Secondary organic aerosol (SOA) constitutes a major fraction of atmospheric particles worldwide. It is composed of a multitude of organic compounds (e.g., Kourtchev et al., 2016). Our current understanding and modeling of SOA formation processes are highly uncertain (Pai et al., 2020) and involve representing the complex interplay between gas-phase oxidation and condensation of semi-and low-volatile organic species. SOA models need to include processes such as (a) the multi-step oxidation of the large variety of organic compounds emitted naturally and by human activities, (b) the condensation of semi-volatile species to the particle phase, and (c) the heterogeneous and in-particle reactivity of condensed species. This complexity can only be represented in models that explicitly account for aerosol physico-chemical processes. In these so-called explicit models, the aim is to represent the fate of each individual chemical species through individual reactions, which can number in the 10 9 range (e.g., Aumont et al., 2005). The Generator of Explicit Chemistry and Kinetics for Organics in the Atmosphere (GECKO-A, Aumont et al., 2005) is an example of such a model able to generate chemical mechanisms that explicitly describe the oxidation of organic compounds in the atmosphere, as well as their condensation into the particle phase (Camredon et al., 2007). It has previously been used to study SOA formation in various settings such as atmospheric chamber experiments (