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首页> 外文期刊>The Astrophysical journal >INTERSTELLAR DUST ABSORPTION FEATURES IN THE INFRARED SPECTRUM OF HH 100-IR: SEARCHING FOR THE NITROGEN COMPONENT OF THE ICES
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INTERSTELLAR DUST ABSORPTION FEATURES IN THE INFRARED SPECTRUM OF HH 100-IR: SEARCHING FOR THE NITROGEN COMPONENT OF THE ICES

机译:HH 100-IR红外光谱中星际尘埃吸收特性的研究:寻找冰的氮元素

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摘要

We present observations of solid-state absorption features due to water ice, CO ice, and silicate dust in the spectrum of the bright infrared source (IRS 1) associated with the Herbig-Haro nebula HH 100 in the R Coronae Australis dark cloud. These absorptions are shown to arise predominantly in the molecular cloud rather than in circumstellar matter associated with the infrared source itself, which we deduce to be a pre-main-sequence star obscured by ~25 mag of visual extinction. In common with other lines of sight, the spectra indicate the presence of distinct hydrogen-rich (polar) and hydrogen-poor (nonpolar) phases in the ice toward HH 100-IR. The nonpolar phase is dominated by CO. The strength of the solid CO feature at 4.67 μm suggests that as much as ~40% of all CO in the line of sight may be in the solid phase. Our data show a lack of significant absorption at 4.62 μm that might arise in CN-bearing molecules formed by energetic processing of the mantles. A previous report of structure in the profile of the 3 μm water-ice feature in HH 100-IR that might be attributed to the N-H resonance in condensed ammonia at ~2.96 μm is not confirmed. The abundance ratio NH_3:H_2O in the ices is found to be no more than ~8%, which is probably insufficient to account for the 3.3-3.6 μm "ice-band wing" in terms of ammonium hydrate. However, we propose that the wing might be explained by hydrates containing other bases in addition to ammonia/Further progress is likely to require new laboratory data for appropriate ice mixtures.
机译:我们在与冠冕黑星暗云中的Herbig-Haro星云HH 100相关的明亮红外光源(IRS 1)的光谱中,观察到由于水冰,CO冰和硅酸盐尘而引起的固态吸收特征。这些吸收主要是在分子云中产生的,而不是与红外源本身相关的星际物质中产生的,我们推断这是被约25 mag的视觉灭绝所掩盖的前序星。与其他视线相同,光谱表明向HH 100-IR方向的冰中存在明显的富氢(极性)和贫氢(非极性)相。非极性相由CO主导。固态CO特性的强度为4.67μm,表明视线中多达约40%的CO可能在固态中。我们的数据显示,在4.62μm处缺乏明显的吸收,这可能是由地幔的高能处理形成的含CN分子中可能出现的。尚未确认HH 100-IR中3μm水冰特征的轮廓结构的先前报道,该结构可能归因于〜2.96μm的冷凝氨中的N-H共振。发现冰中的NH_3:H_2O丰度比不超过8%,这可能不足以用水合铵来说明3.3-3.6μm的“冰带翼”。但是,我们建议机翼可以用除氨以外还含有其他碱的水合物来解释/进一步的进展可能需要新的实验室数据来确定合适的冰混合物。

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