General Relativity
© The scientific sentence. 2010
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Relativity: Equivalence Energy-Metric
1. Vectorial expression of the geodesic equation
The Geodesic equation is :
dvk/dτ +
Γkijvivj = 0
In terms of coordinates, it is:
d2xα/dτ2 +
Γαμν (dxμ/dτ)(dxν/dτ) = 0
Or
d2xα/dτ2 = -
Γαμν (dxμ/dτ)(dxν/dτ)
We will take the following approximation and
generalize after.
The motion of the particle is slow (v << c), and
The gravitational field is week and stationary (static).
The motion of the particle is slow implies
neglecting the spatial part terms dx1/dτ, dx2/dτ,
dx3/dτ in comparison with the
term dx0/dτ = c dt/dτ. Then the geodesic equation becomes:
d2xα/dτ2 = -
Γα00 c2 (dt/dτ)2
The field is week implies:
∂gμν/∂t = 0.
Therefore the affine
connection, that is the Christoffel symbol:
Γkij = (1/2) gkl
[dgil/∂xj + dgjl/∂xi - dgij/∂xl]
becomes:
Γα00 = (1/2) gαβ
[dg0β/∂x0 + dg0β/∂x0 - dg00/∂xβ]
=
(1/2) gαβ
[2 dg0β/∂x0 - dg00/∂xβ]
We have:
2 ∂g0β/∂x0 = 0 (field is week). It remains:
Γα00 = (-1/2) gαβ
∂g00/∂xβ
Γα00 = (-1/2) gαβ
∂g00/∂xβ
For a week field we have:
gμν = ημν + hμν + O(h2)
and
∂gμν/∂t =
c ∂gμν/∂x0 = 0
Where
hμν is the first order deviation in h from the flat Minkowski space
(space time) that corresponds to the absence of gravitational field: |hμν| < 1.
Therefore:
Γα00 = (-1/2) ηαβ
∂h00/∂xβ
= (-1/2) δαβ
∂h00/∂xβ
And only the spatial parts of remains. We have the Kronecker in the Minkowski space-time:
δαβ = - 1 for spatial parts.
So
Γα00 = (1/2) dh00/∂xβ
Γα00 = (1/2) dh00/∂xβ
The geodesic equation, with c = 1, then becomes:
d2xα/dτ2 = (- 1/2)
(dt/dτ)2 dh00/∂xβ
d2xα/dτ2 = (- 1/2)
(dt/dτ)2 ∂h00/∂xβ
Vectorially, for the spacial parts:
∂
d2xα/dτ2 = (- 1/2)
(dt/dτ)2 ∇βh00
For the approximations considered:
The motion of the particle is slow , and
the gravitational field is week and stationary,
we have dt/dτ = 1,
so
The geodesic equation, with c = 1, then becomes:
d2xα/dt2 = (- 1/2) ∇βh00
Vectorial Geodesic equation
d2x/dt2 = (- 1/2) ∇βh00
2. Newtonian limit
Recall the Newtonian (classical) acceleration
field g is:
g = g(r) = F/m = (GMm/r2)/m = GM/r2 =
- ∂Φ/∂r,
where Φ = - GM/r is the
Newtonian gravitational potential.
With del or gradient operator, it can be written:
g = - ∇Φ
Its gradient has the expression:
∇. g = - 4 πGρ
And the Poisson's equation for gravity is:
∇2Φ = 4 πGρ
Now, we want the vectorial Geodesic equation:
d2x/dt2 = (- 1/2) ∇βh00
coincides with the newton equation:
g = - ∇Φ
That is:
(- 1/2) ∇βh00 = - ∇Φ
or
h00 = 2Φ + constant
We have the following convention :
Far from any masses, where Φ = 0, and the metric is gμν = ημν , we have h00 = 0. Then constant = 0
Hence, from the equation:
gμν = ημν + hμν + O(h2)
We have in the weak-field limit:
g00 = 1 + h00 = 1 + 2Φ
g00 = 1 + 2Φ = 1 + 2(Φ/c2)
The Poisson's equation for gravity :
∇2Φ = 4 πGρ
becomes:
∇2Φ = (1/2)∇2g00 = 4 πGρ
But ρ is the T00 component of the tensor Energy-Momentum
Tμν. So
∇2Φ = 4 πGT00
or
(1/2)∇2g00 = 4 πGT00
That is, for a particle moving slowly in a weak gravitational
field:
∇2g00 = 8 πGT00
Particle moving slowly in a weak gravitational
field:
∇2g00 = 8 πGT00
Now, we make a tensor:
g00∇2g00 = 8 πG g00T00
= 8 πG T00
And denote g00∇2g00 by
G00
Therefore:
G00 = 8 πG T00
We generalize and write:
Gμν = 8 πG Tμν
Equivalence Energy-Metric:
Gμν = gμν∇2gμν = 8 πGTμν = (8 πG/c4)Tμν
Recall:
Gμν = 8 πGTμν
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