Abstract

Context. In the near future, high spatial and spectral infrared (IR) data of star-forming regions obtained by the James Webb Space Telescope may reveal new solid-state features of various species, including more intriguing classes of chemical compounds. The identification of complex organic molecules (COMs) in the upcoming data will only be possible when laboratory IR ice spectra of these species under astronomically relevant conditions are available for comparison. For this purpose, systematic series of laboratory measurements are performed, providing high-resolution IR spectra of COMs. Here, spectra of pure methylamine (CH3NH2) and methylamine-containing ices are discussed. Aims. The work is aimed at characterizing the mid-IR (500–4000 cm−1, 20–2.5 μm) spectra of methylamine in pure and mixed ices to provide accurate spectroscopic data of vibrational bands that are most suited to trace this species in interstellar ices. Methods. Fourier transform infrared spectroscopy is used to record spectra of CH3NH2 in the pure form and mixed with H2O, CH4, and NH3, for temperatures ranging from 15 to 160 K. The IR spectra in combination with HeNe laser (632.8 nm) interference data of pure CH3NH2 ice was used to derive the IR band strengths of methylamine in pure and mixed ices. Results. The refractive index of amorphous methylamine ice at 15 K was determined as being 1.30 ± 0.01. Accurate spectroscopic information and band strength values are systematically presented for a large set of methylamine-containing ices and different temperatures. Selected bands are characterized and their use as methylamine tracers is discussed. The selected bands include the following: the CH3 antisymmetric stretch band at 2881.3 cm−1 (3.471 μm), the CH3 symmetric stretch band at 2791.9 cm−1 (3.582 μm), the CH3 antisymmetric deformation bands, at 1455.0 and 1478.6 cm−1 (6.873 and 6.761 μm), the CH3 symmetric deformation band at 1420.3 cm−1 (7.042 μm), and the CH3 rock at 1159.2 cm−1 (8.621 μm). Using the laboratory data recorded in this work and ground-based spectra of ices toward YSOs (Young Stellar Objects), upper-limits for the methylamine ice abundances are derived. In some of these YSOs, the methylamine abundance is less than 4% relative to H2O.

Highlights

  • Amino acids are key molecules to life on Earth

  • Changes in the IR absorbance profile of pure methylamine and mixed ices are described, and some ideas concerning the origins of these changes are pointed out

  • The peak positions and full width at half maximum (FWHM) of the selected bands are organized in Tables B1–B15, and the integrated absorbance of the methylamine in different ice mixtures is listed in Tables C1–C15

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Summary

Introduction

Amino acids are key molecules to life on Earth. Whereas such species have been found in meteorites, already more than half a century ago (Kvenvolden et al 1970), the simplest amino acid, glycine (NH2CH2COOH) still has not been unambiguously detected in the interstellar medium (ISM). Its formation pathways in the gas phase and in the solid state have been a matter of ongoing debate (Elsila et al 2007). A direct consequence of this has been that several molecules, regarded as potential glycine precursors, have become a target in new surveys with the ultimate goal being point out sources that may host glycine at a detectable level. Recent examples include the search for amino acetonitrile (NH2CH2CN) by Belloche et al

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