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arXiv 1012.3488astro-ph.GA
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亚毫米尘埃不透明度的观测限制

Observational Constraints on Submillimeter Dust Opacity

Yancy L. Shirley, Tracy L. Huard, Klaus M. Pontoppidan, David J. Wilner, Amelia M. Stutz, John H. Bieging, Neal J. Evans

摘要:

红外消光图和亚毫米尘埃连续图是探测恒星形成核心包层密度结构的有力工具。我们对低质量0级核心B335的红外和亚毫米尘埃连续观测进行了直接比较,以限制亚毫米与红外不透明度(\kaprat)的比值和亚毫米不透明度幂律指数($κ\propto λ^{-β}$)。利用理论尘埃不透明度模型在2.2 \micron的平均值,我们将尘埃不透明度限制在850和450 \micron。利用由B335的干涉观测得到的破幂律密度结构和由B335的分子谱线观测得到的下落模型,我们发现尘埃的不透明度比为$\frac{κ_{850}}{κ_{2.2}} = (3.21 - 4.80)^{+0.44}_{-0.30} \times 10^{-4}$和$\frac{κ_{450}}{κ_{2.2}} = (12.8 - 24.8)^{+2.4}_{-1.3} \times 10^{-4}$,其亚毫米不透明度指数为$β_{smm} = (2.18 - 2.58)^{+0.30}_{-0.30}$。引用值的范围由B335物理模型的不确定性确定。对于平均2.2 \micron \不透明度的$3800 \pm 700$ cm $^2$ g $^{-1}$,我们发现在850和450 \micron \的$κ_{850} = (1.18 - 1.77)^{+0.36}_{-0.24}$和$κ_{450} = (4.72 - 9.13)^{+1.9}_{-0.98}$ cm $^2$ g $^{-1}$的灰尘不透明度。这些不透明度来自于Ossenkopf和Henning广泛使用的理论不透明度中的$(0.65 - 0.97) κ^{\rm{OH}5}_{850}$,用于850 \micron下具有薄地幔的凝结冰粒。

英文摘要:

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 (\kaprat) and the submillimeter opacity power-law index ($κ\propto λ^{-β}$). Using the average value of theoretical dust opacity models at 2.2 \micron, we constrain the dust opacity at 850 and 450 \micron . 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 $\frac{κ_{850}}{κ_{2.2}} = (3.21 - 4.80)^{+0.44}_{-0.30} \times 10^{-4}$ and $\frac{κ_{450}}{κ_{2.2}} = (12.8 - 24.8)^{+2.4}_{-1.3} \times 10^{-4}$ with a submillimeter opacity power-law index of $β_{smm} = (2.18 - 2.58)^{+0.30}_{-0.30}$. The range of quoted values are determined from the uncertainty in the physical model for B335. For an average 2.2 \micron\ opacity of $3800 \pm 700$ cm$^2$g$^{-1}$, we find a dust opacity at 850 and 450 \micron\ of $κ_{850} = (1.18 - 1.77)^{+0.36}_{-0.24}$ and $κ_{450} = (4.72 - 9.13)^{+1.9}_{-0.98}$ cm$^2$g$^{-1}$ of dust. These opacities are from $(0.65 - 0.97) κ^{\rm{OH}5}_{850}$ of the widely used theoretical opacities of Ossenkopf and Henning for coagulated ice grains with thin mantles at 850\micron.

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