Heterogeneous Reactions of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub>/NH<sub>3</sub> on α-Fe<sub>2</sub>O<sub>3</sub> Particles: The Effects of Relative Humidity on Secondary Organic Aerosol Formation

Heterogeneous reactions of volatile organic compounds (VOCs) with mineral dust can influence secondary aerosol formation in the atmosphere. This study investigated the heterogeneous reactions of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub> in the presence of NH<sub>3</sub> on α-Fe<sub>2</sub>O<sub>3</sub> particles using a gas-flow system combined with Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS) under simulated different relative humidity (RH) conditions. The results indicate that a secondary organic aerosol (SOA) is formed from the appearance of η<sup>2</sup>(N,O) bands at 1341 cm<sup>-1</sup> and R-COOH bands at 1476 and 1608 cm<sup>-1</sup>. C<sub>3</sub>H<sub>6</sub> reacts with O<sub>3</sub> to form the Criegee intermediates (CIs) such as CH<sub>3</sub>HCOO and CH<sub>2</sub>OO. Some of these CIs are neutralized with NH<sub>3</sub> to form amides, while others react with aldehydes to form intermediates that finally decompose into carboxylic acids. Water molecules play negative potential roles in the formation of SOA on α-Fe<sub>2</sub>O<sub>3</sub> particles. Under continuous RH changes, the formation rate of organic amides increases from 1.07 × 10<sup>16</sup> to 2.73 × 10<sup>16</sup> ions·g<sup>-1</sup>·s<sup>-1</sup>, while the formation rate of carboxylic acids increases from 9.39 × 10<sup>15</sup> to 2.11 × 10<sup>16</sup> ions·g<sup>-1</sup>·s<sup>-1</sup> with decreasing RH in the range of 80-0%. Furthermore, the reactive uptake coefficient for NH<sub>3</sub> in the initial stage increases from (4.85 ± 0.35) × 10<sup>-10</sup> to (2.08 ± 0.03) × 10<sup>-9</sup> with decreasing RH from 77.4% to 0% during the heterogeneous reaction of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub>/NH<sub>3</sub> on α-Fe<sub>2</sub>O<sub>3</sub> particles under constant RH conditions. The inhibiting effect under high RHs indicates that water molecules are unfavorable for SOA formation due to the consumption of reactant gases and the competitive effect on active sites of α-Fe<sub>2</sub>O<sub>3</sub> particles. These results not only significantly enhance the understanding of the reaction kinetics of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub>/NH<sub>3</sub> on the surface of α-Fe<sub>2</sub>O<sub>3</sub> particles under different RHs but also provide theoretical insights into SOA formation mechanisms under atmospheric pollution conditions.

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Journal
The Journal of Physical Chemistry A
Published
2025-10-02
DOI
https://doi.org/10.1021/acs.jpca.5c05512
Primary Topic
Atmospheric chemistry and aerosols
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article
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article

Heterogeneous Reactions of C3H6/O3/NH3 on α-Fe2O3 Particles: The Effects of Relative Humidity on Secondary Organic Aerosol Formation

Qi-Ling Xiao, Mingzhe Dong, Xi Xi, Sijie Wen et al.
The Journal of Physical Chemistry A
Atmospheric chemistry and aerosols
article

Heterogeneous Reactions of C3H6/O3/NH3 on α-Fe2O3 Particles: The Effects of Relative Humidity on Secondary Organic Aerosol Formation

Qi-Ling Xiao, Mingzhe Dong, Xi Xi, Sijie Wen, Zhicheng Ma, Xiang He
article en

Abstract

Heterogeneous reactions of volatile organic compounds (VOCs) with mineral dust can influence secondary aerosol formation in the atmosphere. This study investigated the heterogeneous reactions of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub> in the presence of NH<sub>3</sub> on α-Fe<sub>2</sub>O<sub>3</sub> particles using a gas-flow system combined with Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS) under simulated different relative humidity (RH) conditions. The results indicate that a secondary organic aerosol (SOA) is formed from the appearance of η<sup>2</sup>(N,O) bands at 1341 cm<sup>-1</sup> and R-COOH bands at 1476 and 1608 cm<sup>-1</sup>. C<sub>3</sub>H<sub>6</sub> reacts with O<sub>3</sub> to form the Criegee intermediates (CIs) such as CH<sub>3</sub>HCOO and CH<sub>2</sub>OO. Some of these CIs are neutralized with NH<sub>3</sub> to form amides, while others react with aldehydes to form intermediates that finally decompose into carboxylic acids. Water molecules play negative potential roles in the formation of SOA on α-Fe<sub>2</sub>O<sub>3</sub> particles. Under continuous RH changes, the formation rate of organic amides increases from 1.07 × 10<sup>16</sup> to 2.73 × 10<sup>16</sup> ions·g<sup>-1</sup>·s<sup>-1</sup>, while the formation rate of carboxylic acids increases from 9.39 × 10<sup>15</sup> to 2.11 × 10<sup>16</sup> ions·g<sup>-1</sup>·s<sup>-1</sup> with decreasing RH in the range of 80-0%. Furthermore, the reactive uptake coefficient for NH<sub>3</sub> in the initial stage increases from (4.85 ± 0.35) × 10<sup>-10</sup> to (2.08 ± 0.03) × 10<sup>-9</sup> with decreasing RH from 77.4% to 0% during the heterogeneous reaction of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub>/NH<sub>3</sub> on α-Fe<sub>2</sub>O<sub>3</sub> particles under constant RH conditions. The inhibiting effect under high RHs indicates that water molecules are unfavorable for SOA formation due to the consumption of reactant gases and the competitive effect on active sites of α-Fe<sub>2</sub>O<sub>3</sub> particles. These results not only significantly enhance the understanding of the reaction kinetics of C<sub>3</sub>H<sub>6</sub>/O<sub>3</sub>/NH<sub>3</sub> on the surface of α-Fe<sub>2</sub>O<sub>3</sub> particles under different RHs but also provide theoretical insights into SOA formation mechanisms under atmospheric pollution conditions.

The Journal of Physical Chemistry AVol. 129(41)
Ministry of Education of the People's Republic of China (CN), Xinjiang University (CN)
Openalex Percentile: Top 68%
Atmospheric chemistry and aerosols
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