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The IR Spectral Energy Distribution

Mid-Infrared Imaging of the Einstein Cross QSO

Eric Agol , Stuart Wyithe, Barbara Jones, Omer Blaes, Chris Fluke, PASA, 18 (2), in press.

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Contents Page: Volume 18, Number 2

The IR Spectral Energy Distribution

The surprising fact is that nearly all of the dust in this QSO is at the sublimation temperature, T$\sim$ 1800K. This is indicated by the SED peak at around 2-3 $\mu$m, and sharp decrease towards longer wavelengths (see Agol et al. 2001). There are a handful of other QSOs which show infrared bumps around the same wavelength (Wills 1987); however, in larger samples they appear to be quite rare (Edelson & Malkan 1986, Sanders et al. 1989). The infrared spectrum can be fit with a thin (i.e. dense) shell of dust with the temperature as a function of radius determined by reradiation of the QSO light (which may be absorbed by dust further in). The inner radius, Rin is set by the sublimation temperature, while radius at which an optical depth of 3 is reached is at

Rout = 3 Rin. The covering factor is about $2 \pi$. Extrapolated to longer wavelength, the dust spectrum falls well below the millimeter upper limits (Agol et al. 2001).



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