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Heterogeneous Reaction of SO2 on Manganese Oxides: the Effect of Crystal Structure and Relative Humidity

机译:SO2在氧化锰上的非均相反应:晶体结构和相对湿度的影响

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摘要

Manganese oxides from anthropogenic sources can promote the formation of sulfate through catalytic oxidation of SO2. In this study, the kinetics of SO2 reactions on MnO2 with different morphologies (α, β, γ and δ) was investigated using flow tube reactor and in situ Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS). Under dry conditions, the reactivity towards SO2 uptake was highest on δ-MnO2 but lowest on β-MnO2, with a geometric uptake coefficient (γobs) of (2.42 ± 0.13) ×10–2 and a corrected uptake coefficient (γc) of (1.48 ± 0.21) ×10−6 for the former while γobs of (3.35 ± 0.43) ×10−3 and γc of (7.46 ± 2.97) ×10−7 for the latter. Under wet conditions, the presence of water altered the chemical form of sulfate and was in favor for the heterogeneous oxidation of SO2. The maximum sulfate formation rate was reached at 25% RH and 45% for δ-MnO2 and γ-MnO2, respectively, possibly due to their different crystal structures. The results suggest that morphologies and RH are important factors influencing the heterogeneous reaction of SO2 on mineral aerosols, and that aqueous oxidation process involving transition metals of Mn might be a potential important pathway for SO2 oxidation in the atmosphere.
机译:来自人为来源的锰氧化物可通过SO2的催化氧化促进硫酸盐的形成。在这项研究中,使用流管反应器和原位漫反射红外傅里叶变换光谱(DRIFTS)研究了不同形态(α,β,γ和δ)的MnO2上SO2反应的动力学。在干燥条件下,δ-MnO2对SO2吸收的反应性最高,而β-MnO2对SO2吸收的反应性最低,其几何吸收系数(γobs)为(2.42±0.13)×10 –2 ,且校正后前者的吸收系数(γc)为(1.48±0.21)×10 −6 ,而γobs为(3.35±0.43)×10 -3 ,γc为(7.46± 2.97)×10 −7 。在潮湿条件下,水的存在改变了硫酸盐的化学形式,有利于SO2的多相氧化。 δ-MnO2和γ-MnO2的最大硫酸盐生成速率分别在25%RH和45%时达到,可能是由于它们的晶体结构不同。结果表明,形态和相对湿度是影响SO2与矿物气溶胶异相反应的重要因素,涉及Mn过渡金属的水氧化过程可能是大气中SO2氧化的潜在重要途径。

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