Formation of complex organic molecules in hot molecular cores through nondiffusive grain-surface and ice-mantle chemistry

TL;DR

This paper presents a comprehensive gas-grain chemical model for hot molecular cores, incorporating nondiffusive surface and ice-mantle reactions, which better reproduces observed complex organic molecules and their formation regimes.

Contribution

It introduces a novel nondiffusive chemistry approach in hot core models, improving agreement with observations and revealing new formation pathways for complex organic molecules.

Findings

Model reproduces observed molecular abundances accurately.

Nondiffusive chemistry enables earlier formation of COMs.

Radical release during water desorption enhances COM synthesis.

Abstract

A new, more comprehensive model of gas-grain chemistry in hot molecular cores is presented, in which nondiffusive reaction processes on dust-grain surfaces and in ice mantles are implemented alongside traditional diffusive surface/bulk-ice chemistry. We build on our nondiffusive treatments used for chemistry in cold sources, adopting a standard collapse/warm-up physical model for hot cores. A number of other new chemical model inputs and treatments are also explored in depth, culminating in a final model that demonstrates excellent agreement with gas-phase observational abundances for many molecules, including some (e.g. methoxymethanol) that could not be reproduced by conventional diffusive mechanisms. Observed ratios of structural isomers methyl formate, glycolaldehyde and acetic acid are well reproduced by the models. The main temperature regimes are identified in which various complex organic molecules (COMs) are formed. Nondiffusive chemistry advances the production of many COMs to much earlier times and lower temperatures than in previous model implementations. Those species may form either as by-products of simple-ice production, or via early photochemistry within the ices while external UV photons can still penetrate. Cosmic ray-induced photochemistry is less important than in past models, although it affects some species strongly over long timescales. Another production regime occurs during the high-temperature desorption of solid water, whereby radicals trapped in the ice are released onto the grain/ice surface, where they rapidly react. Several recently-proposed gas-phase COM-production mechanisms are also introduced, but they rarely dominate. New surface/ice reactions involving CH and CH$_2$ are found to contribute substantially to the formation of certain COMs.