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Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in the Anthropocene

机译:在二次有机气溶胶和矿物粉尘中形成的反应性氧物种,影响云化学和人类的公共卫生

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Mineral dust and secondary organic aerosols (SOA) account for a major fraction of atmospheric particulate matter, affecting climate, air quality and public health. How mineral dust interacts with SOA to influence cloud chemistry and public health, however, is not well understood. Here, we investigated the formation of reactive oxygen species (ROS), which are key species of atmospheric and physiological chemistry, in aqueous mixtures of SOA and mineral dust by applying electron paramagnetic resonance (EPR) spectrometry in combination with a spin-trapping technique, liquid chromatography-tandem mass spectrometry (LC-MS/MS), and a kinetic model. We found that substantial amounts of ROS including OH, superoxide as well as carbon- and oxygen-centred organic radicals can be formed in aqueous mixtures of isoprene, alpha-pinene, naphthalene SOA and various kinds of mineral dust (ripidolite, montmorillonite, kaolinite, palygorskite, and Saharan dust). The molar yields of total radicals were similar to 0.02-0.5% at 295 K, which showed higher values at 310 K, upon 254 nm UV exposure, and under low pH (<3) conditions. ROS formation can be explained by the decomposition of organic hydroperoxides, which are a prominent fraction of SOA, through interactions with water and Fenton-like reactions with dissolved transition metal ions. Our findings imply that the chemical reactivity and aging of SOA particles can be enhanced upon interaction with mineral dust in deliquesced particles or cloud/fog droplets. SOA decomposition could be comparably important to the classical Fenton reaction of H2O2 with Fe2+ and that SOA can be the main source of OH radicals in aqueous droplets at low concentrations of H2O2 and Fe2+. In the human respiratory tract, the inhalation and deposition of SOA and mineral dust can also lead to the release of ROS, which may contribute to oxidative stress and play an important role in the adverse health effects of atmospheric aerosols in the Anthropocene.
机译:矿物粉尘和次级有机气溶胶(SOA)占大气颗粒物质的主要部分,影响气候,空气质量和公共卫生。然而,矿物粉尘如何与SOA相互作用以影响云化学和公共卫生,并没有很好地理解。在这里,我们研究了活性氧物质(ROS)的形成,其是大气和生理化学的关键物种,通过将电子顺磁共振(EPR)光谱与旋转捕获技术组合使用电子顺磁共振(EPR)光谱,液相色谱 - 串联质谱(LC-MS / MS)和动力学模型。我们发现,在异戊二烯,α-甲烯,萘SOA和各种矿物粉尘(Ripidolite,Montmorillonite,高岭石,帕莱戈斯斯坦特和撒哈拉尘埃)。总基团的摩尔产率在295 k下类似于0.02-0.5%,其在310 k下显示出较高的值,在254nm紫外线暴露时,在低pH(<3)条件下。可以通过与溶解的过渡金属离子的水和芬顿状反应的相互作用来解释ROS形成,这是一种有机氢过氧化物的分解,这是SOA的突出级分。我们的研究结果暗示,在潮上颗粒或云/雾液滴中的矿物粉尘相互作用,可以提高SOA颗粒的化学反应性和老化。 SOA分解可能与Fe2 +的H 2 O 2的经典芬顿反应相当重要,并且SOA可以是低浓度的H2O2和Fe2 +的水滴中的OH基团的主要来源。在人类呼吸道中,SOA和矿物粉尘的吸入和沉积也可以导致ROS的释放,这可能有助于氧化应激,并在乌甲基烯的大气气溶胶的不利健康影响中发挥重要作用。

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