Infrared extinction maps and submillimeter dust continuum maps are powerful probes of the density structure in the envelope of star-forming cores. We make a direct comparison between infrared and submillimeter dust continuum observations of the low-mass Class 0 core, B335, to constrain the ratio of submillimeter to infrared opacity (úsmm/úir) and the submillimeter opacity power-law index (ú vprop û-ò). Using the average value of theoretical dust opacity models at 2.2 üm, we constrain the dust opacity at 850 and 450 üm. Using new dust continuum models based upon the broken power-law density structure derived from interferometric observations of B335 and the infall model derived from molecular line observations of B335, we find that the opacity ratios are \{\κ ₈₅₀}{\κ 2.2} = (3.21{--}4.80)+0.44-0.30 \× 10⁻⁴ and \{\κ ₄₅₀}{\κ 2.2} = (12.8{--}24.8)+2.4-1.3 \× 10⁻⁴with a submillimeter opacity power-law index of òsmm = (2.18-2.58)+0.30 -0.30. The range of quoted values is determined from the uncertainty in the physical model for B335. For an average 2.2 üm opacity of 3800 ñ 700 cm2 g-1, we find a dust opacity at 850 and 450 üm of ú850 = (1.18-1.77)+0.36 -0.24 and ú450 = (4.72-9.13)+1.9 -0.98 cm2 g-1 of dust. These opacities are from (0.65-0.97)úOH5 850 of the widely used theoretical opacities of Ossenkopf and Henning for coagulated ice grains with thin mantles at 850 üm.
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Shirley et al. (2011) studied this question.
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