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Dust models post-Planck: constraining the far-infrared opacity of dust in the diffuse interstellar medium

机译:普朗克后的尘埃模型:限制星际弥散介质中尘埃的远红外不透明度

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Aims. We compare the performance of several dust models in reproducing the dust spectral energy distribution (SED) per unit extinction in the diffuse interstellar medium (ISM). We use our results to constrain the variability of the optical properties of big grains in the diffuse ISM, as published by the Planck collaboration. Methods. We use two different techniques to compare the predictions of dust models to data from the Planck HFI, IRAS, and SDSS surveys. First, we fit the far-infrared emission spectrum to recover the dust extinction and the intensity of the interstellar radiation field (ISRF). Second, we infer the ISRF intensity from the total power emitted by dust per unit extinction, and then predict the emission spectrum. In both cases, we test the ability of the models to reproduce dust emission and extinction at the same time. Results. We identify two issues. Not all models can reproduce the average dust emission per unit extinction: there are differences of up to a factor ~2 between models, and the best accord between model and observation is obtained with the more emissive grains derived from recent laboratory data on silicates and amorphous carbons. All models fail to reproduce the variations in the emission per unit extinction if the only variable parameter is the ISRF intensity: this confirms that the optical properties of dust are indeed variable in the diffuse ISM. Conclusions. Diffuse ISM observations are consistent with a scenario where both ISRF intensity and dust optical properties vary. The ratio of the far-infrared opacity to the V band extinction cross-section presents variations of the order of ~20% (40?50% in extreme cases), while ISRF intensity varies by ~30% (~60% in extreme cases). This must be accounted for in future modelling.
机译:目的我们比较了几种粉尘模型在再现星际弥散介质(ISM)中每单位灭绝的粉尘光谱能量分布(SED)方面的性能。正如普朗克合作发表的那样,我们使用我们的结果来约束弥散ISM中大晶粒光学特性的可变性。方法。我们使用两种不同的技术将灰尘模型的预测与来自普朗克HFI,IRAS和SDSS调查的数据进行比较。首先,我们拟合远红外发射光谱以恢复尘埃的消光和星际辐射场(ISRF)的强度。其次,我们从单位灭绝的粉尘发射的总功率推断出ISRF强度,然后预测发射光谱。在这两种情况下,我们都测试模型同时再现粉尘排放和灭绝的能力。结果。我们确定两个问题。并非所有模型都能再现出每单位绝灭后的平均粉尘排放量:各模型之间的差异最大可达2倍左右,并且模型和观测值之间的最佳吻合来自最近关于硅酸盐和非晶态的实验室数据得出的放射性更强的颗粒。碳。如果唯一可变的参数是ISRF强度,则所有模型都无法再现单位消光的发射变化:这证实了在扩散ISM中灰尘的光学特性确实是可变的。结论。弥散ISM观察与ISRF强度和尘埃光学特性均发生变化的情况一致。远红外不透明度与V波段消光截面的比率呈现约20%的变化(极端情况下为40%至50%),而ISRF强度变化为〜30%(极端情况下为60%) )。在以后的建模中必须考虑到这一点。

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