We use a fixed spatial mesh of 10637 points. In order to adequately resolve the region of rapid acceleration, the initial 1025 points have a spacing that increases linearly from 0.001 to 0.01 R* over the radius range r = 1-5 R*. The remaining points use a constant spacing of 0.01 R*spanning the range r= 5-101 R*.
| quantity | symbol | value |
| stellar mass | M | 40 |
| photospheric radius | R* | 19 |
| effective temperature |
|
37800 K |
| CAK exponent | 0.7 | |
| opacity constant |
|
3500 cm2/g |
| line strength cut-off |
|
0.001 |
| H abundance by mass | X | 0.73 |
| He abundance by mass | Y | 1-X |
| thermal speed |
|
0.28
|
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Figure 1: Snapshot of the reference model in the inner wind, at 2.0 Msec after the start of the simulation. The dashed line in the upper panels represents time-averaged values. |
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Figure 2: Same as Fig. 1, but for a representative portion of the outer wind. Note that the range in radius is larger than on the previous figure. |
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Figure 4: Snapshot of the reference model at 2 Msec, now plotted versus the Lagrangian mass coordinate m defined in Eq. (10). The upper panel shows the Eulerian radius, while the remaining panels show the velocity, density, and temperature. The dashed lines in these lower panels show the corresponding time-averaged values. |
Figures 1 and 2 show snapshots of the radial variation of velocity, density and temperature in the inner and outer wind. Many of the features have been extensively discussed in other papers (e.g. OCR, Feldmeier 1995; Feldmeier et al. 1997b, OP99), and so here we focus mainly on the radial evolution of the overall structure properties.
The wind can be divided into a number of geometric regions for which the boundaries are somewhat fuzzy, but which nevertheless have their own typical characteristics.
The outflow at the base of the wind is almost steady.
But starting at
irregular variations appear in the velocity and density. The variations
rapidly steepen into shocks
(for a detailed discussion of the onset of structure in SSF models, see OP99).
These initial shocks are reverse type, which means that they propagate
inward relative to the gas, although the overall outflow advects them outward
relative to the star. They decelerate and compress rarefied gas that
has been accelerated to high-speed by the instability. Most of the
velocity peaks in the upper panel of
Fig. 1
are steep rarefaction waves terminated by a reverse shock.
In this initial structure, most of the stellar wind material thus becomes collected into in a sequence of dense clumps bounded on the inside by a reverse shock that separates the clumps from the much more rarefied, high speed flow in between them. After a few stellar radii many clumps also become bounded on the outside by a weaker forward shock, whenever clumps flow faster than material ahead of them. For example, a weak forward shock is visible around 5.3 R*, just beyond a strong reverse shock. The structure then finds its definite form: a sequence of dense clumps bounded on both sides by shocks that feed rarefied gas into the clumps. Most of the shocks in Fig. 2 occur in such reverse-forward pairs.
The clumps are typically an order of magnitude denser than the average wind.
They move at approximately the terminal velocity but have finite
relative velocities, causing them to collide and form
denser clumps. This can be seen from
Fig. 3, which shows the
density (normalised to the mean density
)
as a
function of radius and time, with the dark streaks indicating the
motion of a clump. The importance of clump collisions for X-ray production
has been emphasised by Feldmeier et al. (1997b). In the simulations
by these authors, the base of the wind was perturbed by a sound wave
or turbulence. Our results show that clump collisions can also
occur when the structure is self-excited, although generally
with lower relative speeds than in the perturbed models.
As they result in denser clumps,
collisions also play an important rôle in maintaining structure.
Note moreover that collisions can persist to quite large distances from
the star.
Fig. 4 shows a wind snapshot at 2 Msec
plotted versus a Lagrangian mass coordinate (OCR, OP99) defined by
On the other hand, the mass plots of velocity and density illustrate quite well the persistence of substantial velocity dispersion and clumping through an extended range of material in the outer wind.
At the base of the wind (below
), the mass distribution is
smooth (
)
and the variations in the velocity are
extremely small (
).
As is typical for SSF calculations (OP99), structure appears with almost
perfectly anti-correlated variations of density and velocity (
).
These variations grow dramatically and steepen into shocks.
The subsequent nonlinear interaction from clump collisions quickly
disrupts this flow anti-correlation, so that above
there is little net velocity-density correlation, indicating there is
roughly equal mixture of forward and reverse propagating structure.
The steep initial rise in velocity dispersion reflects the initial
strong amplification of velocity variations by the line-driven
instability. This initial rise is temporarily halted as the high-speed
rarefactions are filled in and the anti-correlation vanishes.
But then,
quite surprisingly, there develops a second rise in dispersion,
characterised now by little net correlation between velocity and density.
Moreover, even after the dispersion reaches an absolute maximum rms
amplitude of
kms-1 at around
,
the subsequent
decline is quite gradual, with a residual dispersion of
kms-1persisting even at
.
Perhaps even more surprising, the density clumping factor actually continues
to rise out to nearly
.
The supersonic collisions among the clumps tend to compress them
further, causing a steady rise in the clumping factor.
But as these collisions become weaker and less frequent in the outer
wind, the pressure-driven expansion of individual clumps into the rarefied
regions between them eventually causes the overall clumping factor to slowly decline.
One simple way to maintain structure up to large distances would be to have cold, high density gas in pressure equilibrium with hot, rarefied gas. Shocks do heat some gas to very high temperatures, but due to the efficiency of radiative cooling, only the most rarefied gas can remain hot. It is, however, not hot enough to balance the pressure of the dense clumps. It appears therefore, that under the present assumptions, clump collisions are the key mechanism to maintain a structured wind.
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Figure 6: Statistical properties of the reference model (solid line), compared to two models where the external forces have been set to zero beyond 11 R*(dotted line) and 31 R* (dashed line). |
Copyright ESO 2002