In this present study, we have expounded upon our previous work by performing comparative
electron irradiations of the crystalline and amorphous phases of pure H2S and SO2
astrochemical ice analogues, thus simulating the processing such ices undergo during their
interaction with galactic cosmic rays, stellar winds, or magnetospheric plasmas as a result of
the production of large quantities of secondary electrons (Mason et al. 2014, Boyer et al. 2016).
Solid H2S is known to exhibit a number of stable crystalline phases under low temperature and
ambient pressure conditions (Fathe et al. 2006), but it is the crystalline phase III (hereafter
simply referred to as the crystalline H2S phase) which is of importance under conditions
relevant to astrochemistry. This phase is orthorhombic, having eight molecules per unit cell
and adopting the Pbcm space group. SO2 may also exist as an orthorhombic crystalline solid
under astrochemical conditions, but in this case the Aba2 space group is adopted and there are
only two molecules per unit cell (Schriver-Mazzuoli et al. 2003).
Although sulphur is one of the most abundant elements in the cosmos and is of importance in
both biochemical and geochemical contexts, much remains unknown regarding its chemistry
in interstellar and outer Solar System settings (Mifsud et al. 2021a). It is thought, for instance,
that H2S ice processing by galactic cosmic rays or ultraviolet photons accounts for the apparent
depletion of sulphur (relative to its total cosmic abundance) in dense interstellar clouds by
producing large quantities of atomic sulphur or molecular sulphur chains and rings which are
difficult to detect using current observation techniques (Jiménez-Escobar and Muñoz-Caro
2011, Jiménez-Escobar et al. 2014). H2S itself has not yet been definitively detected in
interstellar icy grain mantles (Boogert et al. 2015). Conversely, SO2 ice has been detected
within both the dense interstellar medium as well as on the surfaces of outer Solar System
bodies such as the Galilean moons of Jupiter (Boogert et al. 1997, Carlson et al. 1999).
However, the exact chemical mechanisms leading to its formation in these settings remain
widely debated (Mifsud et al. 2021a).
The purpose of this study is thus two-fold: (i) to determine whether the phase of irradiated
sulphur-bearing molecular ices influences the radiation-induced rate of decay as was previously
demonstrated for non-sulphur-bearing ices; and (ii) to contribute further to our (comparatively
poor) understanding of the extra-terrestrial chemistry of sulphur. To achieve these goals, the
amorphous and crystalline phases of pure H2S and SO2 ices were respectively irradiated with
2 and 1.5 keV electrons, and the resultant physico-chemical changes were followed in situ
using Fourier-transform mid-infrared (FT-IR) transmission absorption spectroscopy.
2 Experimental Methodology
The irradiation experiments were performed using the Ice Chamber for Astrophysics-
Astrochemistry (ICA); a custom-built experimental apparatus located at the Institute for
Nuclear Research (Atomki) in Debrecen, Hungary. This apparatus (Fig. 1) has been described
in detail in previous publications (Herczku et al. 2021, Mifsud et al. 2021b), and so only a brief
description of the most salient details will be provided here. The ICA is a UHV-compatible
chamber with a nominal base pressure of a few 10–9 mbar which is achieved by the combined
action of a dry rough vacuum pump and a turbomolecular pump. Within the centre of the
chamber is a gold-coated oxygen-free copper sample holder which supports up to four ZnSe
deposition substrates, onto which astrochemical ice analogues may be prepared. The