Table 1
Input parameters, clumping stratification, and predicted wind properties of our best-fit R144-primary, R144-secondary, and R136al hydro-dynamic models.
Parameter | R144-prim | R144-sec | R136a1 Fixed Dcl | R136a1 Fixed M, vturb tests | ||
---|---|---|---|---|---|---|
spectral type | WN5/6h | WN6/7h | WN5h | WN5h | WN5h | WN5h |
T⋆[kK] | 49.3 | 45.5 | 46.8 | 46.8 | 47.5 | 48 |
Teff(τRoss = 2/3) [kK] | 45.6 | 41.4 | 46 | 46.2 | 46.1 | 45.7 |
log(L⋆/L⊙) | 6.44 | 6.39 | 6.79 | 6.79 | 6.79 | 6.79 |
R⋆/R⊙ | 22.81 | 25.28 | 37.87 | 37.87 | 36.76 | 36 |
RτRoss = 2/3/R⊙ | 26.62 | 30.41 | 38.78 | 38.82 | 39.01 | 39.74 |
M⋆/M⊙ | 74 | 70 | 233 | 242.1 | 242.1 | 242.1 |
X | 0.25 | 0.3 | 0.5 | 0.5 | 0.5 | 0.5 |
vturb [km s−1] | 21.21 | 21.21 | 21.21 | 21.21 | 70.71 | 100 |
Dcl,∞ | 30 | 22 | 45 | 45 | 40 | 42 |
vcl [km s−1] | 90 | 125 | 100 | 23 | 75 | 82 |
log(![]() |
−4.572 | −4.649 | −4.686 | −4.692 | −4.747 | −4.74 |
v∞[km s−1] | 1361.4 | 1257.9 | 2649.03 | 2722.8 | 2699 | 2672.4 |
log(![]() |
−4.297 | −4.370 | −4.875 | −4.893 | −4.970 | −4.947 |
v(r = rsonic) [km s−1] | 20.53 | 19.53 | 19.99 | 21.07 | 19.1 | 20.98 |
v(r = rcrit) [km s−1] | 29.27 | 28.46 | 29.06 | 29.82 | 73.14 | 101.73 |
βeff,in | 2.6 | 2 | 2.4 | 2.3 | 2.9 | 3.3 |
βeff,out | 1.3 | 1.3 | 0.9 | 0.9 | 1 | 1 |
Γe,R⋆ | 0.713 | 0.701 | 0.608 | 0.574 | 0.591 | 0.588 |
τF,sonic | 1.779 | 1.596 | 0.767 | 0.693 | 0.778 | 0.859 |
τF,crit | 1.592 | 1.383 | 0.734 | 0.666 | 0.576 | 0.541 |
log(QH I[ phot s−1]) | 50.30 | 50.25 | 50.66 | 50.65 | 50.66 | 50.67 |
log(QHe I[ phot s−1]) | 49.73 | 49.62 | 50.10 | 50.07 | 50.12 | 50.14 |
log(QHe II[ phot s−1]) | 40.17 | 40.05 | 41.17 | 41.23 | 41.20 | 41.24 |
Notes. The inputs we adopt from previous literature are marked in bold-faced text. For R144-primary and secondary components, we adopt the luminosities and the dynamical masses from Shenar et al. (2021). The surface H for R144 were also initially adopted from Shenar et al. (2021), but was later reduced by 0.1 to achieve better fits to H/He lines. For R136a1, the luminosities and surface H are adopted from Bestenlehner et al. (2020), and the masses are from homogeneous relations from Gräfener et al. (2011).
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.