Rafael Rianço-Silva , Pedro Machado , Zita Martins , Emmanuel Lellouch , Jean-Christophe Loison , Michel Dobrijevic , João A. Dias , José Ribeiro
{"title":"土卫六超高分辨率可见光谱研究:可见光 CH4 波段的谱线特征和寻找 C3","authors":"Rafael Rianço-Silva , Pedro Machado , Zita Martins , Emmanuel Lellouch , Jean-Christophe Loison , Michel Dobrijevic , João A. Dias , José Ribeiro","doi":"10.1016/j.pss.2023.105836","DOIUrl":null,"url":null,"abstract":"<div><p>The atmosphere of Titan is a unique natural laboratory for the study of atmospheric evolution and photochemistry akin to that of the primitive Earth, with a wide array of complex molecules discovered through infrared and sub-mm spectroscopy. Here, we explore high resolution visible spectra of Titan (obtained with VLT-UVES) and retrieve an empirical high resolution list of methane absorption features at high resolution, (<span><math><mrow><mi>R</mi><mo>=</mo><mn>100</mn><mo>.</mo><mn>000</mn></mrow></math></span>) between 5250 Å and 6180 Å, for which no linelists are yet available. Furthermore, we search for the predicted, but previously undetected carbon trimer, C<span><math><msub><mrow></mrow><mrow><mn>3</mn></mrow></msub></math></span>, on the atmosphere of Titan, at its 4051 Å band. Our results are consistent with the presence of C<span><math><msub><mrow></mrow><mrow><mn>3</mn></mrow></msub></math></span> at the upper atmosphere of Titan, with a column density of <span><math><mrow><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mn>13</mn></mrow></msup></mrow></math></span> cm<sup>−2</sup>. This study of Titan’s atmosphere with high-resolution visible spectroscopy presents a unique opportunity to observe a planetary atmosphere where CH<span><math><msub><mrow></mrow><mrow><mn>4</mn></mrow></msub></math></span> is the main visible molecular absorber, from which CH<span><math><msub><mrow></mrow><mrow><mn>4</mn></mrow></msub></math></span> optical proprieties can be studied. It also showcases the use of a close planetary target to test new methods for chemical retrieval of minor atmospheric compounds, in preparation for upcoming studies of cold terrestrial exoplanet atmospheres.</p></div>","PeriodicalId":20054,"journal":{"name":"Planetary and Space Science","volume":"240 ","pages":"Article 105836"},"PeriodicalIF":1.8000,"publicationDate":"2024-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S0032063323002052/pdfft?md5=11b88a0e45862f58da6c7ba9fb67dbec&pid=1-s2.0-S0032063323002052-main.pdf","citationCount":"0","resultStr":"{\"title\":\"A study of very high resolution visible spectra of Titan: Line characterisation in visible CH4 bands and the search for C3\",\"authors\":\"Rafael Rianço-Silva , Pedro Machado , Zita Martins , Emmanuel Lellouch , Jean-Christophe Loison , Michel Dobrijevic , João A. Dias , José Ribeiro\",\"doi\":\"10.1016/j.pss.2023.105836\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The atmosphere of Titan is a unique natural laboratory for the study of atmospheric evolution and photochemistry akin to that of the primitive Earth, with a wide array of complex molecules discovered through infrared and sub-mm spectroscopy. Here, we explore high resolution visible spectra of Titan (obtained with VLT-UVES) and retrieve an empirical high resolution list of methane absorption features at high resolution, (<span><math><mrow><mi>R</mi><mo>=</mo><mn>100</mn><mo>.</mo><mn>000</mn></mrow></math></span>) between 5250 Å and 6180 Å, for which no linelists are yet available. Furthermore, we search for the predicted, but previously undetected carbon trimer, C<span><math><msub><mrow></mrow><mrow><mn>3</mn></mrow></msub></math></span>, on the atmosphere of Titan, at its 4051 Å band. Our results are consistent with the presence of C<span><math><msub><mrow></mrow><mrow><mn>3</mn></mrow></msub></math></span> at the upper atmosphere of Titan, with a column density of <span><math><mrow><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mn>13</mn></mrow></msup></mrow></math></span> cm<sup>−2</sup>. This study of Titan’s atmosphere with high-resolution visible spectroscopy presents a unique opportunity to observe a planetary atmosphere where CH<span><math><msub><mrow></mrow><mrow><mn>4</mn></mrow></msub></math></span> is the main visible molecular absorber, from which CH<span><math><msub><mrow></mrow><mrow><mn>4</mn></mrow></msub></math></span> optical proprieties can be studied. It also showcases the use of a close planetary target to test new methods for chemical retrieval of minor atmospheric compounds, in preparation for upcoming studies of cold terrestrial exoplanet atmospheres.</p></div>\",\"PeriodicalId\":20054,\"journal\":{\"name\":\"Planetary and Space Science\",\"volume\":\"240 \",\"pages\":\"Article 105836\"},\"PeriodicalIF\":1.8000,\"publicationDate\":\"2024-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.sciencedirect.com/science/article/pii/S0032063323002052/pdfft?md5=11b88a0e45862f58da6c7ba9fb67dbec&pid=1-s2.0-S0032063323002052-main.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Planetary and Space Science\",\"FirstCategoryId\":\"101\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0032063323002052\",\"RegionNum\":4,\"RegionCategory\":\"物理与天体物理\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ASTRONOMY & ASTROPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Planetary and Space Science","FirstCategoryId":"101","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0032063323002052","RegionNum":4,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
引用次数: 0
摘要
土卫六的大气层是研究大气演化和光化学的一个独特的天然实验室,与原始地球的大气层类似,通过红外和亚毫米光谱发现了大量复杂的分子。在这里,我们探索了土卫六的高分辨率可见光谱(由 VLT-UVES 获得),并以高分辨率(R=100.000)检索了 5250 Å 和 6180 Å 之间的甲烷吸收特征的经验性高分辨率列表,目前还没有关于这些特征的线性列表。此外,我们还在土卫六大气的 4051 Å 波段搜索了预测到但之前未检测到的碳三聚体 C3。我们的结果与土卫六上层大气中存在的 C3 相符,其柱密度为 1013 cm-2。这项利用高分辨率可见光谱对土卫六大气进行的研究为观测以 CH4 为主要可见分子吸收体的行星大气提供了一个独特的机会,可以从中研究 CH4 的光学特性。它还展示了利用近行星目标来测试大气中次要化合物化学检索的新方法,为即将进行的寒冷陆地系外行星大气研究做准备。
A study of very high resolution visible spectra of Titan: Line characterisation in visible CH4 bands and the search for C3
The atmosphere of Titan is a unique natural laboratory for the study of atmospheric evolution and photochemistry akin to that of the primitive Earth, with a wide array of complex molecules discovered through infrared and sub-mm spectroscopy. Here, we explore high resolution visible spectra of Titan (obtained with VLT-UVES) and retrieve an empirical high resolution list of methane absorption features at high resolution, () between 5250 Å and 6180 Å, for which no linelists are yet available. Furthermore, we search for the predicted, but previously undetected carbon trimer, C, on the atmosphere of Titan, at its 4051 Å band. Our results are consistent with the presence of C at the upper atmosphere of Titan, with a column density of cm−2. This study of Titan’s atmosphere with high-resolution visible spectroscopy presents a unique opportunity to observe a planetary atmosphere where CH is the main visible molecular absorber, from which CH optical proprieties can be studied. It also showcases the use of a close planetary target to test new methods for chemical retrieval of minor atmospheric compounds, in preparation for upcoming studies of cold terrestrial exoplanet atmospheres.
期刊介绍:
Planetary and Space Science publishes original articles as well as short communications (letters). Ground-based and space-borne instrumentation and laboratory simulation of solar system processes are included. The following fields of planetary and solar system research are covered:
• Celestial mechanics, including dynamical evolution of the solar system, gravitational captures and resonances, relativistic effects, tracking and dynamics
• Cosmochemistry and origin, including all aspects of the formation and initial physical and chemical evolution of the solar system
• Terrestrial planets and satellites, including the physics of the interiors, geology and morphology of the surfaces, tectonics, mineralogy and dating
• Outer planets and satellites, including formation and evolution, remote sensing at all wavelengths and in situ measurements
• Planetary atmospheres, including formation and evolution, circulation and meteorology, boundary layers, remote sensing and laboratory simulation
• Planetary magnetospheres and ionospheres, including origin of magnetic fields, magnetospheric plasma and radiation belts, and their interaction with the sun, the solar wind and satellites
• Small bodies, dust and rings, including asteroids, comets and zodiacal light and their interaction with the solar radiation and the solar wind
• Exobiology, including origin of life, detection of planetary ecosystems and pre-biological phenomena in the solar system and laboratory simulations
• Extrasolar systems, including the detection and/or the detectability of exoplanets and planetary systems, their formation and evolution, the physical and chemical properties of the exoplanets
• History of planetary and space research