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Observational Constraints on The Evolution of Dust in ...

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14 Introducti<strong>on</strong><br />

Figure 1.4 – Evidence <strong>of</strong> gra<strong>in</strong> growth <strong>in</strong> the Si–O stretch<strong>in</strong>g and O–Si–O bend<strong>in</strong>g mode features.<br />

<strong>The</strong> top panels show the observed normalized spectra <strong>in</strong> the (a) 10 µm and (b) 20 µm regi<strong>on</strong>s for<br />

sub-samples <strong>of</strong> our sources. <strong>The</strong> bottom two panels show the normalized absorpti<strong>on</strong> efficiencies<br />

(Q abs ) for models <strong>of</strong> spherical gra<strong>in</strong>s <strong>of</strong> amorphous oliv<strong>in</strong>es with various gra<strong>in</strong> sizes calculated for<br />

the 10 and 20 µm regi<strong>on</strong>s. Models <strong>of</strong> filled homogeneous spheres calculated us<strong>in</strong>g Mie theory are<br />

shown <strong>in</strong> (c) and (d), and models <strong>of</strong> hollow spheres calculated us<strong>in</strong>g distributi<strong>on</strong> <strong>of</strong> hollow spheres<br />

(DHS) theory are shown <strong>in</strong> (e) and (f) (Kessler-Silacci et al. 2006).<br />

have been proposed to expla<strong>in</strong> this formati<strong>on</strong> <strong>of</strong> crystal gra<strong>in</strong>s: thermal anneal<strong>in</strong>g <strong>of</strong><br />

amorphous gra<strong>in</strong>s or vaporizati<strong>on</strong> followed by gas-phase c<strong>on</strong>densati<strong>on</strong>. Both methods<br />

require high temperatures (above ∼1000 K, Fabian et al. 2000; Gail 2004), mean<strong>in</strong>g<br />

that either method could work <strong>in</strong> the <strong>in</strong>ner parts <strong>of</strong> disks, where temperatures are<br />

high enough. Yet, observati<strong>on</strong>s show crystall<strong>in</strong>e gra<strong>in</strong>s over the entire extent <strong>of</strong> disk<br />

surfaces covered by IR observati<strong>on</strong>s (van Boekel et al. 2004). Large-scale radial mix<strong>in</strong>g<br />

has been <strong>in</strong>voked to expla<strong>in</strong> the presence <strong>of</strong> crystals at low temperatures <strong>in</strong> the<br />

outer disk (Bockelée-Morvan et al. 2000; Gail 2004; Ciesla 2009). A third proposed<br />

formati<strong>on</strong> mechanism for crystal formati<strong>on</strong> is that <strong>of</strong> shock waves, which could locally<br />

heat amorphous silicates and crystallize them (Desch & C<strong>on</strong>nolly 2002; Harker<br />

& Desch 2002).<br />

M<strong>in</strong>eralogical studies <strong>of</strong> Solar System bodies show a range <strong>of</strong> crystall<strong>in</strong>ity fracti<strong>on</strong>s.<br />

Evidence from primitive ch<strong>on</strong>drites shows that the abundance <strong>of</strong> crystall<strong>in</strong>e<br />

silicate material varies from nearly noth<strong>in</strong>g to up to 20 – 30 % (e.g. Acfer 094 and<br />

ALH77307, P<strong>on</strong>toppidan & Brearley 2010 and references there<strong>in</strong>). Oort cloud comets,<br />

with l<strong>on</strong>g periods and large distances from the Sun, have <strong>in</strong>ferred crystall<strong>in</strong>ity fracti<strong>on</strong>s<br />

up to 60 – 80 % (e.g. Hale-Bopp, Wooden et al. 1999, 2007). Jupiter-family, or

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