worldline , given by , where λ is some affine parameter. Let us choose this parameter λ as the observer’s proper time τ also denoted by T. The tangent vector then is the observer’s 4-velocity that is normalized according to
(5.6.1)
since ds2 = −c2dτ2 along the observer’s world-line. In the following we will denote the unit vector in the direction of uμ by
(5.6.2)
Let
(5.6.3)
be the observer’s 4-acceleration, a vector that is perpendicular to uμ since
(5.6.4)
in virtue of the normalization condition and gμν;σ = 0.
A set of four orthonormal vectors with being given by (5.6.2) and
(5.6.5)
along is called a tetrad field along . Such tetrad fields are valuable quantities that can be used in different respects, e.g., for the construction of observables.
They can also be used to define useful local coordinates Xα = (cT, Xa) for the observer. First the local time coordinates T will be chosen as proper time τ of the observer whose world-line should be given by Xa = 0, i.e., the observer is located at the spatial origin of his local coordinate system. Next we define: a local system of coordinates Xα is called tetrad-induced if
(5.6.6)
From this definition we find that the tetrad vectors in tetrad-induced coordinates (TIC) take a particularly simple form
(5.6.7)
Using this condition in TIC we find
(5.6.8)
Hence, TIC are locally Minkowskian. We will now construct certain TIC in the neighbourhood of by imposing certain constraints on the Christoffel-symbols. To this end we consider the following quantities
(5.6.9)
Because of the simple form of tetrad vectors in TIC, Eq. (5.6.7), we have
that leads to
(5.6.10)
Lemma 5.1
The Christoffel-symbols in TIC obey the following relations at:
(5.6.11)
where Aaare the spatial tetrad components of the 4-acceleration of E, i.e.,
(5.6.12)
and
(5.6.13)
The quantities Ω(
a)(
b)are called Ricci-rotation coefficients.
Exercise 5.1
Use the orthonormality of tetrad vectors to proof the antisymmetry of rotation coefficients
(5.6.14)
The proof of Lemma 5.1 follows from (5.6.10), the definition of the 4-acceleration and the orthonormality of tetrad vectors. This Lemma implies that all Christoffel-symbols of TIC at the observer’s worldline are fixed apart from . We now have several possibilities to fix these remaining quantities at .
Exercise 5.2
Suppose the X, Y, Z coordinates lines , which are integral curves to the tetrad , are geodesics, parametrized with proper length s. Show that for that case
(5.6.15)
Corresponding TIC will be called local geodetic proper coordinates.
The last Exercise shows one possible choice for . Another one is given by TIC that are locally harmonic. The harmonicity condition at can be written in the form
i.e.,
(5.6.16)
One solution of the harmonicity condition along reads
(5.6.17)
We will call local TIC with such Christoffel-symbols local harmonic proper coordinates.
Because the covariant derivative of the metric tensor vanishes, i.e.,
(5.6.18)
the Christoffel-symbols at determine the partial derivatives of Gαβ at the worldline of E.
Exercise 5.3
Show that condition (5.6.18) for local geodetic proper coordinates proper coordinates leads to
(5.6.19)
Together with this leads to a metric tensor of the form
(5.6.20)
with
(5.6.21)
For local harmonic proper coordinates condition (5.6.18) leads to
(5.6.22)
at the observer’s world-line. Using this leads to a metric tensor of the form
Finally, let us try to understand the meaning of our ‘angular velocity’ Ωb. To this end the definition of the Fermi-derivative is useful. Let Bμ be some contravariant vector-field along with tangent vector field eμ = uμ∕c and 4-acceleration aμ. Then the Fermi-derivative
DF of Bμ is defined by
(5.6.24)
with
(5.6.25)
Exercise 5.4
Show that the Fermi-derivative has the following properties:
(i)
.
(ii)
Let Aμ and Bμ be two contravariant vector-fields along with
Then
(iii)
Let Aμ be some contravariant vector-field along , perpendicular to uμ, then
where ⊥ denotes the projection of a vector Bμ perpendicular to uμ, i.e.,
Let us now consider the vector-field
Obviously we can decompose Cμ according to
i.e., at the observer’s worldline we get
(5.6.26)
From the orthonormality condition
we get
that we can use to rewrite the first term in the right-hand side of (5.6.26). Adding to this equation a vanishing uμaμ-term we get along :
(5.6.27)
This relation proofs the following:
Theorem 5.2
If the tetradalongis Fermi-Walker transported, i.e.,
the Ricci rotation-coefficients vanish, i.e., Ω(a)(b) = 0.
Finally let us study the motion of a test-body in free-fall in the vicinity of the observer. Let denote the world-line of this test-body, given by a geodesic of the form
that we will analyze at , i.e., for Za = 0. By taking into account of the corresponding Christoffel-symbols at Xa = 0 this equation in local harmonic proper coordinates takes the form
(5.6.28)
with V ≡ dZ∕dT. Hence, Ω describes nothing but a Coriolis-force due to the rotational motion of spatial axes. The term on the right-hand side of (5.6.28) presents the inertial acceleration due to the 4-acceleration of the observer.
Exercise 5.5
Show that in local geodetic proper coordinates the geodesic equation at takes the form (see also Misner et al. 1973, Exercise (13.14))
(5.6.29)
Local TIC will be called dynamically non-rotating or locally inertial if Ω = 0. In that case the local reference system will show no inertial forces due to the rotational motion of spatial basis vectors. Technically speaking this means that G0a = 0 for dynamically non-rotating local coordinates. As we have seen the dynamically non-rotating local proper coordinates result from Fermi-transported tetrad vectors.
5.7 Proper Reference Systems of Accelerated Observers
Let us start with inertial Minkowskian coordinates xμ = (ct, x) and consider an observer that is moving along the x-axis with constant 4-acceleration, i.e.,
(5.7.1)
Together with uμuμ = −c2 or
(5.7.2)
and uμaμ = 0, i.e.,
(5.7.3)
we get
or
(5.7.4)
Thus,
(5.7.5)
A special solution of these two differential equations is given by
(5.7.6)
with
From this we get
(5.7.7)
and
(5.7.8)
Since the trajectory of the observer, , is given by
(5.7.9)
i.e., by a hyperbola in our inertial Minkowskian coordinates. Next we construct a local co-moving tetrad field along . The observer’s 4-velocity reads
so that the unit vector in the direction of uμ is given by
(5.7.10)
The corresponding spatial tetrad vectors, kinematically non-rotating with respect to the original Minkowskian coordinates, can then be chosen according to
(5.7.11)
It is interesting to note that this tetrad field can easily be obtained from the Minkowskian basic vectors at rest:
(5.7.12)
We first write the tetrads in terms of the observer’s coordinate velocity
(5.7.13)
With
we get
(5.7.14)
From this we see that the co-moving tetrads can be obtained from by means of a Lorentz-boost:
(5.7.15)
with
(5.7.16)
Nest we consider the coordinate transformation from inertial Minkowskian coordinates xμ = (ct, x) to local co-moving coordinates Xα = (cT, X) with T = τ, the proper-time of the observer, with the ansatz
(5.7.17)
where ξμ is at least of second order in |X|. For the Jacobian of this transformation
(5.7.18)
we get
(5.7.19)
Since
can be written in the form
(5.7.20)
with
Now, our original Minkowskian coordinates are both geodetic and harmonic. For the local coordinates the condition of TIC ensures that the local metric tensor, Gαβ, is Minkowskian at the origin, i.e., Gαβ(X = 0) = ηαβ. Higher order terms in |X|, linear, quadratic and higher are not fixed so far. We can fix them by coordinate conditions that we can impose on the local coordinates or we can specify the transformation functions ξμ.
Let us start with
(5.7.21)
Then the metric tensor Gαβ in local coordinates according to the tensor transformation rule takes the form:
(5.7.22)
or
(5.7.23)
Exercise 5.6
Proof that the spatial coordinate lines X = X(λ);T = τ = const. are geodesics, i.e., the coordinates (cT, X) defined by are geodesic proper coordinates.
Next we will assume a special form of the local metric tensor
(5.7.24)
In that case
(5.7.25)
and
(5.7.26)
so that these spatial coordinates are harmonic up to terms of order c−4.
Exercise 5.7
Show that the local metric (5.7.24) can be obtained with
(5.7.27)
where
(5.7.28)
5.8 The Landau-Lifshitz Formulation of GR
5.8.1 The Landau-Lifshitz Field Equations
Landau and Lifshitz (1941, 1971) have derived a special form of the Einstein field equations, which presents a very useful starting point for solving the field equations with perturbative expansions. The atomic variable of the Landau-Lifshitz (LL) formalism is called hαβ, defined by (5.8.13) and the field equation in harmonic gauge are quasi-linear hyperbolic differential equations of the form , where is the flat space d’Alembertian (the flat space wave operator) and ταβ is the gravitational source tensor, that itself contains hαβ-terms. Under a condition of ‘no incoming gravitational radiation’, the field equations (in harmonic gauge) can formally be solved in terms of retarded integrals (see (5.8.36) below) over quantities involving the atomic variable itself. To derive explicit results for hαβ, the source term ταβ can be expanded in terms of small quantities as measures of weak gravitational fields, small velocities and small internal stresses. The MPM-formalism discussed in Chap. 7 presents such a scheme, where suitable expansions of ταβ lead to fully explicit expressions for hαβ, even at high orders in the small parameters.
The LL-formalism is based upon the ‘gothic metric’, defined by
(5.8.1)
where . Note, that is not a tensor but a tensor density. Let be the inverse of and . Then,
Equation (5.8.10) is equivalent to the local equations of motion: Tαβ;β = 0 .
Exercise 5.8
At a certain point choose local coordinates such that the first derivatives of the usual covariant metric tensor vanishes at p, i.e., gαβ,γ(p) = 0. Show that in such coordinates at p: and
in accordance with (5.8.6). Details can be found in Poisson & Will (2014).
5.8.2 Harmonic Gauge
The formulation of the harmonic gauge is especially simple in terms of the gothic metric:
(5.8.12)
Let us define
(5.8.13)
Then the harmonic condition reads:
(5.8.14)
Exercise 5.9
Show that the following relations hold:
(5.8.15)
(5.8.16)
(5.8.17)
(5.8.18)
where indices on hαβ are lowered and contracted with the Minkowski metric ημν, thus hαβ ≡ ηαμηβνhμν and h ≡ ηαβhαβ.
Solution
From the definitions we have
(5.8.19)
Next we compute which is a polynomial of 4th order in G. We get
and with (1 + x)−1∕2 = 1 − x∕2 + 3x2∕8 + …, relation (5.8.16) follows. gαβ can then be obtained from gαβ = (−g)−1∕2(ηαβ + hαβ) and it is easy to check that gαβ is inverse to gαβ, i.e., .
Exercise 5.10
Assume that h00 is of order c−2, h0i of order c−3 and hij of order c−4. Show that (Poisson and Will 2014):
(5.8.20)
(5.8.21)
(5.8.22)
(5.8.23)
(5.8.24)
In the harmonic gauge we have
(5.8.25)
where
(5.8.26)
is the flat-space d’Alembertian. Then the field equations take the form
(5.8.27)
or
(5.8.28)
with
(5.8.29)
and
(5.8.30)
Usually the Einstein field equations in harmonic gauge are written in the form
(5.8.31)
where the ‘gravitational source term’ Λαβ reads
or, written out
(5.8.32)
We see that the gravitational source terms contains products of the metric tensor that are at least quadratic in h and first and second derivatives. We write in obvious notation
(5.8.33)
with
(5.8.34)
All indices are lowered and raised with the Minkowski metric ημν; h ≡ ηαβhαβ; the parenthesis around indices indicate symmetrization. Explicit expressions for and can be found in Blanchet and Faye (2001a).
Under certain assumptions the field equations (5.8.28) can formally be solved. Usually one imposes some ‘no incoming radiation’ condition of the form
(5.8.35)
Under this condition equation (5.8.28) is formally solved by