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This article has an erratum: [https://doi.org/10.1051/0004-6361/200912084e]

   

Table 2:

Input parameters ($L_\star $, $T_{\rm eff}$, $\log$(C-O), P) and the resulting avergage mass loss rate, average wind speed and the mean degree of dust condensation at the outer boundary for a subset of models with $M_\star = 1~M_\odot$ and $\Delta u_{\rm p} = 4.0~\mbox{km~s}^{-1}$.

$\log(L_\star)$ 		$T_{\rm eff}$ log(C-O)+12 P $\langle\dot{M}\rangle$ $\langle u_{\rm out} \rangle$ $\langle {\rm f_c} \rangle$ $\langle {\rho_{\rm d}/\rho_{\rm g}} \rangle$ $\langle a_{\rm gr}\rangle$
[$L_\odot$] [$\mbox{K}$]   [days] [$M_\odot$ yr-1] [km s-1]     [cm]
3.70 2400 8.20 295 - - - - 1.26E-04
3.70 2400 8.50 295 1.05E-06 3.80E+00 2.44E-01 6.61E-04 2.32E-05
3.70 2400 8.80 295 3.02E-06 2.00E+01 3.19E-01 1.73E-03 1.19E-05
3.70 2400 9.10 295 4.46E-06 3.86E+01 4.75E-01 5.13E-03 5.78E-06
3.85 2400 8.20 393 - - - - 1.08E-04
3.85 2400 8.50 393 3.15E-06 7.76E+00 2.13E-01 5.77E-04 2.32E-05
3.85 2400 8.80 393 5.40E-06 2.19E+01 2.85E-01 1.54E-03 1.15E-05
3.85 2400 9.10 393 7.95E-06 4.15E+01 5.24E-01 5.65E-03 6.19E-06
4.00 2400 8.20 524 2.42E-06 8.67E-01 2.54E-01 3.45E-04 8.30E-05
4.00 2400 8.50 524 8.50E-06 1.14E+01 2.15E-01 5.83E-04 2.48E-05
4.00 2400 8.80 524 1.23E-05 2.42E+01 3.36E-01 1.82E-03 1.26E-05
4.00 2400 9.10 524 1.59E-05 4.43E+01 5.88E-01 6.34E-03 6.70E-06
3.70 2600 8.20 295 - - - - -
3.70 2600 8.50 295 7.60E-07 6.24E+00 2.11E-01 5.72E-04 -
3.70 2600 8.80 295 1.95E-06 2.68E+01 4.00E-01 2.16E-03 1.41E-05
3.70 2600 9.10 295 3.96E-06 4.39E+01 5.84E-01 6.30E-03 7.38E-06
3.85 2600 8.20 393 - - - - 1.05E-04
3.85 2600 8.50 393 1.67E-06 6.24E+00 1.71E-01 4.63E-04 1.87E-05
3.85 2600 8.80 393 4.04E-06 2.65E+01 3.22E-01 1.74E-03 1.24E-05
3.85 2600 9.10 393 5.66E-06 4.65E+01 5.25E-01 5.67E-03 6.20E-06
4.00 2600 8.20 524 1.22E-06 1.34E+00 2.06E-01 2.80E-04 5.52E-05
4.00 2600 8.50 524 4.85E-06 1.04E+01 1.57E-01 4.26E-04 2.10E-05
4.00 2600 8.80 524 8.43E-06 2.80E+01 3.25E-01 1.76E-03 1.18E-05
4.00 2600 9.10 524 1.09E-05 4.55E+01 4.88E-01 5.27E-03 6.26E-06
3.70 2800 8.20 295 - - - - -
3.70 2800 8.50 295 - - - - -
3.70 2800 8.80 295 1.46E-06 3.00E+01 4.55E-01 2.46E-03 1.66E-05
3.70 2800 9.10 295 2.52E-06 4.10E+01 4.69E-01 5.06E-03 6.94E-06
3.85 2800 8.20 393 - - - - -
3.85 2800 8.50 393 1.49E-06 1.71E+01 2.25E-01 6.10E-04 -
3.85 2800 8.80 393 2.71E-06 2.83E+01 3.15E-01 1.70E-03 1.28E-05
3.85 2800 9.10 393 4.77E-06 4.68E+01 5.14E-01 5.55E-03 7.57E-06
4.00 2800 8.20 524 - - - - 5.71E-05
4.00 2800 8.50 524 3.72E-06 1.31E+01 1.72E-01 4.66E-04 2.15E-05
4.00 2800 8.80 524 5.76E-06 2.81E+01 2.94E-01 1.59E-03 1.33E-05
4.00 2800 9.10 524 8.07E-06 4.96E+01 3.87E-01 4.18E-03 6.12E-06
3.70 3000 8.20 295 - - - - -
3.70 3000 8.50 295 - - - - -
3.70 3000 8.80 295 - - - - 1.25E-05
3.70 3000 9.10 295 5.50E-07 3.09E+01 2.84E-01 3.06E-03 4.79E-06
3.85 3000 8.20 393 - - - - -
3.85 3000 8.50 393 - - - - -
3.85 3000 8.80 393 1.47E-06 3.12E+01 3.76E-01 2.03E-03 -
3.85 3000 9.10 393 3.62E-06 4.27E+01 4.25E-01 4.59E-03 6.55E-06
4.00 3000 8.20 524 - - - - -
4.00 3000 8.50 524 1.72E-06 1.83E+01 1.75E-01 4.74E-04 2.66E-05
4.00 3000 8.80 524 3.85E-06 2.73E+01 2.86E-01 1.55E-03 1.21E-05
4.00 3000 9.10 524 8.00E-06 4.76E+01 5.56E-01 6.00E-03 7.43E-06
3.70 3200 8.20 295 - - - - -
3.70 3200 8.50 295 - - - - -
3.70 3200 8.80 295 - - - - -
3.70 3200 9.10 295 1.13E-06 4.56E+01 3.22E-01 3.47E-03 5.64E-06
3.85 3200 8.20 393 - - - - -
3.85 3200 8.50 393 - - - - -
3.85 3200 8.80 393 - - - - -
3.85 3200 9.10 393 5.17E-07 3.98E+01 2.77E-01 2.99E-03 5.03E-06
4.00 3200 8.20 524 - - - - -
4.00 3200 8.50 524 - - - - -
4.00 3200 8.80 524 1.64E-06 3.33E+01 3.09E-01 1.67E-03 1.47E-05
4.00 3200 9.10 524 3.68E-06 5.10E+01 3.65E-01 3.94E-03 5.75E-06

The dust-to-gas mass ratio $\rho_{\rm d}/\rho_{\rm g}$ is calculated from $f_{\rm c}$ as described in Höfner & Dorfi (1997) and the grain radius is defind as $a_{\rm gr}=r_0~(K_1/K_0)$, where K0, K1 are the zeroth and first moment of the grain-size distribution, respectively. Models with $\log$(C-O)+12 = 7.90 are not included, since none of them produced any outflow.


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