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Gas-phase hydrolysis of triplet SO2: A possible direct route to atmospheric acid formation

机译:三重态SO2的气相水解:直接形成大气酸的可能途径

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摘要

Sulfur chemistry is of great interest to the atmospheric chemistry of several planets. In the presence of water, oxidized sulfur can lead to new particle formation, influencing climate in significant ways. Observations of sulfur compounds in planetary atmospheres when compared with model results suggest that there are missing chemical mechanisms. Here we propose a novel mechanism for the formation of sulfurous acid, which may act as a seed for new particle formation. In this proposed mechanism, the lowest triplet state of SO2 (3B1), which may be accessed by near-UV solar excitation of SO2 to its excited 1B1 state followed by rapid intersystem crossing, reacts directly with water to form H2SO3 in the gas phase. For ground state SO2, this reaction is endothermic and has a very high activation barrier; our quantum chemical calculations point to a facile reaction being possible in the triplet state of SO2. This hygroscopic H2SO3 molecule may act as a condensation nucleus for water, giving rise to facile new particle formation (NPF).
机译:硫化学对几个行星的大气化学非常感兴趣。在水的存在下,氧化的硫会导致新的颗粒形成,从而对气候产生重大影响。与模型结果相比,对行星大气中含硫化合物的观察表明存在缺失的化学机理。在这里,我们提出了一种新的亚硫酸形成机理,它可以作为新颗粒形成的种子。在此机制中,SO2的最低三重态( 3 B1)可以通过近紫外太阳激发SO2进入其激发的 1 B1状态,然后再进入快速的系统间交换,直接与水反应形成气相的H2SO3。对于基态SO2,该反应是吸热的,具有很高的活化势垒。我们的量子化学计算表明,在SO2的三重态下,容易发生反应。这种具有吸湿性的H2SO3分子可以充当水的缩合核,从而形成新的粒子(NPF)。

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