10 Kの氷から光脱離する水の核スピン異性体比と宇宙の水の起源について;10 Kの氷から光脱離する水の核スピン異性体比と宇宙の水の起源について;Ortho-to-para Ratio of Water Photodesorbed from Ice at 10 K and the Origin of Interstellar Water

Tetsuya Hama, Akira Kouchi, Naoki Watanabe
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Abstract

Chemistry of interstellar H2O is essential for understanding the formation of stars and planetary systems because of the ubiquity of H2O in space. The abundance ratio of nuclear spin isomers (the ortho-to-para ratio, OPR) can be a key for interstellar water chemistry, when assuming that the OPR desorbed from ice is closely related to the ice formation temperature. However, the above assumption has not been experimentally validated. Here, we report that H2O photodesorbed from ice at 10 K shows a statistical OPR of 3, even when the ice is produced in situ by hydrogenation of O2, a known formation process of interstellar H2O. This invalidates the hypothesis for relation between OPR and temperature. Reinterpretation of previous observations is necessary to improve our understanding of interstellar chemistry and the formation of the solar system and comets.
关于从10k的冰中光脱离的水的核自旋异构体比和宇宙中水的起源;关于从10k的冰中光脱离的水的核自旋异构体比和宇宙中水的起源;orto -to-para Ratio of Water Photodesorbed from Ice at 10k and the Origin of Interstellar Water
星际水的化学性质对于理解恒星和行星系统的形成至关重要,因为水在太空中无处不在。当假设从冰中解吸的OPR与冰的形成温度密切相关时,核自旋异构体的丰度比(正对位比,OPR)可以成为星际水化学的关键。然而,上述假设尚未得到实验验证。在这里,我们报告了在10 K下从冰中光解吸的H2O显示出统计OPR为3,即使冰是通过O2的氢化产生的,这是一种已知的星际水的形成过程。这使得OPR与温度关系的假设失效。重新解释以前的观测结果对于提高我们对星际化学以及太阳系和彗星形成的理解是必要的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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