C3H6/O3/NH3对α-Fe2O3颗粒的非均相反应:相对湿度对二次有机气溶胶形成的影响

IF 2.8 2区 化学 Q3 CHEMISTRY, PHYSICAL
Qiyue Xiao, , , Xiang He*, , , Xi Xi, , , Zhicheng Ma, , , Mingsong Dong, , and , Sijie Wen, 
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引用次数: 0

摘要

挥发性有机化合物(VOCs)与矿物粉尘的非均相反应可以影响大气中二次气溶胶的形成。在模拟不同相对湿度(RH)条件下,利用气体流动系统结合漫反射红外傅立叶变换光谱(DRIFTS)研究了NH3存在下C3H6/O3在α-Fe2O3颗粒上的非均相反应。结果表明:1341 cm-1 η2(N,O)带和1476、1608 cm-1 R-COOH带的出现形成了二次有机气溶胶(SOA)。C3H6与O3反应生成Criegee中间体(CIs),如CH3HCOO和ch260。其中一些CIs与NH3中和形成酰胺,而另一些则与醛反应形成中间体,最终分解成羧酸。水分子在α-Fe2O3颗粒上形成SOA的过程中起负作用。在RH持续变化的条件下,有机酰胺的生成速率从1.07 × 1016增加到2.73 × 1016离子·g-1·s-1,羧酸的生成速率从9.39 × 1015增加到2.11 × 1016离子·g-1·s-1, RH在80-0%范围内降低。在恒RH条件下,C3H6/O3/NH3在α-Fe2O3颗粒上的非均相反应,NH3的反应吸收系数从(4.85±0.35)× 10-10增加到(2.08±0.03)× 10-9, RH从77.4%降低到0%。高RHs条件下的抑制效应表明,由于反应气体的消耗和α-Fe2O3颗粒活性位点的竞争作用,水分子不利于SOA的形成。这些结果不仅显著提高了对不同RHs下C3H6/O3/NH3在α-Fe2O3颗粒表面的反应动力学的认识,而且为大气污染条件下SOA形成机理提供了理论见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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

Heterogeneous Reactions of C3H6/O3/NH3 on α-Fe2O3 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 C3H6/O3 in the presence of NH3 on α-Fe2O3 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 η2(N,O) bands at 1341 cm–1 and R-COOH bands at 1476 and 1608 cm–1. C3H6 reacts with O3 to form the Criegee intermediates (CIs) such as CH3HCOO and CH2OO. Some of these CIs are neutralized with NH3 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-Fe2O3 particles. Under continuous RH changes, the formation rate of organic amides increases from 1.07 × 1016 to 2.73 × 1016 ions·g–1·s–1, while the formation rate of carboxylic acids increases from 9.39 × 1015 to 2.11 × 1016 ions·g–1·s–1 with decreasing RH in the range of 80–0%. Furthermore, the reactive uptake coefficient for NH3 in the initial stage increases from (4.85 ± 0.35) × 10–10 to (2.08 ± 0.03) × 10–9 with decreasing RH from 77.4% to 0% during the heterogeneous reaction of C3H6/O3/NH3 on α-Fe2O3 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-Fe2O3 particles. These results not only significantly enhance the understanding of the reaction kinetics of C3H6/O3/NH3 on the surface of α-Fe2O3 particles under different RHs but also provide theoretical insights into SOA formation mechanisms under atmospheric pollution conditions.

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来源期刊
The Journal of Physical Chemistry A
The Journal of Physical Chemistry A 化学-物理:原子、分子和化学物理
CiteScore
5.20
自引率
10.30%
发文量
922
审稿时长
1.3 months
期刊介绍: The Journal of Physical Chemistry A is devoted to reporting new and original experimental and theoretical basic research of interest to physical chemists, biophysical chemists, and chemical physicists.
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