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8. Sensitivity to mass-loss rate

 

A change in the mass-loss rate leads to a change in the neutral-hydrogen column seen by the parent photon, and hence the scattering and absorption optical depths. The Raman photons will therefore originate in different parts of the wind for different mass-loss rates, and the line profiles will reflect this. Four models were computed in order to investigate this sensitivity, using mass-loss rates of tex2html_wrap_inline3606 and -8 (Fig. 13 (click here)).

The morphology of the tex2html_wrap_inline3610 (reference-model) polarization profile was discussed earlier. The intensity profile of the tex2html_wrap_inline3612 model shows a two-peaked intensity structure, with the bluewards peak centred at the Raman-line rest wavelength, showing that it is a result of photospheric scattering. The polarized flux is triple-peaked, with all the peaks polarized in the same direction; there is no polarization flip. The three peaks originate in the material between the two stars (approaching the OVI source), in the red-giant photosphere, and in the region `behind' the red giant (as seen from the hot component). There is, relatively speaking, insufficient material `above' and `below' the hot component to introduce significant features at orthogonal polarizations. This interpretation is confirmed by the tex2html_wrap_inline3616 model, which shows a two-peaked intensity profile, with the bluewards peak the strongest. This peak corresponds to photospheric scattering; there is very little scattering in the rarified wind. The polarized flux peak again occurs at the Raman-line rest wavelength, and is a result of photospheric scattering. The very small redward peak is associated with wind scattering in the extended region `behind' the red giant.

The tex2html_wrap_inline3618 model has a higher intensity than the reference model, and shows a four-peaked structure in polarized flux. The first three peaks (going from blue to red) have the same interpretation as in the reference model, with no significant photospheric scattering. The redmost peak arises because there is sufficient wind density the allow multiple scatterings from `above' to `below' the hot component (and vice versa). As expected, therefore, the mass-loss rate (or, more strictly, the density distribution) has a dramatic effect on both the Raman-line intensity and its polarization morphology.


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