论文标题
二氧化碳冰的红外自由电子激光辐照
Infrared free-electron laser irradiation of carbon dioxide ice
论文作者
论文摘要
据信,星际冰粒在空间中检测到的许多简单且复杂的有机物种的形成中起着关键作用。但是,关于与冰谷物中物种形成和生存有关的物理化学过程的许多基本问题仍未得到解答。在大规模设施(例如自由电子激光器(FELS))的大规模设施的现场工作可以通过为实验室天体物理学界提供新颖的工具来帮助调查冰晶粒的组成和形态。我们将荷兰HFML-Felix-2在HFML-Felix实验室的高可调性,宽红外光谱范围和强度结合在一起,以及超高真空丽莎末端站的特征,以执行依赖于波长的Mid-Mid-Mid-Mid-Mid-Mid-Mid-Mid-Mid-MID-IR辐射实验,该实验是在20 K. Co2 k.20 k.的空间范围内使用20 k.的频率。通过傅立叶变换反射 - 吸收红外(FT-RAIR)光谱法对选定频率的振动能量注入二氧化碳冰中,以研究冰重组效应。这项工作提高了我们对外部触发器(如光子,电子,宇宙射线)以及来自新生原始原始恒星或田间星星的热加热等外部触发器引入的理解的理解。此外,它增加了目前的文献辩论,即在低温下沉积时观察到的二氧化碳的无定形和多晶结构,表明,在我们的实验条件下,二氧化碳在20 k处沉积时会出现非晶态特征,并且在75 k处沉积时是明确的结晶。
Interstellar ice grains are believed to play a key role in the formation of many of the simple and complex organic species detected in space. However, many fundamental questions on the physicochemical processes linked to the formation and survival of species in ice grains remain unanswered. Field work at large-scale facilities such as free-electron lasers (FELs) can aid the investigation of the composition and morphology of ice grains by providing novel tools to the laboratory astrophysics community. We combined the high tunability, wide infrared spectral range and intensity of the FEL beam line FELIX-2 at the HFML-FELIX Laboratory in the Netherlands with the characteristics of the ultrahigh vacuum LISA end station to perform wavelength-dependent mid-IR irradiation experiments of space-relevant pure carbon dioxide (CO2) ice at 20 K. We used the intense monochromatic radiation of FELIX to inject vibrational energy at selected frequencies into the CO2 ice to study ice restructuring effects in situ by Fourier Transform Reflection-Absorption Infrared (FT-RAIR) spectroscopy. This work improves our understanding of how vibrational energy introduced by external triggers such as photons, electrons, cosmic rays, and thermal heating coming from a nascent protostar or field stars is dissipated in an interstellar icy dust grain in space. Moreover, it adds to the current literature debate concerning the amorphous and polycrystalline structure of CO2 ice observed upon deposition at low temperatures, showing that, under our experimental conditions, CO2 ice presents amorphous characteristics when deposited at 20 K and is unambiguously crystalline if deposited at 75 K.