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Mid-infrared imaging spectroscopic measurements of C2H4 frost simulating the outer solar system environments

Earth Planets and Space 2024 1 citation ? Citation count from OpenAlex, updated daily. May differ slightly from the publisher's own count. Score: 35 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Ryoichi Koga, Shohei Negishi, Shohei Negishi, Biao Zhao, Biao Zhao, Yuan Li, Fumiyuki Ito, Yasumasa Kasaba, Yasuhiro Hirahara

Summary

Researchers developed novel cryogenic experimental equipment to simulate the low-temperature solid-phase formation of ethylene (C2H4) frost under outer solar system conditions, using mid-infrared imaging spectroscopy to characterize the resulting frost structure in situ. The study provides laboratory reference data for interpreting C2H4 ice features detected in spacecraft observations of Titan and other icy solar system bodies.

Abstract In the dense and cold atmosphere of Titan, the presence of C 2 H 4 haze has been confirmed by the observations of spacecraft. In the present study, original cryogenic experimental equipment was developed to simulate the low-temperature solid formation of C 2 H 4 in combination with in-situ infrared spectroscopic measurements. As a result, out-of-plane bending vibration ν 7 of solid-phase C 2 H 4 located at ~ 10.5 μm was successfully detected with high sensitivity, and two-dimensional spectrographs of C 2 H 4 at low temperatures were obtained. The obtained spectra of C 2 H 4 can be fitted to the double Lorentzian function with various heights, central wavelengths, and full widths at half the maximum (FWHM) of the two-component Lorentzian functions. They were classified into three types using the fitting parameters. However, their spectral shapes are different from the amorphous, metastable, and crystalline forms obtained by the previous laboratory experiment in terms of the distance of two peak wavelengths and FWHM. The results may link to understanding the spectral band properties of C 2 H 4 condensation in the haze component of Titan. Graphical Abstract

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