Gas-phase Ortho-to-para Ratio of Formaldehyde Formed at Low Temperatures in Laboratory Ices

K. M. Yocum, O. Wilkins, J. C. Bardwell, S. N. Milam, P. Gerakines
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Abstract

The ortho-to-para ratio (OPR) of formaldehyde (H2CO) has been used as a probe to estimate the formation temperature of molecules in interstellar, circumstellar, and cometary environments, relying on the assumption that nuclear spin conversion is extremely slow, preserving the OPR from molecular formation. An OPR for H2CO less than 3 corresponds to a spin temperature below 30 K and has been proposed to result from formation at low temperatures within an ice, whereas an OPR of 3 is interpreted as arising from warmer formation in the gas phase. In spite of this common assumption, there is no laboratory evidence in the literature to date in support of it. Here, in the first study of its kind for H2CO, we report rotational spectroscopy measurements of the OPR of H2CO sublimated after its formation in methanol (CH3OH) ice samples that were photolyzed by ultraviolet light at 10, 15, 20, and 40 K. None of the measured OPR values correlated with the ice formation temperature.
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实验室冰层中低温形成的甲醛气相正对比例
甲醛(H2CO)的正对位比(OPR)已被用作探测器来估计星际、星周和彗星环境中分子的形成温度,依赖于核自旋转换极其缓慢的假设,使OPR免于分子的形成。H2CO的OPR小于3对应于自旋温度低于30k,并且被认为是冰内低温形成的结果,而OPR为3则被解释为气相中较热形成的结果。尽管有这种普遍的假设,但迄今为止文献中还没有实验室证据支持这种假设。在此,我们首次对H2CO进行了此类研究,报告了在10、15、20和40 K紫外光分解的甲醇(CH3OH)冰样品中形成H2CO后升华的OPR的旋转光谱测量。所有测量的OPR值都与冰的形成温度无关。
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