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Scattering from dust in molecular clouds: Constraining the dust grain size distribution through near-infrared cloudshine and infrared coreshine

机译:尘埃在分子云中的散射:通过近红外云雾和红外核心光泽限制尘埃粒径分布

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Context. The largest grains (0.5?1 μm) in the interstellar size distribution are efficient in scattering near- and mid-infrared radiation. These wavelengths are therefore particularly well suited to probe the still uncertain high-end of the size distribution. Aims. We investigate the change in appearance of a typical low-mass molecular core from the Ks (2.2 μm) band to the Spitzer IRAC 3.6 and 8 micron bands, and compare with model calculations, which include variations of the grain size distribution. Methods. We combine Spitzer IRAC and ground-based near-infrared observations to characterize the scattered light observed at the near- and mid-infrared wavelengths from the core L260. Using a spherical symmetric model core, we perform radiative transfer calculations to study the impact of various dust size distributions on the intensity profiles across the core. Results. The observed scattered light patterns in the Ks and 3.6 μm bands are found to be similar. By comparison with radiative transfer models the two profiles place constraints on the relative abundance of small and large (more than 0.25 μm) dust grains. The scattered light profiles are found to be inconsistent with an interstellar silicate grain distribution extending only to 0.25 μm and large grains are needed to reach the observed fluxes and the flux ratios. The shape of the Ks band surface brightness profile limits the largest grains to 1?1.5 μm. Conclusions. In addition to observing coreshine in the Spitzer IRAC channels, the combination with ground-based near-infrared observations are suited to constrain the properties of large grains in cores.
机译:上下文。星际尺寸分布中最大的晶粒(0.5?1μm)可有效散射近红外和中红外辐射。因此,这些波长特别适合探测尺寸分布仍不确定的高端。目的我们调查了从Ks(2.2μm)谱带到Spitzer IRAC 3.6和8微米谱带的典型低质量分子核外观的变化,并与模型计算(包括晶粒尺寸分布的变化)进行了比较。方法。我们将Spitzer IRAC和基于地面的近红外观测结果相结合,以表征从核心L260在近红外和中红外波长处观测到的散射光。使用球形对称模型核心,我们执行辐射转移计算,以研究各种灰尘尺寸分布对整个核心强度分布的影响。结果。发现在Ks和3.6μm波段中观察到的散射光图案相似。与辐射传输模型相比,这两个剖面对大小颗粒(大于0.25μm)的相对丰度具有约束。发现散射光轮廓与仅延伸到0.25μm的星际硅酸盐晶粒分布不一致,并且需要大晶粒才能达到观察到的通量和通量比。 Ks带表面亮度分布图的形状将最大晶粒限制在1〜1.5μm。结论。除了在Spitzer IRAC通道中观察岩心亮度外,还可以结合地面近红外观测值来限制岩心中大晶粒的特性。

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