https://pubs.acs.org/doi/full/10.1021/acs.est.3c08408

*Authors*
Fangqun Yu, Bruce E. Anderson, Jeffrey R. Pierce, Alex Wong, Arshad Nair,
Gan Luo, and Jason Herb

*Publication Date: April 9, 2024*

https://doi.org/10.1021/acs.est.3c08408

*Abstract*

Stratospheric aerosol injection (SAI) is proposed as a means of reducing
global warming and climate change impacts. Similar to aerosol enhancements
produced by volcanic eruptions, introducing particles into the stratosphere
would reflect sunlight and reduce the level of warming. However,
uncertainties remain about the roles of nucleation mechanisms, ionized
molecules, impurities (unevaporated residuals of injected precursors), and
ambient conditions in the generation of SAI particles optimally sized to
reflect sunlight. Here, we use a kinetic ion-mediated and homogeneous
nucleation model to study the formation of H2SO4 particles in aircraft
exhaust plumes with direct injection of H2SO4 vapor. We find that under the
conditions that produce particles of desired sizes (diameter ∼200–300 nm),
nucleation occurs in the nascent (t < 0.01 s), hot (T = 360–445 K), and dry
(RH = 0.01–0.1%) plume and is predominantly unary. Nucleation on chemiions
occurs first, followed by neutral new particle formation, which converts
most of the injected H2SO4 vapor to particles. Coagulation in the aging and
diluting plumes governs the subsequent evolution to a narrow (σg = 1.3)
particle size distribution. Scavenging by exhaust soot is negligible, but
scavenging by acid impurities or incomplete H2SO4 evaporation in the hot
exhaust plume and enhanced background aerosols can matter. This research
highlights the need to obtain laboratory and/or real-world experiment data
to verify the model prediction.

*Source: ACS PUBLICATIONS *

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