High-spatial-resolution imaging of thermal emission from debris disks

Details High-spatial-resolution imaging of thermal emission from debris disks High-spatial-resolution imaging of thermal emission from debris disks

2010-11-05

arxiv.org/abs/1011.1410v2

The Astrophysical Journal, Volume 723, Issue 2, pp. 1418-1435 (2010)

Astronomy and Astrophysics

Astrophysics

Solar and Stellar Astrophysics

46 pages, 12 figures

Scientific paper

10.1088/0004-637X/723/2/1418

We have obtained sub-arcsec mid-IR images of a sample of debris disks within 100 pc. For our sample of nineteen A-type debris disk candidates chosen for their IR excess, we have resolved, for the first time, five sources plus the previously resolved disk around HD 141569. Two other sources in our sample have been ruled out as debris disks since the time of sample selection. Three of the six resolved sources have inferred radii of 1-4 AU (HD 38678, HD 71155, and HD 181869), and one source has an inferred radius ~10-30 AU (HD 141569). Among the resolved sources with detections of excess IR emission, HD 71155 appears to be comparable in size (r~2 AU) to the solar system's asteroid belt, thus joining Zeta Lep (HD 38678, reported previously) to comprise the only two resolved sources of that class. Two additional sources (HD 95418 and HD 139006) show spatial extent that implies disk radii of ~1-3 AU, although the excess IR fluxes are not formally detected with better than 2-sigma significance. For the unresolved sources, the upper limits on the maximum radii of mid-IR disk emission are in the range ~1-20 AU, four of which are comparable in radius to the asteroid belt. We have compared the global color temperatures of the dust to that expected for the dust in radiative equilibrium at the distances corresponding to the observed sizes or limits on the sizes. In most cases, the temperatures estimated via these two methods are comparable, and therefore, we see a generally consistent picture of the inferred morphology and the global mid-IR emission. Finally, while our sample size is not statistically significant, we notice that the older sources (>200 Myr) host much warmer dust (T > 400 K) than younger sources (in the 10s of Myr).

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