Size-Dependent Sigmoidal Reaction Kinetics for Pyruvic Acid Condensation at the Air–Water Interface in Aqueous Microdroplets
Meng Li,
Christian Boothby,
Robert E. Continetti
et al.
Abstract:The chemistry of pyruvic acid (PA) under thermal dark
conditions
is limited in bulk solutions, but in microdroplets it is shown to
readily occur. Utilizing in situ micro-Raman spectroscopy as a probe,
we investigated the chemistry of PA within aqueous microdroplets in
a relative humidity- and temperature-controlled environmental cell.
We found that PA undergoes a condensation reaction to yield mostly
zymonic acid. Interestingly, the reaction follows a size-dependent
sigmoidal kinetic profile, i.e., an inductio… Show more
“…Both S/V and pH effects together contribute to the enhancement factor (referring to the ratio of sulfate production rates in microdroplets to that in the bulk solution) ranging from ∼1.56 × 10 3 to ∼1.14 × 10 4 times (Figure f). This striking size-dependent acceleration trend observed in this study agrees well with findings in early publications reported by our group and other research groups. ,,,,, Numerical calculations further highlight a significant acceleration of the photosensitized formation of atmospheric sulfate at the AWI of microdroplets under atmosphere-relevant conditions.…”
Section: Resultssupporting
confidence: 92%
“…This striking sizedependent acceleration trend observed in this study agrees well with findings in early publications reported by our group and other research groups. 26,35,36,45,59,60 Numerical calculations further highlight a significant acceleration of the photosensitized formation of atmospheric sulfate at the AWI of microdroplets under atmosphere-relevant conditions. Before we set out to reveal the photosensitized reaction mechanism and make a comparison between reaction pathways that occur in the bulk and interface, key chemical features of HULIS were initially characterized.…”
The multiphase oxidation of sulfur dioxide (SO2) to
form sulfate is a complex and important process in the atmosphere.
While the conventional photosensitized reaction mainly explored in
the bulk medium is reported to be one of the drivers to trigger atmospheric
sulfate production, how this scheme functionalizes at the air–water
interface (AWI) of aerosol remains an open question. Herein, employing
an advanced size-controllable microdroplet-printing device, surface-enhanced
Raman scattering (SERS) analysis, nanosecond transient adsorption
spectrometer, and molecular level theoretical calculations, we revealed
the previously overlooked interfacial role in photosensitized oxidation
of SO2 in humic-like substance (HULIS) aerosol, where a
3–4 orders of magnitude increase in sulfate formation rate
was speculated in cloud and aerosol relevant-sized particles relative
to the conventional bulk-phase medium. The rapid formation of a battery
of reactive oxygen species (ROS) comes from the accelerated electron
transfer process at the AWI, where the excited triplet state of HULIS
(3HULIS*) of the incomplete solvent cage can readily capture
electrons from HSO3
– in a way that is
more efficient than that in the bulk medium fully blocked by water
molecules. This phenomenon could be explained by the significantly
reduced desolvation energy barrier required for reagents residing
in the AWI region with an open solvent shell.
“…Both S/V and pH effects together contribute to the enhancement factor (referring to the ratio of sulfate production rates in microdroplets to that in the bulk solution) ranging from ∼1.56 × 10 3 to ∼1.14 × 10 4 times (Figure f). This striking size-dependent acceleration trend observed in this study agrees well with findings in early publications reported by our group and other research groups. ,,,,, Numerical calculations further highlight a significant acceleration of the photosensitized formation of atmospheric sulfate at the AWI of microdroplets under atmosphere-relevant conditions.…”
Section: Resultssupporting
confidence: 92%
“…This striking sizedependent acceleration trend observed in this study agrees well with findings in early publications reported by our group and other research groups. 26,35,36,45,59,60 Numerical calculations further highlight a significant acceleration of the photosensitized formation of atmospheric sulfate at the AWI of microdroplets under atmosphere-relevant conditions. Before we set out to reveal the photosensitized reaction mechanism and make a comparison between reaction pathways that occur in the bulk and interface, key chemical features of HULIS were initially characterized.…”
The multiphase oxidation of sulfur dioxide (SO2) to
form sulfate is a complex and important process in the atmosphere.
While the conventional photosensitized reaction mainly explored in
the bulk medium is reported to be one of the drivers to trigger atmospheric
sulfate production, how this scheme functionalizes at the air–water
interface (AWI) of aerosol remains an open question. Herein, employing
an advanced size-controllable microdroplet-printing device, surface-enhanced
Raman scattering (SERS) analysis, nanosecond transient adsorption
spectrometer, and molecular level theoretical calculations, we revealed
the previously overlooked interfacial role in photosensitized oxidation
of SO2 in humic-like substance (HULIS) aerosol, where a
3–4 orders of magnitude increase in sulfate formation rate
was speculated in cloud and aerosol relevant-sized particles relative
to the conventional bulk-phase medium. The rapid formation of a battery
of reactive oxygen species (ROS) comes from the accelerated electron
transfer process at the AWI, where the excited triplet state of HULIS
(3HULIS*) of the incomplete solvent cage can readily capture
electrons from HSO3
– in a way that is
more efficient than that in the bulk medium fully blocked by water
molecules. This phenomenon could be explained by the significantly
reduced desolvation energy barrier required for reagents residing
in the AWI region with an open solvent shell.
“…Growing evidence points to reactions of VOCs with Criegee intermediates, and autoxidation reactions initiated by addition of OH to alkenes, providing rapid routes to highly oxygenated molecules (HOMs) which can accumulate in SOA particles. ,,− Laboratory studies of the rates and products of such reactions and of new-particle SOA nucleation and growth, the latter in simulation chambers equipped with particle counters, are now unravelling this complicated chemistry. Sunlight-induced oligomerization of tropospherically photoactive compounds such as pyruvic acid and other α-keto acids dissolved in or at the surface of aqueous aerosol droplets is another proposed route to SOA formation supported by recent laboratory investigations. − As a further illustration of the importance of interfacial chemistry in aerosols, pyruvic acid was also recently shown to undergo condensation reactions at the air–water interface of aqueous droplets, forming zymonic acid under dark conditions …”
Section: Laboratory Studies Of Atmospheric Photochemistrymentioning
confidence: 95%
“…109−112 As a further illustration of the importance of interfacial chemistry in aerosols, pyruvic acid was also recently shown to undergo condensation reactions at the air−water interface of aqueous droplets, forming zymonic acid under dark conditions. 113 Although not yet implemented directly in experiments on micrometer-scale water droplets, ultrafast transient absorption (TA) spectroscopy studies of photochemical reactions in bulk solutions can provide insights about aqueous photochemistry in atmospheric organic aerosols. Recent examples include measurements using both broadband UV−visible and timeresolved infrared (TRIR) spectroscopy of nitroaromatic compounds (nitrobenzene and nitrophenols), 114 which are important chromophores in brown carbon aerosols produced by biomass burning.…”
Section: The Journal Of Physical Chemistrymentioning
Research that explores the chemistry of Earth's atmosphere is central to the current understanding of global challenges such as climate change, stratospheric ozone depletion, and poor air quality in urban areas. This research is a synergistic combination of three established domains: earth observation, for example, using satellites, and in situ field measurements; computer modeling of the atmosphere and its chemistry; and laboratory measurements of the properties and reactivity of gas-phase molecules and aerosol particles. The complexity of the interconnected chemical and photochemical reactions which determine the composition of the atmosphere challenges the capacity of laboratory studies to provide the spectroscopic, photochemical, and kinetic data required for computer models. Here, we consider whether predictions from computational chemistry using modern electronic structure theory and nonadiabatic dynamics simulations are becoming sufficiently accurate to supplement quantitative laboratory data for wavelength-dependent absorption cross-sections, photochemical quantum yields, and reaction rate coefficients. Drawing on presentations and discussions from the CECAM workshop on Theoretical and Experimental Advances in Atmospheric Photochemistry held in March 2024, we describe key concepts in the theory of photochemistry, survey the state-of-the-art in computational photochemistry methods, and compare their capabilities with modern experimental laboratory techniques. From such considerations, we offer a perspective on the scope of computational (photo)chemistry methods based on rigorous electronic structure theory to become a fourth core domain of research in atmospheric chemistry.
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