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Table 4

Observations and model results for fractional abundances at 105 yr.

Species IR-edge IR-peak Cloud
Obs. Mod. Obs. Mod. Obs. Mod.

O (10-5) 11 7.3 5.9
N (10-6) 16 1.1 1.3
CN (10-8) 2.3 1.0 0.2
NO (10-9) 0.07 77 103
O2(10-7)  <0.01 7.2 62
OH (10-7) 0.01 1.8 1.3
CO(10-5) 6.0 9.6 9.9
H2O(10-9) 0.4 170 193
C2H(10-8) 3.3 1.6 3.0 0.3 0.2 0.07
c-C3H(10-10) 1.9 5.4 0.6 1.4
l-C3H(10-10) 1.0 2.9 8.0 0.9
c-C3H2(10-10) 13 2.3 11 10 0.4 2.3
C4H(10-9) 9.5 1.3 3.6 2.0 0.8 0.1
CH4(10-9) 0.03 33 50
C6H(10-11) 1.4 4.1 0.2
HCO(10-10) 0.03 17a 0.1 0.2
NH3(10-8)  <0.01 1.2 2.5
HCN(10-10) 0.8 40 26
HNC(10-10) 0.9 67 17
HC3N(10-11)  <0.01 5.7b 0.7 0.3
HC5N(10-12)  <0.01 4 0.13
CH+(10-12) 5 0.02  <0.01
CO+(10-13)  ≤5c 20 3.2 1.3
HCO+(10-9) 0.9d 0.02 10 3.9d 11
HOC+(10-12) 4e 6 73 27
OH+(10-13) 4 15 5
H2O+(10-13) 8 33 12
H3O+(10-10) 0.1 45 37
23 10 0.2
1.5 19 12
CS(10-8) 1.6f 0.04 4.0f 0.04 0.01
HCS+(10-11) 0.07 4.0g 0.08 0.1

Notes. The IR-edge is at AV = 1.56 ± 0.73, the IR-peak is at AV = 4.55 ± 1.7 and the Cloud region is at AV = 11.7 ± 4.1. The model results are for the high column-dependent ζ from Fig. 2. Observations are from Pety et al. (2005) unless otherwise noted.

(a)

HCO at AV ≈ 4 by Gerin et al. (2009).

(b)

HC3N observed at AV ≈ 4 by Teyssier et al. (2004).

(c)

Upper limit at AV < 2, from Goicoechea et al. (2009b).

(d)

HCO+ from H13CO+ at AV ≈ 2 and AV ≈ 10 by Gerin et al. (2009). The calculated abundance at AV = 3 is in close agreement with the observed edge value.

(e)

Observed at AV ≈ 2 by Goicoechea et al. (2009b).

(f)

For the IR-peak and IR-edge, from Teyssier et al. (2004).

(g)

HCS+ observed at AV ≈ 4 by Goicoechea et al. (2006).

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