Observational Constraints on The Evolution of Dust in ...
Observational Constraints on The Evolution of Dust in ...
Observational Constraints on The Evolution of Dust in ...
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90 Spitzer Survey <strong>of</strong> Protoplanetary Disk <strong>Dust</strong> <strong>in</strong> Serpens<br />
Figure 4.7 – IRS spectra <strong>of</strong> the disk sources <strong>in</strong> Serpens, c<strong>on</strong>td.<br />
are <strong>in</strong>deed tracers <strong>of</strong> gra<strong>in</strong> size. <strong>The</strong> relati<strong>on</strong>ship is much tighter for the 10 µm feature,<br />
as also seen by the great spread <strong>in</strong> the correlati<strong>on</strong> for the 20 µm feature.<br />
Follow<strong>in</strong>g their procedure, we first subtracted the c<strong>on</strong>t<strong>in</strong>uum <strong>of</strong> each spectrum by<br />
fitt<strong>in</strong>g a sec<strong>on</strong>d-order polynomial to the follow<strong>in</strong>g regi<strong>on</strong>s: blueward <strong>of</strong> the 10 µm<br />
feature, between the 10 and the 20 µm features, and redward <strong>of</strong> the 20 µm feature<br />
(6.8–7.5, 12.5–13.5 and 30–36 µm). <strong>The</strong> peak fluxes at 9.8, 10, 11.3, 19, 20, and 23.8<br />
µm were then determ<strong>in</strong>ed (see Table 4.2). Figure 4.9 shows the results for our sample<br />
<strong>of</strong> disks, exclud<strong>in</strong>g those with PAH emissi<strong>on</strong>. <strong>The</strong> best fit found by Kessler-Silacci et<br />
al. (2006) for the c2d IRS first look sample <strong>of</strong> YSOs has been <strong>in</strong>dicated for comparis<strong>on</strong><br />
(solid l<strong>in</strong>e). <strong>The</strong> agreement <strong>of</strong> the Serpens data with the best fit <strong>of</strong> Kessler-Silacci et<br />
al. (2006) is excellent, and more evident for the 10 µm than for the 20 µm feature<br />
due to the larger scatter <strong>in</strong> the latter group.<br />
Ol<strong>of</strong>ss<strong>on</strong> et al. (2009) generated synthetic 10 µm features calculated for different<br />
gra<strong>in</strong> sizes and compositi<strong>on</strong>s. <strong>The</strong>ir models are generated for amorphous silicates<br />
<strong>of</strong> oliv<strong>in</strong>e and pyroxene stoichiometry and a 50:50 mixture, with gra<strong>in</strong> size vary<strong>in</strong>g