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The mid-infrared extinction in molecular clouds - Case study of B 335

机译:分子云中的中红外消光-B 335的案例研究

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Aims. The purpose of the present investigation is to probe the dust properties inside a molecular cloud, in particular how particle growth and the presence of ice coatings may change the overall shape of the extinction curve. Methods. Field stars behind a molecular cloud can be used to probe the cloud extinction for both the reddening and the absorption features. By combining multi-colour photometry and IR spectroscopy the spectral class of the star can be determined as can the extinction curve, including the vibrational bands of ices and silicates. Results. Based on observations of field stars behind the dark globule B?335, we determine the reddening curve from 0.35 to 24?μm. The water ice band at 3.1?μm is weaker (τ(3.1)?=?0.4) than expected from the cloud extinction (AV?≈?10 for the sightline to the most obscured star). On the other hand, the CO ice band at 4.7?μm is strong (τ(4.67)?=?0.7) and indicates that the mass column density of frozen CO is about the same as that of water ice. We fit the observations to model calculations and find that the thin ice coatings on the silicate and carbon grains (assumed to be spherical) lower the optical extinction by a few percent. We show that the reddening curves for the two background stars, for which the silicate band has been measured, can be accurately modelled from the UV to 24??μm. These models only include graphite and silicate grains (plus thin ice mantles for the most obscured star), so there is no need for any additional major grain component to explain the slow decline of the reddening curve beyond the K band. As expected, the dust model for the dense part of the cloud has more large grains than for the outer regions. We propose that the well established shallow reddening curve beyond the K band has two different explanations: larger graphite grains in dense regions and relatively small grains in the diffuse ISM, giving rise to substantially less extinction beyond the K band than previously thought. Conclusions. For the sight line towards the most obscured star, we derive the relation AKs?=?0.97·E(J???KKs), and assuming that all silicon is bound in silicates, N(2?H2+H)??≈????1.5?×?1021·AV???≈???9?×?1021·AKs. For the rim of the cloud we get AKs?=?0.51·E(J???Ks), which is close to recent determinations for the diffuse ISM. The corresponding gas column density is N(2?H2+H)??≈???2.3?×?1021·AV???≈???3?×?1022·AKs.
机译:目的本研究的目的是探究分子云内部的粉尘特性,特别是颗粒生长和冰层的存在如何改变消光曲线的整体形状。方法。分子云后面的场星可用于探测云消光的变红和吸收特征。通过将多色光度法和红外光谱法结合起来,可以像消光曲线一样确定恒星的光谱类别,包括冰和硅酸盐的振动带。结果。根据对暗球B?335后面的场星的观察,我们确定了从0.35到24?μm的变红曲线。在3.1?μm处的水冰带比云层灭绝所期望的要弱(τ(3.1)?=?0.4)(视线到最被遮挡的恒星的AV?≈?10)。另一方面,在4.7μm处的CO冰带很强(τ(4.67)θ=α0.7),表明冷冻的CO的质量柱密度与水冰的质量柱密度大致相同。我们将观测值用于模型计算,发现硅酸盐和碳粒上的薄冰层(假定为球形)使光学消光率降低了百分之几。我们表明,已经测量了硅酸盐带的两个背景恒星的变红曲线可以从紫外线到24?μm精确建模。这些模型仅包括石墨和硅酸盐颗粒(对于最模糊的恒星,加上稀薄的冰幔),因此不需要任何其他主要颗粒成分来解释变红曲线在K波段以外的缓慢下降。不出所料,云的密集部分的尘埃模型具有比外围区域更大的颗粒。我们认为,在K波段以外建立良好的浅红色曲线有两种不同的解释:密集区域中较大的石墨晶粒和弥散ISM中的晶粒相对较小,与以前所认为的相比,在K波段以外的消光现象要少得多。结论。对于朝向最模糊恒星的视线,我们推导关系AKs?=?0.97·E(J ??? KKs),并假定所有硅都结合在硅酸盐中,N(2?H2 + H)?? 1.5××1021·AV≈9××1021·AKs。对于云的边缘,我们得到AKs?=?0.51·E(J ??? Ks),这与最近对弥散ISM的确定相近。相应的气柱密度为N(2·H2 + H)≈≈2.3××1021·AV≈≈3××1022·AKs。

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