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Carbonyl sulfide isotopologues: Ultraviolet absorption cross sections and stratospheric photolysis

机译:羰基硫同位素同位素:紫外吸收截面和平流层光解

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摘要

Ultraviolet absorption cross sections of the main and substituted carbonyl sulfide isotopologues were calculated using wavepacket dynamics. The calculated absorption cross section of~(16)O~(12)C~(32)S is in very good agreement with the accepted experimental spectrum between 190 and 250 nm. Relative to ~(16)O~(12)C~(32)S, isotopic substitution shows a significant enhancement of the cross section for ~(16)0~(13)C~(32)S, a significant reduction for ~(18)O~(12)C~( 32)S and ~(17)O~(12)C~(32)S and almost no change for the sulfur isotopologues ~(16)O~(12)C~( 33)S ~(16)O~(12)C~(34)S, and ~(16)O~(12)C ~(36)S The analysis of the initial wavepackets shows that these changes can be explained in terms of the change in the norm of the initial wavepacket. Implications for our understanding of the stratospheric sulfur cycle are discussed.
机译:利用波包动力学计算了主要和取代的羰基硫同位素同分异构体的紫外吸收截面。计算得出的〜(16)O〜(12)C〜(32)S的吸收截面与公认的190至250 nm实验光谱非常吻合。相对于〜(16)O〜(12)C〜(32)S,同位素置换显示〜(16)0〜(13)C〜(32)S的横截面显着增强,~~ 16 (18)O〜(12)C〜(32)S和〜(17)O〜(12)C〜(32)S,硫同位素~~(16)O〜(12)C〜( 33)S〜(16)O〜(12)C〜(34)S和〜(16)O〜(12)C〜(36)S对初始波包的分析表明,这些变化可以用术语解释初始wavepacket规范的变化。讨论了对我们理解平流层硫循环的意义。

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