In this work, we reexamine sulfur chemistry occurring on and in the ice mantles of interstellar dust grains, and report the effects of two new modifications to standard astrochemical models; namely, (a) the incorporation of cosmic ray-driven radiation Corresponding author: Christopher N. Shingledecker cns@mpe.mpg.de Shingledecker et al. et al. (2016). In that work, the authors concluded that this S 2 likely formed in the pre-solar nebula via the radiolysis of species such as H 2 S. In an attempt to improve how astrochemical models treat non-thermal processes, particularly those driven by cosmic rays, we have recently developed methods for including such radiation chemistry in rate-equation-based codes . Our preliminary findings are that the addition of these new mechanisms generally improves the agreement between models and observations (Shingledecker et al. 2018); however, given the novelty of our approach, no modeling studies have yet been done which focus on the effects of cosmic raybombardment on the abundances of sulfur-bearing species in ice mantles.
CalmonteAnother major source of uncertainty in current simulations of grain chemistry concerns reactions within the bulk of dust-grain ice mantles. One significant source of uncertainty in such models involves whether or to what degree bulk diffusion is important, and if so, what the underlying mechanism behind this diffusion might be. Commonly, models today typically assume, for example, swapping (Öberg et al. 2009; Fayolle et al. 2011) or diffusion via interstitial sites (Lamberts et al. 2013; Chang & Herbst 2014; Shingledecker et al. 2017), where the energetic barriers to bulk diffusion, E bulk b, are taken to be some fraction of the desorption energy, E D , and are highly uncertain. In Shingledecker et al. (2019a), we attempted to reduce this ambiguity by simulating well-constrained experiments, rather than the ISM. In our preliminary studies reported there, we found that the assumption that radicals within ices react via thermal diffusion leads to generally poor agreement between calculated and empirical results, due to the much slower chemistry in the simulations than what is shown to occur in the lab. Conversely, good agreement with experimental data was achieved by assuming that radicals in the ice react predominantly with their nearest neighbors, i.e. nondiffusively. These results are in qualitative agreement with a recent study by Ghesquière et al. (2018), who concluded that true bulk diffusion does not occur, rather, as temperatures increase, bulk species can be "passively" transported due to structural changes such as pore collapse or crystallization, or can "actively" diffuse along internal surfaces or cracks.This work, therefore, is an attempt to build upon these recent investigations, and to examine what effect (a) cosmic ray-driven radiation chemistry, and (b) the fast, non-diffusive reaction of radicals in