Enhanced oxidation of SO2 by H2O2 during haze events: constraints from sulfur isotopes
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Sulfate aerosols play a critical role in atmospheric chemistry and climate change. However, the mechanism of sulfate formation during haze events remains highly uncertain. In this work, sulfur isotopic compositions of SO<sub>2</sub> and sulfate in PM<sub>2.5</sub> samples collected in Tianjin, China as well as a Rayleigh distillation model are used to constrain SO<sub>2</sub> oxidation pathways. Here, we show the sulfur isotopic compositions of SO<sub>2</sub> and sulfate as well as concentrations of major ions in PM2.5. Our results show that a large sulfur isotope fractionation between SO<sub>2</sub> and sulfate observed in the first stage of haze events may be attributed to an enhanced oxidation of SO<sub>2</sub> by H<sub>2</sub>O<sub>2</sub>. This study highlights the important role of SO<sub>2</sub> oxidation by H<sub>2</sub>O<sub>2</sub> during the haze events. In addition, it is particularly important to note that the sulfur isotopic fractionation factors during haze events dispaly a distinct trend to other periods, indicating that this isotopic approach is useful in understanding the sulfate formation during haze events.
硫酸盐气溶胶(Sulfate aerosols)在大气化学与气候变化中发挥着关键作用。然而,霾天气过程中硫酸盐的形成机制仍存在极高不确定性。本研究采集了中国天津地区细颗粒物(PM₂.₅)样品中的二氧化硫(SO₂)与硫酸盐的硫同位素组成,并结合瑞利蒸馏模型(Rayleigh distillation model)对二氧化硫的氧化路径进行约束。本文展示了细颗粒物样品中二氧化硫、硫酸盐的硫同位素组成以及主要离子浓度。研究结果表明,霾天气初期观测到的二氧化硫与硫酸盐之间显著的硫同位素分馏,可能由过氧化氢(H₂O₂)对二氧化硫的强化氧化作用所致。本研究凸显了H₂O₂介导的二氧化硫氧化在霾天气过程中的重要作用。此外,需特别注意的是,霾天气期间的硫同位素分馏因子与其他时段呈现出显著差异,这表明该同位素方法有助于理解霾天气下硫酸盐的形成机制。



