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arXiv 1710.04598astro-ph.GA
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在半透明视线中与普朗克强度和偏振数据相容的尘埃模式

Dust models compatible with Planck intensity and polarization data in translucent lines of sight

V. Guillet, L. Fanciullo, L. Verstraete, F. Boulanger, A. P. Jones, M. -A. Miville-Deschênes, N. Ysard, F. Levrier, M. Alves

摘要:

从普朗克观测的总辐射和偏振辐射分析中推断出的尘埃性质对目前的尘埃模型提出了挑战。我们提出了新的尘埃模型兼容的偏振和非偏振数据消光和发射半透明的视线($0.5 < A_V < 2.5$)。我们修改了DustEM工具,以模拟偏振消光和发射。我们拟合的平均消光,偏振消光,SED和偏振SED与多环芳烃,星状硅酸盐和无定形碳(a-C)的光谱依赖性。星状硅酸盐人口沿磁场线排列,而a-C人口可能是对齐或不对齐。以其目前的光学性质,扁球形星状硅酸盐颗粒的发射率不足以重现普朗克数据得出的发射消光偏振比$P_{353}/p_V$。模型使用长星状硅酸盐颗粒与伸长率$a/b=3$和20%的孔隙度的夹杂物成功。偏振SED的光谱依赖性是陡峭的,在我们的模型比数据。当a-C晶粒对齐时,模型表现稍好。在星形硅酸盐基质中包含小体积(6%)的a-C消除了对孔隙率和完美的晶粒排列的需要,并改善了与极化SED的拟合。基于星状硅酸盐的尘埃模型可以通过调整颗粒的形状和在星状硅酸盐基质中添加孔隙或a-C的夹杂物来与普朗克数据相协调。

英文摘要:

The dust properties inferred from the analysis of Planck observations in total and polarized emission challenge current dust models. We propose new dust models compatible with polarized and unpolarized data in extinction and emission for translucent lines of sight ($0.5 < A_V < 2.5$). We amended the DustEM tool to model polarized extinction and emission. We fit the spectral dependence of the mean extinction, polarized extinction, SED and polarized SED with PAHs, astrosilicates and amorphous carbon (a-C). The astrosilicate population is aligned along the magnetic field lines, while the a-C population may be aligned or not. With their current optical properties, oblate astrosilicate grains are not emissive enough to reproduce the emission to extinction polarization ratio $P_{353}/p_V$ derived with Planck data. Models using prolate astrosilicate grains with an elongation $a/b=3$ and an inclusion of 20% of porosity succeed. The spectral dependence of the polarized SED is steeper in our models than in the data. Models perform slightly better when a-C grains are aligned. A small (6%) volume inclusion of a-C in the astrosilicate matrix removes the need for porosity and perfect grain alignment, and improves the fit to the polarized SED. Dust models based on astrosilicates can be reconciled with Planck data by adapting the shape of grains and adding inclusions of porosity or a-C in the astrosilicate matrix.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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