紫外线对臭氧的形成和分解。三、二氯二氟甲烷对臭氧形成和分解的影响

F. Watanabe, O. Shimomura
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引用次数: 0

摘要

用低压汞蒸气石英灯照射紫外线,研究了二氯二氟甲烷(氟里昂12)对臭氧形成和分解的影响。本研究使用的灯为圆柱形15w,其主要光谱线为184.9 nm和253.7 nm。氟利昂气体被供应到三层结构管道的环形中间空间,该管道的中心有灯。然后,在紫外灯照射下,考察了氯浓度与氟利昂流量的关系。同样,向中间空间提供含有少量氟利昂气体的空气。测定了紫外线(184.9 nm)穿过氟利昂层后的强度。在进一步的实验中,氟利昂气体被供应到中间空间,臭氧的浓度保持恒定(10ppm)的空气被供应到管道的环形外部空间。然后,在紫外灯照射下,考察了分解率与气体流量的关系。结果表明:(1)臭氧不能单独被氟里昂分解。(2)氟利昂对波长253.7 nm的紫外线有很强的穿透能力,但对波长184.9 nm的紫外线很容易吸收,阻碍了臭氧的形成。当空气与体积%超过0.9的氟利昂气体混合时,不会形成臭氧。随着氟利昂流量的减小,臭氧的形成率逐渐增大,在0.025 vol%的情况下,臭氧的形成率可达90%。(3)氟里昂吸收波长为184.9 nm的紫外线,部分氟里昂分解后形成氯。在氟利昂气体流速为0.11 l/min的情况下,已知的最高氯浓度为900 ppm。所产生的氯的浓度与空气中氟利昂的比例成正比。(4)波长253.7 nm的紫外线穿过氟利昂层后,能够无阻碍地分解臭氧。也就是说,氟利昂本身并不影响这些紫外线对臭氧的分解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Formation and decomposition of ozone by ultraviolet rays. III : The influence of dichlorodifluoromethane on the formation and decomposition of ozone
The influence of dichlorodifluoromethane (freon 12) on the formation and decomposition of ozone by ultraviolet rays irradiated from a low pressure mercury vapor quartz lamp has been studied. The lamp used in this study was cylinder shaped 15 W and its main spectral lines were 184.9 nm and 253.7 nm. Freon gas was supplied to the annular middle space of a triple structure pipe that had the lamp in its center. Then, with ultraviolet rays irradiating from the lamp, the relationship between chlorine concentration and freon flow rate was examined. Likewise, air with a small amount of freon gas was supplied to the middle space. The intensity of ultraviolet rays (184.9 nm) after passing through the freon layer was also examined. In a further experiment, freon gas was supplied into the middle space and air with ozone whose concentration was kept constant (10 ppm) was supplied to the annular outside space of the pipe. Then, with ultraviolet rays irradiating from the lamp, the relationship between the decomposition ratio and the gas flow rate was examined. The following results were obtained : (1) Ozone is not decomposed by freon alone. (2) Freon is quite able to pass through 253.7 nm wavelength ultraviolet rays, but it hinders the formation of ozone by easily absorbing 184.9 nm wavelength ultraviolet rays. Ozone was not formed when air was mixed with freon gas of over 0.9 vol%. As the freon flow rate decreased, the formation rate of ozone gradually increased, up to 90% in the case of 0.025 vol%. (3) Freon absorbs 184.9 nm wavelength ultraviolet rays, and part of it forms chlorine after being decomposed. The highest chlorine concentrations recognized, in the case of a 0.11 l/min freon gas flow rate, was 900 ppm. The chlorine concentration produced was in proportion to the ratio of freon in the air. (4) After passing through the freon layer, 253.7 nm wavelength ultraviolet rays are able to decompose ozone without hindrance. That is to say, freon itself does not affect the decomposition of ozone by these ultraviolet rays.
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