Astron. Astrophys. 326, 13-22 (1997)
7. Density perturbations
Let us define the relative perturbed density as:
![[EQUATION]](img149.gif)
( is not so defined by other authors. Some
others adopt which becomes in this case
times the value of our
). The final purpose is to deduce
, i.e. how density inhomogeneities evolve,
under the action of gravity and an unperturbed underlying magnetic
configuration. To find the differential equation for
, we must perform some algebra because our set
of equations is still rather large and complicated. We must first
choose which equations will be handled, because as stated before, they
are not all independent. Our unknowns are ,
, , as
has already been determined as a function of
time. We therefore have ten unknowns. The Einstein field equations are
also made up of ten equations, and from them the equations of motion
and energy are derivable. On the other hand, Maxwell's equations have
already been used to deduce the evolution of the magnetic field and
the electrical current. Though we could therefore use only the
Einstein field equations, the final objective is straightforwardly
reached with the equation of motion (54), the equation of energy
balance (49), and Eqs. (62) and (63) from the whole set of Einstein
field equations, selected because they do not contain the tensor
but just its trace h. The unknowns are
now , and h. We
still have more equations than unknowns. Let us rewrite the equations
with the introduction of "present day" quantities, with the subindex
0.
![[EQUATION]](img157.gif)
![[EQUATION]](img158.gif)
![[EQUATION]](img159.gif)
![[EQUATION]](img160.gif)
Here and would
actually be the present values of p and
if our equations were valid for all subsequent periods. The law
is valid for photons in the Acoustic and
Post-Recombination eras. However has recently
been affected by non-linear effects and probably does not coincide
with the present magnetic field. While and
are constant, and
are not. Neither nor
represent actual present values, but they are
preferred as variables because in the variations of
and the effect of pure
expansion is suppressed. We then have:
![[EQUATION]](img166.gif)
![[EQUATION]](img167.gif)
![[EQUATION]](img168.gif)
![[EQUATION]](img169.gif)
As suggested by the equations themselves, we now change the
temporal and spatial variables, and use the definition (64) of
. As new spatial variables we will use
![[EQUATION]](img170.gif)
where K is the constant in the expansion law
![[EQUATION]](img171.gif)
in the radiation-dominated era. Its value is
![[EQUATION]](img172.gif)
and is the cosmological scale factor at the
last time in the period considered in this paper, which is close to
Equality. For we have adopted the value
. It should be noted that
are comoving coordinates measured in seconds.
They now coincide with present coordinates. (It is easily obtained
that ). However is
dimensionless
![[EQUATION]](img178.gif)
where d is the distance in Mpc.
As a temporal variable let us choose
![[EQUATION]](img179.gif)
and therefore
![[EQUATION]](img180.gif)
where is the last time of the period
considered here, close to Equality, corresponding to
, i.e. .
is a time variable increasing backwards from
future to past. We then introduce some time independent functions
defining the magnetic pattern:
![[EQUATION]](img185.gif)
![[EQUATION]](img186.gif)
![[EQUATION]](img187.gif)
where is the gradient using
instead of . In the
unit system we are using . In this way all the
magnitudes of the different quantities involved are close to unity and
the equations become extremely simple.
We also change the nomenclature, so that a point over a quantity's
symbol now means its derivative with respect to
, instead of with respect to t. Thus we
have
![[EQUATION]](img190.gif)
![[EQUATION]](img191.gif)
![[EQUATION]](img192.gif)
![[EQUATION]](img193.gif)
Taking in Eq. (84) and
in equation (85) and subtracting, inserting
this in Eq. (82) to obtain
, calculating in Eq.
(83), taking into account the obtained functions
and in Eq. (84), we
obtain a differential equation containing only
as a variable,
![[EQUATION]](img197.gif)
This is our basic equation, an elliptic linear second order
differential equation with variable coefficients. The complete
discussion may have complications arising from its elliptic nature (if
we prefer not to choose a boundary condition for
). The following section contains a preliminary
insight.
© European Southern Observatory (ESO) 1997
Online publication: April 20, 1998
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