Table 1
Observed and derived quantities.
| Source | l, b | Sν | R<a | AKb | N(H I)0c | N(H I)τd | 2N(H2)e | N(H) | fH2f | N(H)/AK |
|---|---|---|---|---|---|---|---|---|---|---|
| °,° | Jy | kpc | mag | 1022 cm−2 | 1022 cm−2 | 1022 cm−2 | 1022 cm−2 | 1022 cm−2 mag−1 | ||
| J1713-3418 | 351.705, +2.787 | 0.93 | 1.23 | 0.40 | 0.43 | (0.64)g | 0.18 | (0.82) | (0.22) | >1.53 |
| J1717-3341 | 352.733, +2.391 | 0.49 | 1.08 | 0.66 | 0.54 | 0.78 | 0.53 | 1.31 | 0.40 | 1.98 |
| J1733-3722 | 351.818, −2.889 | 0.60 | 1.21 | 0.60 | 0.56 | (1.13) | 0.11 | (1.24) | (0.09) | >1.12 |
| J1744-3116 | 357.863, −0.997 | 0.33 | 0.32 | 1.46 | 0.90 | 1.20 | 1.93 | 3.13 | 0.62 | 2.14 |
Notes. (a) R< = R0 sin(|l|), R0 = 8500 pc. (b) Values from Schultheis et al. (2014); E(B − V)/AK = 3.09 (Schlafly & Finkbeiner 2011). (c) N(H I)0 = 1.823 × 1018 cm−2 ∫ TB(v)dv. (d) N(H I)τ from Eq. (1). (e) N(H2) = N(HCO+)/3 × 10−9, N(HCO+) = 1.10 × 1012Cm−2 ∫ τHCO+ dv (f) fH2 = 2N(H2)/(N(H I) + 2N(H2)). (h) Parenthesized quantities assume N(H)/AK = 2.06 × 1022 cm−2 mag−1, the average for J1717 and J1744.
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