Chemical reactions in atmospheric
organic aerosol (OA) add large
uncertainties to accurate predictions of the effect of aerosol on
health, visibility, and climate. The acceleration of reaction rates
of organic compounds in droplets compared to bulk solution has been
reported; however, the mechanism and the principle of acceleration
largely remains unknown. Malonic acid (MA) is a dicarboxylic acid
that exhibits keto–enol tautomerization and is ubiquitous in
organic aerosols found in the nature. An environment controlled electrodynamic
balance (EDB) coupled with Mie scattering imaging (MSI) and Raman
spectroscopy was used to levitate single charged MA droplets and investigate
the effect of relative humidity (RH: 90%, 70%, 50%, and 30%) and size
(28–91 μm diameter) on the reaction kinetics of keto–enol
tautomerization of MA. Raman spectroscopy of hydrogen–deuterium
isotopic exchange in MA droplets enabled quantitative analysis of
MA tautomerization kinetics. The result showed slower reaction rates
of MA droplets at lower RH as well as in larger-sized droplets. Application
of a step-by-step isotopic exchange model to the MA droplets at 90%
RH condition was used to determine the enolization rate of MA, yielding
a value 10-fold higher than determined in bulk solution. Keto and
enol forms of MA have distinctive physicochemical properties, such
as reactivity and hydrogen bond structure. The result from our work
suggests that keto–enol tautomerization can play an important
role for aging of MA-containing OA in nature, as the enol form of
MA can undergo accelerated chemical reactions due to the presence
of the reactive carbon–carbon double bond.