https://pubs.acs.org/doi/abs/10.1021/acs.jpca.5c04880

*Authors: *
Dennis Lima, Saif Al-Kuwari, Ivan Gladich

*14 November 2025*

*Abstract*
Stratospheric aerosol injection (SAI) has been proposed as a geoengineering
strategy to mitigate global warming by increasing Earth’s albedo.
Silica-based materials, such as diamond-doped silica aerogels, have shown
promising optical properties, but their impact on stratospheric chemistry,
ozone one in particular, remains largely unknown. Here, we present
first-principles molecular dynamics (MD) simulations of the heterogeneous
reaction between hydrogen chloride (HCl) and chlorine nitrate (ClONO2), two
main reservoirs of stratospheric chlorine and nitrogen species, on a dry
and hydroxylated α-quartz silica interface, a surface that serves as a
proxy for silica-based aerosols under low relative humidity and
stratospheric conditions. Our results reveal a barrierless reaction pathway
toward the formation of chlorine gas (Cl2), a major contributor to
stratospheric ozone loss. We design a heterogeneous kinetic model informed
by our MD simulation and available experimental data: despite the
barrierless formation of Cl2, the higher surface affinities and partial
pressures of HNO3 and HCl compared to those of ClONO2 result in a
negligible reaction probability, γClONO2, upon chlorine nitrate collision
with the silica surface. Since γClONO2 enters as a proportionality constant
in the definition of the heterogeneous reaction rate, our kinetic model
indicates that the injection of silica-based aerosols may have only a
limited impact on stratospheric ozone depletion driven by HCl and ClONO2
chemistry. At the same time, our findings also underscore the scarcity of
experimental data, the need of better theoretical frameworks for the
inclusion of MD results into kinetic models, and the urgency for further
experimental validations of silica-based SAI technologies before their
deployment in climate intervention strategies.

*Source: ACS PUBLICATIONS *

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