Abstract

White dwarfs (WDs) with carbon absorption features in their optical spectra are known as DQ WDs. The subclass of peculiar DQ WDs are cool objects ( -->Teff 6000 K) that show molecular absorption bands that have centroid wavelengths ~100-300 A shortward of the bandheads of the C -->2 Swan bands. These peculiar DQ bands have been attributed to a hydrocarbon such as C -->2H. We point out that C -->2H does not show strong absorption bands with wavelengths matching those of the peculiar DQ bands, and neither does any other simple molecule or ion likely to be present in a cool WD atmosphere. C -->2 seems to be the only reasonable candidate for producing the peculiar DQ bands. Many characteristics of those bands can be understood if they are pressure-shifted Swan bands. While current models of WD atmospheres suggest that, in general, peculiar DQ WDs do not have higher photospheric pressures than normal DQ WDs do, that finding requires confirmation by improved models of WD atmospheres and of the behavior of C -->2 at high pressures and temperatures. If it is eventually shown that the peculiar DQ bands cannot be explained as pressure-shifted Swan bands, the only explanation remaining would seem to be that they arise from highly rotationally excited C -->2 ( -->Jpeak 45). In either case, the absorption band profiles can in principle be used to constrain the pressure and the rotational temperature of C -->2 in the line-forming regions of normal and peculiar DQ WD atmospheres, which will be useful for comparison with models. Finally, we note that progress in understanding magnetic DQ WDs may require models that simultaneously consider magnetic fields, high pressures, and rotational excitation of C -->2.

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