1201.1504 (Jonathan J. Fortney)
Jonathan J. Fortney
Recent high resolution spectroscopic analysis of nearby FGK stars suggests
that a high C/O ratio of greater than 0.8, or even 1.0, is relatively common.
Two published catalogs of measurements find C/O>0.8 in 25-30% of systems, and
C/O>1.0 in ~6-10% of systems. It has been suggested that in protoplanetary
disks with C/O>0.8 that the condensation pathways to refractory planet-making
material will differ from what occurred in our solar system, where C/O=0.55.
The carbon-rich disks are calculated to make carbon-dominated rocky planets,
rather than oxygen-dominated ones, which would be very unlike the Earth. Here
we suggest that the derived stellar C/O ratios are overestimated, given the
extreme paucity of carbon dwarfs stars (<0.1%) found in large samples of low
mass stars, such as from the Sloan Digital Sky Survey. The reason for this
overestimation is not immediately apparent, but could be due to the choices of
lines used, or limitations of abundance analysis from one-dimensional LTE
stellar atmosphere models. Furthermore, from the estimated errors on the
measured stellar C/O ratios, we find that the significance of the high C/O tail
is weakened, with a true measured fraction of C/O>0.8 in 10-15% of stars, and
C/O>1.0 in 1-5%, athough these are still likely overestimates. We suggest that
infrared T-dwarf spectra could show how common high C/O is in the stellar
neighborhood, as the chemistry and spectra of such objects would differ
compared to those with solar-like abundances. We expect that carbon-dominated
rocky planets are rarer than others have suggested.
View original:
http://arxiv.org/abs/1201.1504
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