Table 2
Predicted mass-loss rates and terminal velocities for different abundances and different effective temperatures.
| Solar | [C/H] = −1 | [C/H] = 1 | [N/H] = −1 | [N/H] = 1 | [O/H] = −1 | [O/H] = 1 | |||||||||||||||||||||
| Model | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | |||||||||||||
|
|
|||||||||||||||||||||||||||
| T30 | 210 | 3650 | 190 | 2280 | 210 | 5490 | 120 | 4010 | 370 | 4410 | 100 | 4110 | 190 | 4390 | |||||||||||||
| T28 | 160 | 4380 | 150 | 2620 | 110 | 8610 | 67 | 4540 | 160 | 5520 | 160 | 4500 | 130 | 4260 | |||||||||||||
| T26 | 96 | 3070 | 60 | 2400 | 60 | (2340) | 64 | (2440) | 90 | 4790 | 100 | 2990 | 79 | 3040 | |||||||||||||
| T24 | 39 | 1700 | 23 | 1720 | 42 | 1820 | 4.8 | 2040 | 38 | 3620 | 25 | 1850 | 39 | 1700 | |||||||||||||
| T22 | 7.9 | 1690 | 8.5 | 1580 | 14 | 1490 | 0.71 | 1760 | 14 | 2730 | 6.5 | 1820 | 12 | 1600 | |||||||||||||
| T20 | 3.4 | 1290 | 2.3 | 1250 | 1.5 | 1410 | 1.6 | 1260 | 6.4 | 1720 | 3.2 | 1300 | 3.6 | 1200 | |||||||||||||
| T18 | 0.91 | 820 | 0.42 | 460 | 0.58 | 900 | 0.51 | 760 | 1.8 | 1120 | 0.84 | 720 | 0.88 | 790 | |||||||||||||
| T16 | 0.072 | (240) | 0.023 | (180) | 0.06 | 520 | 0.038 | (230) | 0.17 | 420 | 0.058 | (240) | 0.06 | (230) | |||||||||||||
| T14 | no wind | no wind | no wind | no wind | no wind | no wind | no wind | ||||||||||||||||||||
| [Si/H] = 1 | [Si/H] = 2 | [Si/H] = 3 | [S/H] = −1 | [S/H] = 1 | [Fe/H] = 1 | [Fe/H] = 2 | |||||||||||||||||||||
| Model | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | Ṁ | v ∞ | |||||||||||||
|
|
|||||||||||||||||||||||||||
| T30 | 250 | 4020 | 320 | 4490 | 490 | 2910 | 180 | 3720 | 380 | 3390 | 230 | 3040 | 1700 | 1720 | |||||||||||||
| T28 | 180 | 5510 | 210 | 5180 | 240 | 3200 | 130 | 4640 | 280 | 3850 | 140 | 3570 | 370 | 1910 | |||||||||||||
| T26 | 110 | (5270) | 150 | 3720 | 160 | 3070 | 83 | 3220 | 170 | 2820 | 83 | 3060 | 57 | 2390 | |||||||||||||
| T24 | 54 | 4580 | 81 | (1620) | 77 | 2450 | 29 | 1760 | 81 | 1710 | 31 | 1790 | 16 | 1740 | |||||||||||||
| T22 | 21 | 4020 | 23 | 6390 | 9.9 | 2250 | 5.3 | 1820 | 22 | 1730 | 6 | 1900 | 8.5 | 1690 | |||||||||||||
| T20 | 7.5 | 3630 | 8.4 | 7740 | 4.6 | 380 | 3 | 1270 | 4.5 | 1360 | 2.6 | 1320 | 1.8 | 1290 | |||||||||||||
| T18 | 3.1 | 1990 | 3.6 | 5270 | 1.9 | 510 | 0.84 | 790 | 1.4 | 830 | 0.74 | 830 | 0.39 | 790 | |||||||||||||
| T16 | 0.7 | 1400 | 0.7 | 2440 | 0.17 | (170) | 0.056 | (240) | 0.085 | (270) | 0.041 | (250) | no wind | ||||||||||||||
| T14 | 0.01 | 650 | 0.004 | 1290 | 0.002 | 1550 | no wind | no wind | no wind | no wind | |||||||||||||||||
Notes. Mass-loss rates are given in units of 10-11 M⊙ year-1. The terminal velocities v∞ are given in units of km s-1. The terminal velocity in parentheses denotes a model for which it was not possible to calculate a monotonic solution to large radii (see the text).
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