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
{"title":"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","authors":"Tetsuya Hama, Akira Kouchi, Naoki Watanabe","doi":"10.3131/JVSJ2.60.264","DOIUrl":null,"url":null,"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.","PeriodicalId":17344,"journal":{"name":"Journal of The Vacuum Society of Japan","volume":"3 1","pages":"264-274"},"PeriodicalIF":0.0000,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of The Vacuum Society of Japan","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3131/JVSJ2.60.264","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
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