Gas–particle partitioning of polyol tracers at a suburban site in Nanjing, east China: increased partitioning to the particle phase

Abstract. Gas–particle partitioning of water-soluble organic compounds plays a significant role in influencing the formation, transport, and lifetime of organic aerosols in the atmosphere, but is poorly characterized. In this work, gas- and particle-phase concentrations of isoprene oxidation products (C5-alkene triols and 2-methylterols), levoglucosan, and sugar polyols were measured simultaneously at a suburban site of the western Yangtze River Delta in east China. All target polyols were primarily distributed into the particle phase (85.9 %–99.8 %). Given the uncertainties in measurements and vapor pressure predictions, a dependence of particle-phase fractions on vapor pressures cannot be determined. To explore the impact of aerosol liquid water on gas–particle partitioning of polyol tracers, three partitioning schemes (Cases 1–3) were proposed based on equilibriums of gas vs. organic and aqueous phases in aerosols. If particulate organic matter (OM) is presumed as the only absorbing phase (Case 1), the measurement-based absorptive partitioning coefficients (Kp,OMm) of isoprene oxidation products and levoglucosan were more than 10 times greater than predicted values (Kp,OMt). The agreement between Kp,OMm and Kp,OMt was substantially improved when solubility in a separate aqueous phase was included, whenever water-soluble and water-insoluble OM partitioned into separate (Case 2) or single (Case 3) liquid phases, suggesting that the partitioning of polyol tracers into the aqueous phase in aerosols should not be ignored. The measurement-based effective Henry's law coefficients (KH,em) of polyol tracers were orders of magnitude higher than their predicted values in pure water (KH,wt). Due to the moderate correlations between log⁡(KH,em/KH,wt) and molality of sulfate ions, the gap between KH,em and KH,wt of polyol tracers could not be fully parameterized by the equation defining “salting-in” effects and might be ascribed to mechanisms of reactive uptake, aqueous phase reaction, “like-dissolves-like” principle, etc. These study results also partly reveal the discrepancy between observation and modeling of organic aerosols.

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Gas-particle partitioning of polyol tracers in the western Yangtze River Delta, China: Absorptive or Henry's law partitioning?

10.5194/acp-2021-230 ◽

2021 ◽

Author(s):

Chao Qin ◽

Yafeng Gou ◽

Yuhang Wang ◽

Yuhao Mao ◽

Hong Liao ◽

...

Keyword(s):

Yangtze River ◽

Organic Aerosols ◽

Yangtze River Delta ◽

Water Soluble ◽

Oxidation Products ◽

Particle Phase ◽

Henry's Law ◽

Henry’S Law ◽

Isoprene Oxidation ◽

Isoprene Oxidation Products

Abstract. Gas-particle partitioning of water-soluble organic compounds plays a significant role in the formation and source apportionment of organic aerosols, but is poorly characterized. In this work, gas- and particle-phase concentrations of isoprene oxidation products (C5-alkene triols and 2-methylterols), levoglucosan, and sugar polyols were measured simultaneously at a suburban site of the western Yangtze River Delta in east China. All target polyols were primarily distributed into the particle phase (85.9–99.8 %), and their average particle-phase fractions were not strictly dependent on vapor pressures. Moreover, the measurement-based partitioning coefficients (Kp,OM) of isoprene oxidation products and levoglucosan were 102 to 104 times larger than their predicted Kp,OM based on the equilibrium absorptive partitioning model. These are likely attributed to the hygroscopic properties of polyol tracers and high aerosol liquid water (ALW) concentrations (~20 µg m−3) of the study location. Due to the large gaps (up to 107) between measurement-based effective Henry's law coefficients (KH,e) and predicted values in pure water (KH,w), the gas-particle partitioning of polyol tracers could not be depicted using Henry's law alone either. The regressions of log (KH,w/KH,e) versus molality of major water-soluble components in ALW indicated that sulfate ions (salting-in effect) and water-soluble organic carbon can promote the partitioning of polyol tracers into the aqueous phase. These results suggest a partitioning mechanism of enhanced aqueous-phase uptake for polyol tracers, which partly reveals the discrepancy between observation and modeling of secondary organic aerosols.

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Atmospheric aqueous phase radical chemistry of the isoprene oxidation products methacrolein, methyl vinyl ketone, methacrylic acid and acrylic acid – kinetics and product studies

Physical Chemistry Chemical Physics ◽

10.1039/c3cp54859g ◽

2014 ◽

Vol 16 (13) ◽

pp. 6257 ◽

Cited By ~ 38

Author(s):

Luisa Schöne ◽

Janine Schindelka ◽

Edyta Szeremeta ◽

Thomas Schaefer ◽

Dirk Hoffmann ◽

...

Keyword(s):

Acrylic Acid ◽

Aqueous Phase ◽

Methacrylic Acid ◽

Vinyl Ketone ◽

Methyl Vinyl Ketone ◽

Oxidation Products ◽

Methyl Vinyl ◽

Radical Chemistry ◽

Isoprene Oxidation ◽

Isoprene Oxidation Products

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The effects of isoprene and NOx on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water

Atmospheric Chemistry and Physics ◽

10.5194/acp-18-1171-2018 ◽

2018 ◽

Vol 18 (2) ◽

pp. 1171-1184 ◽

Cited By ~ 10

Author(s):

Marwa M. H. El-Sayed ◽

Diana L. Ortiz-Montalvo ◽

Christopher J. Hennigan

Keyword(s):

Secondary Organic Aerosols ◽

Time Lag ◽

Organic Aerosols ◽

Water Soluble ◽

Oxidation Products ◽

Eastern United States ◽

Water Soluble Organic Carbon ◽

Soluble Organic Carbon ◽

Isoprene Oxidation ◽

Organic Gases

Abstract. Isoprene oxidation produces water-soluble organic gases capable of partitioning to aerosol liquid water. The formation of secondary organic aerosols through such aqueous pathways (aqSOA) can take place either reversibly or irreversibly; however, the split between these fractions in the atmosphere is highly uncertain. The aim of this study was to characterize the reversibility of aqSOA formed from isoprene at a location in the eastern United States under substantial influence from both anthropogenic and biogenic emissions. The reversible and irreversible uptake of water-soluble organic gases to aerosol water was characterized in Baltimore, Maryland, USA, using measurements of particulate water-soluble organic carbon (WSOCp) in alternating dry and ambient configurations. WSOCp evaporation with drying was observed systematically throughout the late spring and summer, indicating reversible aqSOA formation during these times. We show through time lag analyses that WSOCp concentrations, including the WSOCp that evaporates with drying, peak 6 to 11 h after isoprene concentrations, with maxima at a time lag of 9 h. The absolute reversible aqSOA concentrations, as well as the relative amount of reversible aqSOA, increased with decreasing NOx ∕ isoprene ratios, suggesting that isoprene epoxydiol (IEPOX) or other low-NOx oxidation products may be responsible for these effects. The observed relationships with NOx and isoprene suggest that this process occurs widely in the atmosphere, and is likely more important in other locations characterized by higher isoprene and/or lower NOx levels. This work underscores the importance of accounting for both reversible and irreversible uptake of isoprene oxidation products to aqueous particles.

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Contribution of Isoprene Oxidation Products to Marine Aerosol over the North-East Atlantic

Advances in Meteorology ◽

10.1155/2010/482603 ◽

2010 ◽

Vol 2010 ◽

pp. 1-10 ◽

Cited By ~ 13

Author(s):

Tatu Anttila ◽

Baerbel Langmann ◽

Saji Varghese ◽

Colin O'Dowd

Keyword(s):

North Atlantic ◽

Organic Aerosol ◽

Water Soluble ◽

Oxidation Products ◽

East Atlantic ◽

High Biological Activity ◽

North East ◽

The North ◽

Isoprene Oxidation ◽

Isoprene Oxidation Products

Secondary organic aerosol (SOA) formation through isoprene oxidation was investigated with the regional-scale climate model REMOTE. The applied modeling scheme includes a treatment for marine primary organic aerosol emissions, aerosol microphysics, and SOA formation through the gas/particle partitioning of semivolatile, water-soluble oxidation products. The focus was on SOA formation taking place over the North-East Atlantic during a period of high biological activity. Isoprene SOA concentrations were up to ~5 ngm−3over North Atlantic in the base case model runs, and isoprene oxidation made a negligible contribution to the marine organic aerosol (OA) mass. In particular, isoprene SOA did not account for the observed water-soluble organic carbon (WSOC) concentrations over North Atlantic. The performed model calculations, together with results from recent field measurements, imply a missing source of SOA over remote marine areas unless the isoprene oxidation products are considerably less volatile than the current knowledge indicates.

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The effects of isoprene and NOx on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water

10.5194/acp-2017-702 ◽

2017 ◽

Author(s):

Marwa M. H. El-Sayed ◽

Diana L. Ortiz-Montalvo ◽

Christopher J. Hennigan

Keyword(s):

Secondary Organic Aerosols ◽

Time Lag ◽

Organic Aerosols ◽

Water Soluble ◽

Oxidation Products ◽

Eastern United States ◽

Water Soluble Organic Carbon ◽

Soluble Organic Carbon ◽

Isoprene Oxidation ◽

Organic Gases

Abstract. Isoprene oxidation produces water-soluble organic gases capable of partitioning to aerosol liquid water. The formation of secondary organic aerosols through such aqueous pathways (aqSOA) can take place either reversibly or irreversibly; however, the split between these fractions in the atmosphere is highly uncertain. The aim of this study was to characterize the reversibility of aqSOA formed from isoprene at a location in the eastern United States under substantial influence from both anthropogenic and biogenic emissions. The reversible and irreversible uptake of water-soluble organic gases to aerosol water was characterized in Baltimore, MD using measurements of particulate water-soluble organic carbon (WSOCp) in alternating dry and ambient configurations. WSOCp evaporation with drying was observed systematically throughout the late spring and summer, indicating reversible aqSOA formation during these times. We show through time lag analyses that WSOCp concentrations, including the WSOCp that evaporates with drying, peak ~ 6–11 h after isoprene concentrations, with maxima at a time lag of 9 h. The absolute reversible aqSOA concentrations, as well as the relative amount of reversible aqSOA, increased with decreasing NOx/isoprene ratios, suggesting that isoprene epoxydiol (IEPOX) or other low-NOx oxidation products were responsible for these effects. The observed relationships with NOx and isoprene suggest that this process occurs widely in the atmosphere, and is likely more important in other locations characterized by higher isoprene and/or lower NOx levels. It is also likely that this phenomenon will increase in importance in the future, given predictions of biogenic and anthropogenic emissions under future regulatory and climate scenarios.

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Explicit modeling of volatile organic compounds partitioning in the atmospheric aqueous phase

Atmospheric Chemistry and Physics ◽

10.5194/acp-13-1023-2013 ◽

2013 ◽

Vol 13 (2) ◽

pp. 1023-1037 ◽

Cited By ~ 30

Author(s):

C. Mouchel-Vallon ◽

P. Bräuer ◽

M. Camredon ◽

R. Valorso ◽

S. Madronich ◽

...

Keyword(s):

Organic Matter ◽

Dissolved Organic Matter ◽

Water Content ◽

Gas Phase ◽

Aqueous Phase ◽

Water Soluble ◽

Chemical Mechanism ◽

Organic Species ◽

Cloud Water Content ◽

Isoprene Oxidation

Abstract. The gas phase oxidation of organic species is a multigenerational process involving a large number of secondary compounds. Most secondary organic species are water-soluble multifunctional oxygenated molecules. The fully explicit chemical mechanism GECKO-A (Generator of Explicit Chemistry and Kinetics of Organics in the Atmosphere) is used to describe the oxidation of organics in the gas phase and their mass transfer to the aqueous phase. The oxidation of three hydrocarbons of atmospheric interest (isoprene, octane and α-pinene) is investigated for various NOx conditions. The simulated oxidative trajectories are examined in a new two dimensional space defined by the mean oxidation state and the solubility. The amount of dissolved organic matter was found to be very low (yield less than 2% on carbon atom basis) under a water content typical of deliquescent aerosols. For cloud water content, 50% (isoprene oxidation) to 70% (octane oxidation) of the carbon atoms are found in the aqueous phase after the removal of the parent hydrocarbons for low NOx conditions. For high NOx conditions, this ratio is only 5% in the isoprene oxidation case, but remains large for α-pinene and octane oxidation cases (40% and 60%, respectively). Although the model does not yet include chemical reactions in the aqueous phase, much of this dissolved organic matter should be processed in cloud drops and modify both oxidation rates and the speciation of organic species.

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