Energetic Electron Irradiations of Amorphous and Crystalline Sulphur - Bearing Astrochemical Ices Duncan V. Mifsud12 Péter Herczku2 Rich árd Rácz2 K.K. Rahul2 Sándor T.S. Kovács2

2025-04-29 0 0 959.16KB 20 页 10玖币
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Energetic Electron Irradiations of Amorphous and Crystalline Sulphur-
Bearing Astrochemical Ices
Duncan V. Mifsud1,2,*, Péter Herczku2,*, Richárd Rácz2, K.K. Rahul2, Sándor T.S. Kovács2,
Zoltán Juhász2, Béla Sulik2, Sándor Biri2, Robert W. McCullough3, Zuzana Kaňuchová4,
Sergio Ioppolo5, Perry A. Hailey1, and Nigel J. Mason1,2,*
1 Centre for Astrophysics and Planetary Science, School of Physical Sciences, University of Kent,
Canterbury CT2 7NH, United Kingdom
2 Institute for Nuclear Research (Atomki), Debrecen H-4026, Hungary
3 Department of Physics and Astronomy, School of Mathematics and Physics, Queen’s University
Belfast, Belfast BT7 1NN, United Kingdom
4 Astronomical Institute, Slovak Academy of Sciences, Tatranská Lomnica SK-059 60, Slovakia
5 School of Electronic Engineering and Computer Science, Queen Mary University of London,
London E1 4NS, United Kingdom
* Correspondence: Duncan V. Mifsud dm618@kent.ac.uk
Péter Herczku herczku@atomki.hu
Nigel J. Mason n.j.mason@kent.ac.uk
ORCID Identification Numbers
Duncan V. Mifsud 0000-0002-0379-354X
Péter Herczku 0000-0002-1046-1375
Richard Rácz 0000-0003-2938-7483
K.K. Rahul 0000-0002-5914-7061
Sándor T.S. Kovács 0000-0001-5332-3901
Zoltán Juhász 0000-0003-3612-0437
Béla Sulik 0000-0001-8088-5766
Sándor Biri 0000-0002-2609-9729
Robert W. McCullough 0000-0002-4361-8201
Zuzana Kaňuchová 0000-0001-8845-6202
Sergio Ioppolo 0000-0002-2271-1781
Perry A. Hailey 0000-0002-8121-9674
Nigel J. Mason 0000-0002-4468-8324
Abstract
Laboratory experiments have confirmed that the radiolytic decay rate of astrochemical ice
analogues is dependent upon the solid phase of the target ice, with some crystalline molecular
ices being more radio-resistant than their amorphous counterparts. The degree of radio-
resistance exhibited by crystalline ice phases is dependent upon the nature, strength, and extent
of the intermolecular interactions that characterise their solid structure. For example, it has
been shown that crystalline CH3OH decays at a significantly slower rate when irradiated by 2
keV electrons at 20 K than does the amorphous phase due to the stabilising effect imparted by
the presence of an extensive array of strong hydrogen bonds. These results have important
consequences for the astrochemistry of interstellar ices and outer Solar System bodies, as they
imply that the chemical products arising from the irradiation of amorphous ices (which may
include prebiotic molecules relevant to biology) should be more abundant than those arising
from similar irradiations of crystalline phases. In this present study, we have extended our work
on this subject by performing comparative energetic electron irradiations of the amorphous and
crystalline phases of the sulphur-bearing molecules H2S and SO2 at 20 K. We have found
evidence for phase-dependent chemistry in both these species, with the radiation-induced
exponential decay of amorphous H2S being more rapid than that of the crystalline phase, similar
to the effect that has been previously observed for CH3OH. For SO2, two fluence regimes are
apparent: a low-fluence regime in which the crystalline ice exhibits a rapid exponential decay
while the amorphous ice possibly resists decay, and a high-fluence regime in which both phases
undergo slow exponential-like decays. We have discussed our results in the contexts of
interstellar and Solar System ice astrochemistry and the formation of sulphur allotropes and
residues in these settings.
Keywords: Astrochemistry; Planetary science; Electron irradiation; Radiation chemistry;
Amorphous ice; Crystalline ice; Sulphur
1 Introduction
It has been established for some time now that the laboratory irradiation of astrochemical ice
analogues using energetic charged particles (i.e., ions and electrons) or ultraviolet photons may
lead to the production of prebiotic molecules relevant to biology, such as amino acids or
nucleobases (e.g., Muñoz-Caro et al. 2002, Hudson et al. 2008, Nuevo et al. 2012). Motivated
by a desire to further understand the non-equilibrium chemistry leading to the formation of
these so-called ‘seeds of life’, many studies have sought to determine and quantify the influence
of various physical parameters on the outcome of such reactions. Perhaps the best studied of
these is ice temperature, with previous works having demonstrated the key influence of this
parameter on the abundance of product molecules formed after irradiation (e.g., Sivaraman et
al. 2007, Mifsud et al. 2022a).
Our recent work has also demonstrated that the solid phase of an irradiated ice plays a crucial
role in determining the outcome of astrochemical reactions mediated by ionising radiation.
Through a series of comparative electron irradiations, we have demonstrated that the radiolytic
decay rate of an astrochemical ice is dependent upon the nature, strength, and extent of the
intermolecular interactions that characterise its solid phase (Mifsud et al. 2022b, Mifsud et al.
2022c). For instance, the decay rate of α-crystalline CH3OH was found to be significantly less
rapid than that of the amorphous phase. This was attributed to the existence of an extensive
network of strong hydrogen bonds that exists in the α-crystalline phase. This network requires
an additional energy input from the projectile electrons to be overcome, thus leaving less
energy overall to drive radiolytic chemistry. Conversely, the amorphous CH3OH ice is
characterised only by localised clusters of hydrogen bonded molecules. Such a structure does
not benefit from the same stabilising effect supplied by the network of hydrogen bonds in the
α-crystalline phase, particularly as hydrogen bonding in CH3OH is known to be a cooperative
phenomenon in which the presence of one hydrogen bond in the network strengthens
successive hydrogen bonds through electrostatic effects (Kleeberg and Luck 1989, Sum and
Sandler 2000).
In the case of N2O ice, the decay rate of the amorphous phase was noted to be only moderately
more rapid than that of the crystalline phase (Mifsud et al. 2022b). The dominant
intermolecular forces of attraction in solid N2O are expected to be dipole-dipole interactions.
Although the orientation of these dipoles in the crystalline phase is anticipated to confer some
degree of resistance against radiolytic decay compared to the amorphous phase, this is
considerably less than that induced by the hydrogen bonding network in α-crystalline CH3OH.
This therefore explains the more similar radiolytic decay rates of amorphous and crystalline
N2O. Such results carry important implications for the radiation processing of astrochemical
ices, as they suggest that the irradiation of amorphous ices is more chemically productive than
that of crystalline ones; particularly in the case of those ices which are able to form strong and
extensive intermolecular bonds when crystalline. Extending this idea further, it is entirely
possible that those astrophysical environments in which space radiation-induced amorphisation
processes dominate over thermally-induced crystallisation may be characterised by a more
productive radiation chemistry. This idea is not unreasonable, particularly in light of the
discovery of several complex organic molecules in pre-stellar cores (e.g., McGuire et al. 2020,
Burkhardt et al. 2021).
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 109 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
摘要:

EnergeticElectronIrradiationsofAmorphousandCrystallineSulphur-BearingAstrochemicalIcesDuncanV.Mifsud1,2,*,PéterHerczku2,*,RichárdRácz2,K.K.Rahul2,SándorT.S.Kovács2,ZoltánJuhász2,BélaSulik2,SándorBiri2,RobertW.McCullough3,ZuzanaKaňuchová4,SergioIoppolo5,PerryA.Hailey1,andNigelJ.Mason1,2,*1CentreforAs...

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