Related Experiment Video
Updated: Apr 25, 2026

Reactive Vapor Deposition of Conjugated Polymer Films on Arbitrary Substrates
Published on: January 17, 2018
Vapor-wall deposition in chambers: theoretical considerations
Renee C McVay1, Christopher D Cappa, John H Seinfeld
1Division of Chemistry and Chemical Engineering and §Division of Engineering and Applied Science, California Institute of Technology , Pasadena, California 91125, United States.
Secondary organic aerosol (SOA) yields increase with seed surface area only when vapor condensation is kinetically limited. Vapor-wall deposition reduces SOA yields, necessitating its consideration for accurate atmospheric extrapolations.
Area of Science:
- Atmospheric Chemistry
- Aerosol Science
- Environmental Science
Background:
- Laboratory chamber studies are crucial for understanding secondary organic aerosol (SOA) formation.
- Vapor-wall deposition is a known artifact in chamber experiments that can influence measured SOA yields.
- The role of kinetic limitations in SOA formation and their interplay with chamber artifacts require further investigation.
Purpose of the Study:
- To investigate the influence of vapor-wall deposition and kinetic limitations on secondary organic aerosol (SOA) yields.
- To determine the conditions under which seed aerosol surface area affects SOA yield measurements.
- To provide a framework for accurately extrapolating laboratory-derived SOA yields to atmospheric conditions.
Main Methods:
- Utilized a coupled vapor-particle dynamics model to simulate toluene oxidation experiments.
- Varied seed aerosol surface area in model simulations to mimic laboratory conditions.
- Compared characteristic time scales of gas-phase reaction, vapor-wall deposition, and gas-particle equilibration.
Main Results:
- A seed surface area dependence of the SOA yield was observed only when the condensation of vapors onto particles was kinetically limited.
- The existence of kinetic limitation was predictable by comparing relevant time scales.
- Vapor-wall deposition was found to consistently depress SOA yields, irrespective of kinetic limitations.
Conclusions:
- The observed increase in SOA yield with seed surface area in laboratory chambers is primarily due to kinetic limitations in vapor condensation, not solely vapor-wall deposition.
- Accurate extrapolation of chamber-derived SOA yields to the atmosphere requires accounting for both vapor-wall deposition and kinetic limitations.
- Understanding gas-particle equilibration, influenced by the accommodation coefficient (αp), is vital for assessing kinetic limitations.
Related Concept Videos
The Van der Waals Equation
Phase Transitions: Vaporization and Condensation
Vaporization
Real Gases: Effects of Intermolecular Forces and Molecular Volume Deriving Van der Waals Equation
Phase Transitions: Sublimation and Deposition
Vapor Pressure

