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Desorption lifetimes and activation energies influencing gas–surface interactions and multiphase chemical kinetics

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Berkemeier,  Thomas
Multiphase Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Pöschl,  Ulrich
Multiphase Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Citation

Knopf, D. A., Ammann, M., Berkemeier, T., Pöschl, U., & Shiraiwa, M. (2024). Desorption lifetimes and activation energies influencing gas–surface interactions and multiphase chemical kinetics. Atmospheric Chemistry and Physics, 24(6), 3445 -3528. doi:10.5194/acp-24-3445-2024.


Cite as: https://hdl.handle.net/21.11116/0000-000F-14DA-5
Abstract
Adsorption and desorption of gases on liquid or solid substrates are involved in multiphase processes and heterogeneous chemical reactions. The desorption energy (), which depends on the intermolecular forces between adsorbate and substrate, determines the residence time of chemical species at interfaces. We show how and temperature influence the net uptake or release of gas species, the rates of surface–bulk exchange and surface or bulk reactions, and the equilibration timescales of gas–particle partitioning. Using literature data, we derive a parameterization to estimate for a wide range of chemical species based on the molecular mass, polarizability, and oxygen-to-carbon ratio of the desorbing species independent of substrate-specific properties, which is possible because of the dominant role of the desorbing species' properties. Correlations between and the enthalpies of vaporization and solvation are rooted in molecular interactions. The relation between and desorption kinetics reflects the key role of interfacial exchange in multiphase processes. For small molecules and semi-volatile organics (VOC, IVOC, SVOC), values around 10–100 kJ mol−1 correspond to desorption lifetimes around nanoseconds to days at room temperature. Even higher values up to years are obtained at low temperatures and for low volatile organic compounds (LVOC, ELVOC/ULVOC) relevant for secondary organic aerosols (SOA). Implications are discussed for SOA formation, gas–particle partitioning, organic phase changes, and indoor surface chemistry. We expect these insights to advance the mechanistic and kinetic understanding of multiphase processes in atmospheric and environmental physical chemistry, aerosol science, materials science, and chemical engineering.