THE OPACITY MECHANISM IN B-TYPE STARS .2. EXCITATION OF HIGH-ORDER G-MODES IN MAIN-SEQUENCE STARS

Citation
Wa. Dziembowski et al., THE OPACITY MECHANISM IN B-TYPE STARS .2. EXCITATION OF HIGH-ORDER G-MODES IN MAIN-SEQUENCE STARS, Monthly Notices of the Royal Astronomical Society, 265(3), 1993, pp. 588-600
Citations number
50
Categorie Soggetti
Astronomy & Astrophysics
ISSN journal
00358711
Volume
265
Issue
3
Year of publication
1993
Pages
588 - 600
Database
ISI
SICI code
0035-8711(1993)265:3<588:TOMIBS>2.0.ZU;2-B
Abstract
We show that the OPAL opacities, in addition to explaining the origin of the pulsations of beta Cep stars, also predict the existence of a l arge region in the main-sequence band at lower luminosities, where hig h-order g-modes of low harmonic degree l are unstable. The excitation mechanism remains the same, and is due to the usual kappa-effect actin g in the metal opacity bump (T almost-equal-to 2 X 10(5) K). The new i nstability domain nearly bridges the gap in spectral types between del ta Sct and beta Cep stars. The periods of the unstable modes are in th e range 0.4-3.5 d for l = 1 and 2. We propose that this excitation mec hanism causes photometric variability in the slowly pulsating B-type s tars (SPB stars), and perhaps in other B stars for which variability i n the same period range has been reported. Typically, a large number o f modes are simultaneously unstable in one model. Most of them have 1 > 2. Such modes are not likely to be detected photometrically, but may be visible in line profile changes. The excitation of many high-l mod es in a star may also cause a spurious contribution to the rotational v sin i values. Sequences of unstable modes at each value of 1 exhibit a periodically varying departure from equal spacing in period. This f eature, first noted in white dwarf g-mode spectra (calculated and meas ured), is in the present case a probe of the region left behind the sh rinking core (the mu-gradient zone). We discuss prospects for and diff iculties of SPB-star asteroseismology.