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A. Relative Abundances <strong>of</strong> Species 153<br />

A. Relative Abundances <strong>of</strong> Species<br />

<strong>The</strong> relative abundances, as result<strong>in</strong>g from the B2C compositi<strong>on</strong>al fitt<strong>in</strong>g (§ 6.3) to<br />

the IRS spectra <strong>of</strong> protoplanetary disks <strong>in</strong> Serpens, Taurus, Upper Sco and η Cha are<br />

shown <strong>in</strong> Tables A.1 and A.2. S<strong>in</strong>ce the opacities <strong>of</strong> amorphous oliv<strong>in</strong>e and pyroxene<br />

are degenerate, the abundances <strong>of</strong> these two species have been added <strong>in</strong>to <strong>on</strong>e, marked<br />

‘Oli/Pyr’ <strong>in</strong> the Tables. Furthermore, ‘Sil’ designates the amorphous silica, and the<br />

crystall<strong>in</strong>e enstatite and forsterite are marked as ‘Ens’ and ‘For’, respectively. In<br />

the tables, the first l<strong>in</strong>e <strong>of</strong> a given object corresp<strong>on</strong>ds to the results <strong>of</strong> the fit to the<br />

warm comp<strong>on</strong>ent and the sec<strong>on</strong>d l<strong>in</strong>e to the results <strong>of</strong> the cold comp<strong>on</strong>ent. For some<br />

objects (20 <strong>in</strong> Serpens, 28 <strong>in</strong> Taurus, all <strong>in</strong> Upper Sco and η Cha), the S/N drops<br />

c<strong>on</strong>siderably at l<strong>on</strong>ger wavelengths and the results <strong>of</strong> the procedure are no l<strong>on</strong>ger<br />

reliable. For these sources, the cold comp<strong>on</strong>ent could not be fitted satisfactorily and,<br />

<strong>in</strong> Tables A.1 and A.2, <strong>on</strong>ly the warm comp<strong>on</strong>ent results are shown.<br />

ID SpT Oli/Pyr a % Ens % For % Sil %<br />

(0.1 µm) (0.1 µm) (0.1 µm) (0.1 µm)<br />

Serpens<br />

1 K2 29.7 +10.7<br />

−15.3 1.0 +2.0<br />

−0.4 2.6 +2.6<br />

−1.4 0.1 +0.9<br />

−0.0<br />

· · · 38.4 +14.5<br />

−15.8 0.0 +1.6<br />

−0.0 8.7 +5.5<br />

−3.6 1.2 +3.0<br />

−0.0<br />

3 M0 26.5 +15.9<br />

−7.3 0.0 +2.4<br />

−0.0 0.9 +3.5<br />

−0.4 0.0 +1.7<br />

−0.0<br />

· · · 27.3 +33.7<br />

−8.6 0.0 +10.5<br />

−0.0 10.2 +19.1<br />

−4.9 0.0 +16.3<br />

−4.0<br />

6 K5 25.4 +4.5<br />

−6.0 0.0 +0.7<br />

−0.0 0.8 +1.1<br />

−0.0 0.0 +0.3<br />

−0.0<br />

· · · 6.4 +3.8<br />

−3.3 4.1 +2.1<br />

−2.3 5.1 +3.4<br />

−0.0 0.5 +1.1<br />

−0.0<br />

7 M0 3.7 +3.1<br />

−0.9 0.0 +2.9<br />

−0.0 0.8 +4.3<br />

−0.0 0.0 +0.9<br />

−0.0<br />

· · · 0.0 +3.4<br />

−0.5 7.2 +4.9<br />

−6.9 8.1 +5.3<br />

−6.9 14.1 +8.3<br />

−11.5<br />

9 – 58.3 +10.9<br />

−8.8 0.0 +1.4<br />

−0.0 0.5 +1.1<br />

−0.0 0.0 +0.7<br />

−0.0<br />

· · · 24.5 +16.3<br />

−14.5 0.0 +3.5<br />

−0.0 14.4 +13.9<br />

−9.8 16.9 +24.0<br />

−15.0<br />

10 – 1.9 +5.9<br />

−0.6 0.0 +2.5<br />

−0.0 2.3 +2.1<br />

−0.7 4.3 +2.4<br />

−1.4<br />

· · · 37.4 +29.1<br />

−9.4 2.0 +10.1<br />

−0.0 0.0 +9.2<br />

−0.0 0.0 +19.4<br />

−0.0<br />

14 M2 11.1 +46.8<br />

−0.0 0.0 +6.0<br />

−0.0 3.0 +7.1<br />

−0.0 0.0 +6.9<br />

−0.0<br />

15 – 35.6 +12.5<br />

−7.0 0.2 +1.5<br />

−0.0 2.9 +1.6<br />

−1.3 0.0 +0.6<br />

−0.0<br />

· · · 36.3 +10.4<br />

−12.9 2.4 +1.8<br />

−1.6 2.2 +3.5<br />

−1.0 1.1 +2.8<br />

−0.9<br />

21 – 2.2 +5.0<br />

−0.0 0.0 +1.6<br />

−0.0 2.7 +3.7<br />

−0.0 0.1 +3.6<br />

−0.0<br />

· · · 33.0 +18.1<br />

−20.7 1.6 +5.2<br />

−0.0 0.0 +2.3<br />

−0.0 1.3 +11.9<br />

−0.0<br />

29 M2 1.4 +6.4<br />

−0.0 0.0 +3.1<br />

−0.0 1.6 +7.8<br />

−0.0 2.7 +6.6<br />

−0.3<br />

30 M1 0.0 +9.7<br />

−0.0 0.1 +4.4<br />

−0.0 3.4 +4.6<br />

−1.2 4.5 +6.8<br />

−0.2<br />

· · · 10.3 +51.7<br />

−13.8 1.7 +15.4<br />

−3.2 5.5 +14.1<br />

−4.3 8.1 +21.6<br />

−6.3<br />

31 – 1.2 +0.8<br />

−0.0 0.0 +0.8<br />

−0.0 0.8 +0.5<br />

−0.0 0.0 +1.0<br />

−0.0<br />

· · · 21.8 +5.3<br />

−4.9 2.4 +1.6<br />

−0.0 0.0 +0.7<br />

−0.0 16.7 +8.7<br />

−7.9<br />

36 K5 22.3 +5.2<br />

−6.2 0.9 +1.6<br />

−0.0 0.6 +1.3<br />

−0.0 0.0 +0.8<br />

−0.0<br />

· · · 37.4 +11.0<br />

−15.4 0.0 +3.9<br />

−0.0 1.6 +2.7<br />

−1.0 2.9 +8.6<br />

−2.5

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