Observations of the D-H ratio in Methane in the atmosphere of Saturns moon, Titan - where did the Saturnian system formReport as inadecuate



 Observations of the D-H ratio in Methane in the atmosphere of Saturns moon, Titan - where did the Saturnian system form


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The details of the Solar systems formation are still heavily debated. Questions remain about the formation locations of the giant planets, and the degree to which volatile material was mixed throughout the proto-planetary system. One diagnostic which offers great promise in helping to unravel the history of planet formation is the study of the level of deuteration in various Solar system bodies. For example, the D-H ratio of methane in the atmosphere of Titan can be used as a diagnostic of the initial conditions of the solar nebula within the region of giant planet formation, and can help us to determine where Titan and, by extension, the Saturnian system accreted its volatile material. The level of Titanian deuteration also has implications for both the sources and long term evolution of Titans atmospheric composition. We present the results of observations taken in the 1.58 microns window using the NIFS spectrometer on the Gemini telescope, and model our data using the VSTAR line-by-line transfer model, which yields a D-H ratio for Titans atmosphere of 143+-16 x 10^{-6} 1. We are currently in the process of modeling the Gemini high resolution GNIRS spectra using new sets of line parameters derived for methane in the region between 1.2-1.7 microns 2.



Author: Lucyna Kedziora-Chudczer; Jeremy Bailey; Jonathan Horner

Source: https://archive.org/







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