In our radiation-hydrodynamical calculations, energy conservation is
enforced and the radiative luminosity of the infinite layer per unit
area equals the accretion energy
.
Any real emision region,
however, has a finite lateral width and looses energy not only from
its top and bottom surfaces but also from its sides (Fig. 1).
Two-dimensional radiation hydrodynamics would then be needed to
calculate the temperature structure. In this section we discuss to
what extent our one-dimensional results are still applicable to
regions of finite extent.
We consider an emission region as depicted in Fig. 1, with finite
width D, cross section D2, and field strength B. In a first
step, we adopt the temperature and velocity profiles along the flow
lines, T(x) and
,
calculated for infinite D also for
the case of finite D.
In the Rybicki code the radiation transport equation was solved with a
mean cyclotron absorption coefficient and electron scattering was
included. For the emission region of finite extent, we calculate the
outgoing flux at angle
by ray tracing using the
temperature profiles along slanted paths as shown schematically in
Fig. 1. For rays starting or ending on the side surfaces, the
temperature and density profiles were truncated appropriately. We
account separately for the cyclotron emissivities in the ordinary ray
(index o) and the extraordinary ray (index e), and add 50% of the
free-free emissivity with Gaunt factor to both. We neglect electron
scattering in the emission region, but include the atmospheric albedo
(van Teeseling et al. 1994). Each ray yields a contribution
to the integrated intensity
(in ergs-1Hz-1sr-1) in that direction and the
summation is extended over n rays,
Figure 8 shows the spectral flux at
against the field direction emitted by an emission region with B =
30MG and an area of 1016cm2 (D = 108cm) on an
0.6
white dwarf at a distance of 10 pc. Cyclotron emission
dominates for low
and bremsstrahlung for high
.
Free-free absorption becomes important near 1015Hz at the
highest
,
but in reality this spectral region is dominated by
the quasi-blackbody component produced by reprocessing of the incident
flux in the white dwarf atmosphere. The results of WB96 on the ratio
of the cyclotron vs. bremsstrahlung luminosities as a function of
and B remain basically valid, but will be modified if the
shock is buried in the atmosphere and X-ray absorption is accounted
for.
Figure 9 illustrates the optical depth dependence of the
cyclotron spectra at
.
Cyclotron emission
lines at low
change into absorption features at high
.
Since in real emission regions the fractional area of the
high-
section is small (Rousseau et al. 1996) observed spectra
show emission lines.
An isolated emission region of lateral width D, shock height
,
and the temperature profile T(x) of the infinite layer appropriate
for the mass flow density
will have
for optically thin and
for optically thick
emission. The overestimate in the latter case results from radiation
emerging from the sides of the region without a compensating
influx. For the optical depths considered here, bremsstrahlung is
practically free of such overestimate, cyclotron radiation is not.
Let us assume for the infinite layer that
feeds two components of
,
namely
and
.
For finite D, we then have
![]() |
Figure 10: Quantity A from Eq. (24) measuring
the excess luminosity
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
In order to assess the size of the possible error for AMHer stars,
we estimate
/D for a typical accretion rate of
gs-1 as a function of
.
The linear width of
the emission region is
cm with
in gcm-2s-1. For a
bremsstrahlung-dominated flow, Eq. (14) yields
(for
= 0.6
)
which is less than unity since in this case
gcm-2s-1. For
a cyclotron-dominated flow, Eq. (21) correspondingly yields
which is
again less than unity since now
gcm-2s-1 and typically
B7 > 1. Hence,
is seriously overestimated only for
isolated narrow subcolumns which are not radiatively shielded by
neighboring fluxtubes.
Let the application of the unmodified one-dimensional temperature
profile T(x)yield a specific luminosity
with r > 1. We can then take then either: (i)
identify the parameters of this emission region with those appropriate
for the increased mass flow rate
;
or (ii) recalculate the emission for a reduced mass flow rate
and identify temperature and emission of that region
as appropriate for the initial
.
In case (ii),
and
are reduced to
(
)
and
(
). This approach
demonstrates that the rising sections of the relations displayed in
Fig. 5 (Eq. (19)) and Fig. 6 (Eq. (20))
are further depressed for narrow columns, while the horizontal parts,
where optically thin bremsstrahlung dominates, are not affected. Both
approaches secure energy conservation but cannot replace a proper
treatment of the problem. They are not recommended for isolated tall
columns.
Copyright ESO 2001