Theoretical models which have been presented include wind compressed discs (Bjorkman and Cassinelli, 1993), wind bi-stability (Lamers and Pauldrach, 1991) and viscous out-flowing discs (Lee et al. 1991, also see Porter 1999).
Each of these models has problems: the wind models (wind compression and bi-stability)
cannot reproduce the Keplerian rotation in the disc as the wind conserves angular
momentum leading to a rotation law similar to v
1/r (see Owocki et al. 1994). The viscous
disc model requires a source of angular momentum to sustain the disc which is currently still
unidentified.
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Sobolev (1960) derived equations that enormously simplified the calculations for radiative transfer in moving atmospheres. The Sobolev approximation is that; the interaction between radiative transfer in a flowing gas is simplified to a local process.
More formally, in the limit of an infinitely narrow interaction region the optical depth, which normally contains an integration of density over distance, depends only on the local conditions at the point of absorption (Lamers and Cassinelli, 1999).
The Sobolev length, Lsob, may be written as
![]() | (1.9) |

is the velocity gradient vector. The Sobolev
optical depth,
sob, may then be written as
![]() | (1.10) |
is the cross-sectional area of interaction and
is the matter density.
Owocki et al. (1996) combined this work with that of the WCD model and found, through 2D
hydrodynamical simulations, that the introduction of these non-radial line driving forces
inhibited the formation of a disc, see Figure 1.8 middle panel. They further modified the
WCD model by introducing the effects of gravity darkening and stellar oblateness, see
Figure 1.8 right panel. Gravity darkening (von Zeipel, 1924) is the decrease in effective
temperature of the equatorial regions of a star due to its rapid rotation (Bjorkman and
Bjorkman, 1994).
The non-radial line-force arises from (i) the stellar oblateness of the stellar surface, which means that the flux vector which should be along the direction of local gravity has a poleward tilt near the star, giving the radiative force a poleward tilt (Owocki et al., 1996). (ii) Asymmetries in the line-of-sight velocity gradient. The lower effective gravity near the equator implies lower outflow speeds, the line of sight velocity gradient is therefore stronger when looking towards the equator rather than the pole when viewed from some mid-latitude location in the wind. Hence photons from the equator impart a stronger impulse than those at the pole, enhancing the the net-poleward line-driving-force (Owocki et al., 1996).
Also to be noted is that WCD models are angular momentum conserving and so the
azimuthal velocity is v
1/r which is in conflict with the observed rotation law of
v
1/r1/2
NRPs cannot, by themselves, eject matter from the surface of a star since the pulsations are too small. Theories which invoke NRP use them to feed energy into the equatorial surface layers to accelerate them to critical velocity. It is then the centrifugal force which causes the mass loss (Balona, 2000).
Whilst a Be star as a whole does not spin at its critical velocity, it has been discussed (see Townsend, 2000a,b) that it may be possible for an equatorial belt to spin at break-up. It would not be possible to observe such a phenomena because the stellar velocity is observed as a whole. It is suggested that NRPs may be able to cause such an effect.
Wind bi-stability is represented by an abrupt “jump” in a star’s terminal velocity (v
) from
v
2.6vesc for stars of spectral type earlier than B1 to v
1.3vesc for those later than
B1, see Figure 1.9.
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The physical process from which the bi-stability jump occurs is thus: radiation driven wind
theory predicts that as a consequence of effective gravity (geff, a decreased gravity
incurred from the radiation pressure of electron scattering) gradually decreasing, the
mass loss rate gradually increases and the terminal velocity gradually decreases.
There is however an abrupt jump in the observed data and models. The difference
between the two data groups is that winds with low Lyman optical depth have a
high ionization and those with high optical depth to Lyman photons have a lower
ionization. The jump is so drastic because once the wind starts to recombine, the
wind velocity decreases and the mass loss rate increases, this causes a high density
in the wind and therefore more recombination. Through a series of monté-carlo
simulations using hydrodynamic codes Vink et al. (1999) find that the FeIV/FeIII
ionization/recombination effect at Teff
25000K is the most dominant process causing the
bi-stability jump.
Lamers and Pauldrach (1991) suggest that this effect may produce out-flowing discs in rapidly rotating early type B-stars. They suggest that the three phases of a Be star, (disc)-(no disc)-(disc re-growth), are explained by the sudden change in the stellar wind. However they must conclude by stating that only if there is some mechanism by which the mass flux at the equator of a B-star is increased more efficiently than by the reduction of gravity will the bi-stability mechanism produce out-flowing discs similar in characteristic to those observed in Be stars.
) is Keplerian (v
R-1/2). At present the viscous disc
model is the only model that naturally yields near Keplerian discs around Be stars
(Okazaki, 2001).
Viscous out-flowing discs successfully reproduce most of the attributes of the observed Be star discs (e.g., continuum excess Porter 1999, V/R variations in the emission lines Okazaki 1997), and indeed are the only discs which can do so that have been suggested to date.