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Home All issues Volume 498 / No 2 (May I 2009) A&A, 498 2 (2009) 517-525 Full HTML
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Table 2:

Similar to Table 1, but with a more efficient convective energy transport in the deeper layers, as explained in the text.
$T_{\rm eff}$ $\log M_{\rm cvz}/M$ $\log P $ $\log T$ $\log \rho$
6000. -7.564 14.516 5.916 0.398
7000. -8.376 13.703 5.769 -0.256
8000. -8.876 13.202 5.691 -0.673
9000. -9.429 12.649 5.602 -1.140
9500. -9.803 12.275 5.536 -1.448
10 000. -10.328 11.749 5.437 -1.877
10 500. -11.040 11.037 5.303 -2.457
11 000. -11.945 10.132 5.135 -3.198
11 100. -12.151 9.926 5.097 -3.367
11 200. -12.364 9.712 5.058 -3.543
11 300. -12.587 9.490 5.019 -3.727
11 400. -12.819 9.258 4.978 -3.919
11 500. -13.058 9.018 4.936 -4.118
11 600. -13.301 8.775 4.895 -4.320
11 700. -13.544 8.532 4.853 -4.522
11 800. -13.806 8.270 4.809 -4.743
11 900. -13.996 8.080 4.777 -4.902
12 000. -14.229 7.847 4.738 -5.097
12 500. -15.555 6.521 4.437 -6.122
13 000. -16.070 6.006 4.326 -6.521

For $T_{\rm eff}$ > 13 000 K the entries are identical with Table 1 and are not repeated here.


Source LaTeX | All tables | In the text

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