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First Observation of the Submillimeter Polarization Spectrum in a Translucent Molecular Cloud

机译:半透明分子云中亚毫米波偏振光谱的首次观察

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Polarized emission from aligned dust is a crucial tool for studies of magnetism in the ISM, but a troublesome contaminant for studies of cosmic microwave background polarization. In each case, an understanding of the significance of the polarization signal requires well-calibrated physical models of dust grains. Despite decades of progress in theory and observation, polarized dust models remain largely underconstrained. During its 2012 flight, the balloon-borne telescope BLASTPol obtained simultaneous broadband polarimetric maps of a translucent molecular cloud at 250, 350, and 500 μm. Combining these data with polarimetry from the Planck?850 μm band, we have produced a submillimeter polarization spectrum, the first for a cloud of this type. We find the polarization degree to be largely constant across the four bands. This result introduces a new observable with the potential to place strong empirical constraints on ISM dust polarization models in a previously inaccessible density regime. Compared to models by Draine & Fraisse, our result disfavors two of their models for which all polarization arises due only to aligned silicate grains. By creating simple models for polarized emission in a translucent cloud, we verify that extinction within the cloud should have only a small effect on the polarization spectrum shape, compared to the diffuse ISM. Thus, we expect the measured polarization spectrum to be a valid check on diffuse ISM dust models. The general flatness of the observed polarization spectrum suggests a challenge to models where temperature and alignment degree are strongly correlated across major dust components.
机译:对准尘埃的极化发射是研究ISM中磁性的重要工具,但对于研究宇宙微波背景极化却是一个麻烦的污染物。在每种情况下,对偏振信号的重要性的理解都需要经过良好校准的尘粒物理模型。尽管在理论和观测上取得了数十年的进步,但极化尘埃模型仍然在很大程度上受约束。气球式望远镜BLASTPol在2012年的飞行过程中,同时获得了250、350和500μm的半透明分子云的宽带极化图。将这些数据与来自普朗克850μm波段的偏振仪相结合,我们产生了亚毫米级的偏振光谱,这是此类云的第一个。我们发现极化度在四个频段上基本上是恒定的。这个结果引入了一个新的可观测的现象,它有可能在以前无法达到的密度状态下对ISM尘埃极化模型施加强大的经验约束。与Draine&Fraisse的模型相比,我们的结果不利于他们的两个模型,因为它们的所有极化仅是由于对齐的硅酸盐晶粒而引起的。通过为半透明云中的偏振发射创建简单模型,我们验证了与漫射ISM相比,云中的消光对偏振光谱形状的影响很小。因此,我们期望所测得的偏振光谱能够有效地验证弥散ISM尘埃模型。所观察到的偏振光谱的总体平坦度表明,对于温度和对准度在主要粉尘成分之间密切相关的模型而言,这是一个挑战。
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