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Observational Constraints on The Evolution of Dust in ...

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88 Spitzer Survey <strong>of</strong> Protoplanetary Disk <strong>Dust</strong> <strong>in</strong> Serpens<br />

additi<strong>on</strong>, the objects with PAH emissi<strong>on</strong> have standard F 30 /F 13 flux ratios, fall<strong>in</strong>g <strong>in</strong><br />

the ‘flat’ and ‘flared’ regi<strong>on</strong>s <strong>of</strong> Figure 4.3.<br />

Only object 120 shows a silicate feature (at 20 µm, as discussed <strong>in</strong> Secti<strong>on</strong> 4.3.3.3),<br />

<strong>in</strong> additi<strong>on</strong> to PAHs. This alludes to an anti-correlati<strong>on</strong> between PAHs and silicates<br />

that could be simply expla<strong>in</strong>ed <strong>in</strong> terms <strong>of</strong> c<strong>on</strong>trast, i.e., it is hard to detect PAH<br />

features when a str<strong>on</strong>g 10 µm silicate feature is present (Geers et al. 2006). In this<br />

sense, PAHs should be more easily detected <strong>in</strong> disks without silicates, s<strong>in</strong>ce the fall<strong>in</strong>g<br />

spectrum provides an <strong>in</strong>crease <strong>in</strong> the feature to c<strong>on</strong>t<strong>in</strong>uum ratio improv<strong>in</strong>g c<strong>on</strong>trast.<br />

4.3.3.3 Silicate Emissi<strong>on</strong><br />

Silicate emissi<strong>on</strong> has been observed around numerous circumstellar disks (e.g., van<br />

Boekel et al. 2003; Przygodda et al. 2003; Kessler-Silacci et al. 2006; Furlan et al.<br />

2006; Bouwman et al. 2008; Ol<strong>of</strong>ss<strong>on</strong> et al. 2009). Some <strong>of</strong> this material has different<br />

characteristics <strong>in</strong> disks compared to primitive <strong>in</strong>terstellar material. <strong>The</strong> strength and<br />

the shape <strong>of</strong> silicate features (at 10 and 20 µm) c<strong>on</strong>ta<strong>in</strong> important <strong>in</strong>formati<strong>on</strong> <strong>on</strong><br />

the dust sizes <strong>in</strong> the surface layer <strong>of</strong> the disk. <strong>The</strong> 89 disk sources <strong>in</strong> this sample<br />

were <strong>in</strong>spected for their silicate characteristics. <strong>The</strong>ir spectra can be seen <strong>in</strong> Figures<br />

4.6–4.8 (completed with Figures 4.4 and 4.5), arranged <strong>in</strong> order <strong>of</strong> decreas<strong>in</strong>g strength<br />

<strong>of</strong> the 10 µm feature and decreas<strong>in</strong>g α 2−24µm spectral slope. No ext<strong>in</strong>cti<strong>on</strong> correcti<strong>on</strong><br />

has been applied to these spectra (see Secti<strong>on</strong> 4.3.3.5).<br />

Five <strong>of</strong> these sources (5% <strong>of</strong> the disk populati<strong>on</strong>) have spectra that are featureless,<br />

i.e., they have neither the 10 nor the 20 µm silicate features <strong>in</strong> emissi<strong>on</strong>, although they<br />

present IR excess (objects 38, 42, 59, 83, and 87). It is found that when the 10 µm<br />

feature appears, the 20 µm band is also present (by visual <strong>in</strong>specti<strong>on</strong> <strong>of</strong> the c<strong>on</strong>t<strong>in</strong>uumsubtracted<br />

spectra, see Secti<strong>on</strong> 4.3.3.4). <strong>The</strong> c<strong>on</strong>trary is not true, as objects 13, 20,<br />

24, 32, 62, 64, 69, 70, 109, 116, 127, 139, 143 and 145 have an observed 20 µm feature<br />

but no apparent 10 µm feature (also reported by Kessler-Silacci et al. (2006) for T<br />

Cha, SR21 and HD 135344B). Also, object 120 shows the 20 µm band and no 10<br />

µm feature, as this regi<strong>on</strong> is dom<strong>in</strong>ated by PAH features <strong>in</strong> this source (see Secti<strong>on</strong><br />

4.3.3.2). When present, the 10 µm feature (S 10µm<br />

peak<br />

µm (S 20µm<br />

peak<br />

) <strong>on</strong>e as is comm<strong>on</strong> <strong>in</strong> disk sources.<br />

) is usually str<strong>on</strong>ger than the 20<br />

Crystall<strong>in</strong>e silicate features (as discussed by, e.g., Bouwman et al. 2001, 2008;<br />

Acke & van den Ancker 2004; van Boekel et al. 2004; Apai et al. 2005; Ol<strong>of</strong>ss<strong>on</strong> et al.<br />

2009; Sargent et al. 2009) are seen <strong>in</strong> several sources. A detailed analysis <strong>in</strong> terms <strong>of</strong><br />

statistics and crystall<strong>in</strong>e fracti<strong>on</strong> <strong>of</strong> these features is n<strong>on</strong>-trivial and bey<strong>on</strong>d the scope<br />

<strong>of</strong> this paper, but will be subject <strong>of</strong> a future publicati<strong>on</strong>.<br />

4.3.3.4 <strong>The</strong> Silicate Strength-Shape Relati<strong>on</strong><br />

As first shown for Herbig Ae stars (van Boekel et al. 2003), there is a dependence<br />

between gra<strong>in</strong> size and silicate shape and strength for both 10 and 20 µm features:<br />

as the sizes <strong>of</strong> the gra<strong>in</strong>s grow, the silicate features appear more and more flattened

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