30.08.2014 Views

Observational Constraints on The Evolution of Dust in ...

Observational Constraints on The Evolution of Dust in ...

Observational Constraints on The Evolution of Dust in ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

140 From Protoplanetary Disks to Planetary Systems<br />

Figure 6.6 – Distributi<strong>on</strong> <strong>of</strong> crystall<strong>in</strong>e fracti<strong>on</strong>s for Serpens (top), Taurus (middle), and Upper<br />

Sco and η Cha comb<strong>in</strong>ed (bottom). Similar distributi<strong>on</strong>s and the same range <strong>of</strong> fracti<strong>on</strong>s are seen<br />

for all clusters. (A color versi<strong>on</strong> <strong>of</strong> this figure is available <strong>in</strong> the <strong>on</strong>l<strong>in</strong>e journal)<br />

for the warm comp<strong>on</strong>ent (Figure 6.6), which is reflected <strong>in</strong> the mean crystall<strong>in</strong>ity<br />

fracti<strong>on</strong>s for each sample (Table 6.3). This discrepancy could be real, or an artifact<br />

due to the signal-to-noise ratio (S/N) be<strong>in</strong>g frequently lower at l<strong>on</strong>ger wavelengths<br />

(cold comp<strong>on</strong>ent) than that at shorter wavelengths (warm comp<strong>on</strong>ent), <strong>in</strong>troduc<strong>in</strong>g<br />

a larger scatter. <strong>The</strong> difference <strong>in</strong> Serpens is more significant (〈C warm 〉 ≃ 11.0%<br />

and 〈C cold 〉 ≃ 17.5%). <strong>The</strong> left panel <strong>of</strong> Figure 6.7 shows the cumulative fracti<strong>on</strong>s<br />

as functi<strong>on</strong>s <strong>of</strong> crystall<strong>in</strong>ity fracti<strong>on</strong>s. Despite small differences between the warm<br />

(red l<strong>in</strong>e) and cold (blue l<strong>in</strong>e) comp<strong>on</strong>ents, the two cumulative fracti<strong>on</strong>s have similar<br />

behavior. If this difference is true, there is a small fracti<strong>on</strong> <strong>of</strong> T Tauri disks with a<br />

higher cold (outer) than warm (<strong>in</strong>ner) crystall<strong>in</strong>ity fracti<strong>on</strong>. This f<strong>in</strong>d<strong>in</strong>g c<strong>on</strong>trasts<br />

with that derived by van Boekel et al. (2004) for the disks around 3 Herbig stars.<br />

<strong>The</strong>ir spatially resolved observati<strong>on</strong>s <strong>in</strong>fer higher crystall<strong>in</strong>ity fracti<strong>on</strong>s <strong>in</strong> the <strong>in</strong>ner<br />

than <strong>in</strong> the outer disks, albeit based <strong>on</strong> <strong>on</strong>ly 10 µm data. A larger sample <strong>of</strong> objects<br />

with good S/N <strong>in</strong>clud<strong>in</strong>g both 10 and 20 µm data is needed to better c<strong>on</strong>stra<strong>in</strong> this<br />

po<strong>in</strong>t. In additi<strong>on</strong>, Figure 6.6 shows that younger and older clusters have similar<br />

distributi<strong>on</strong>s <strong>of</strong> crystall<strong>in</strong>ity fracti<strong>on</strong>s.<br />

As discussed by many authors, both the gra<strong>in</strong> size and the degree <strong>of</strong> crystall<strong>in</strong>ity<br />

affect the silicate features, therefore it is <strong>in</strong>terest<strong>in</strong>g to search for trends between<br />

these two parameters. In Figure 6.8, the mass-average gra<strong>in</strong> sizes are compared to the<br />

crystall<strong>in</strong>ity fracti<strong>on</strong> for both warm (left panel) and cold (right panel) comp<strong>on</strong>ents. No<br />

obvious trends are seen <strong>in</strong> either comp<strong>on</strong>ent, neither any separati<strong>on</strong> between regi<strong>on</strong>s.<br />

This result supports the discussi<strong>on</strong> <strong>of</strong> Ol<strong>of</strong>ss<strong>on</strong> et al. (2010) that whatever processes

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!