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Table 2.

Properties of the components used to model the continuum and the H2O ν2 = 1 − 0 band in IRAS 07251−0248 E.

Component log Lunatta Tdb τ 6 μ m int $ \tau_{\mathrm{6\,{\upmu}m}}^{\mathrm{int}} $c Rd τ 6 μ m fg $ \tau_{6\,{\upmu}\mathrm{m}}^{\mathrm{fg}} $e log Lattf log NH2g XH2Oh log MH2i log Lintj
(L) (K) (pc) (L) (cm−2) (×10−5) (M) (L)
HC 12.0(0.10) ≥200 390(70) 13.2(0.2) 1.16(0.02) 11.4(0.10) 25.3(0.10) 8(2) 8.44(0.10) 11.9 − 12.2
WC 12.3(0.12) 123(4) 98(22) 71(7) 1.16(0.02) 11.9(0.12) 24.6(0.12) 9.13(0.12) 11.7 − 12.1
CCk 12.1(0.12) 45(5) 0 12.1(0.12) 9.57(0.12) 11.5 − 11.8

Notes. (a)Unattenuated luminosity (3 − 1200 μm) assuming isotropic emission. (b)Dust temperature. For the HC, radiative transfer models compute the Td profile as shown in the left insert of Fig. 2, and the lowest Td value is indicated here. (c)Intrinsic optical depth at 6 μm of the component; the full curves for the HC and WC are shown in the right insert of Fig. 2. (d)Radius of the component. (e)Extinction at 6 μm by the foreground layer. (f)Apparent (attenuated) luminosity (3 − 1200 μm) due to foreground extinction. (g)Column density of H2. (h)H2O abundance relative to H2. (i)H2 mass derived from the continuum fit (Appendix C). (j)Plausible ranges for the intrinsic luminosities, which only include the power sources within the physical regions and consider possible departures from isotropic emission (Section 4.1). kThe cold component is assumed to be optically thin in the far-IR, and thus its τ 6 μ m int $ \tau_{\mathrm{6\,{\upmu}m}}^{\mathrm{int}} $ and R cannot be inferred. Estimated uncertainties are given in parenthesis.

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