Carbon and oxygen isotopic ratios are reported for a sample of 51 SRb-and Lb-type variable asymptotic giant branch stars. Vibration-rotation first-and second-overtone CO lines in 1.5 to 2.5 µm spectra were measured to derive isotopic ratios for 12 C/ 13 C, 16 O/ 17 O, and 16 O/ 18 O. Comparisons with previous measurements for individual stars and with various samples of evolved stars, as available in the extant literature, are discussed. Using the oxygen isotopic ratios, the masses of the SRb stars can be derived. Combining the masses with Gaia luminosities, the SRb stars are shown to be antecedents of the Mira variables. The limiting parameters where plane-parallel, hydrostatic equilibrium model atmospheres can be used for abundance analysis of M giants are explored.
Lebzelter et al.This is our second Paper In a series to study the isotopic ratios of C and O in AGB stars. In the first paper of this series (Hinkle et al. 2016, Paper I) we presented an extensive discussion on the influence of stellar parameters and evolution on the isotopic ratios of these two key elements measured at the stellar surface. Here we confine the discussion to a brief summary of the main effects and refer to Paper I (note in particular Figure 10), Lebzelter et al. (2015a), and references therein for a more extensive description.The CNO cycle depletes 12 C and enhances 13 C, a change that becomes visible as a steep drop in the 12 C/ 13 C ratio down to 10 to 25 after the first dredge up. A slight dependence of the resulting ratios on stellar mass is expected, with the more massive stars showing higher 12 C/ 13 C values (Paper I). Extensive observational evidence (e.g. Charbonnel et al. 1999) exists that extra-mixing along the red giant branch (RGB) can further reduce the ratio between the two carbon isotopes by a factor of two in low-mass stars. The interplay between production, mixing, and destruction of the various oxygen isotopes results in a dependence of 16 O/ 17 O on stellar mass (Boothroyd et al, 1994;El Eid 1994;Karakas & Lattanzio 2014), with the istopic ratio decreasing with increasing mass as different depths and thus different regions of 17 O enhancement are reached by the first dredge-up. 18 O, on the other hand, is depleted by H burning and therefore 16 O/ 18 O is increasing with the first dredge-up. This effect, however, is almost independent of mass.The second dredge-up has only a mild effect on the isotopic ratios on the surface. With the third dredge-up episodes, which are predicted to occur in stars with main-sequence masses between approximately 1.3 and 5 M at solar metallicity, 12 C/ 13 C is strongly enhanced, while there is little effect on the oxygen isotopic ratios. In the more massive AGB stars, Hot Bottom Burning (HBB) can effect the oxygen isotopes, in particular the abundance of 18 O which is significantly depleted (Lattanzio et al. 1996). As pointed out by Lebzelter et al. (2015a), the 16 O/ 18 O is good indicator of the primordial 18 O abundance in a star, so that star-to-star variations of this ratio also ...