概括
实验室实验表明,酸在极地平流层云层表面容易发生反应,产生消耗臭氧层的气体. 这些反应还形成酸,这可能会进一步加速南极洲的臭氧破坏.
科学领域:
- 大气化学 大气化学
- 石流层科学 石流层科学
- 臭氧层消耗研究研究
背景情况:
- 极地平流层云 (PSCs) 在南极臭氧消耗中发挥着关键作用.
- 在PSC表面的异质反应有助于将稳定的化合物转化为反应形式.
- 了解这些反应对于预测臭氧层恢复至关重要.
研究的目的:
- 在模拟的PSC表面上研究涉及酸盐 (ClONO(2) 的关键异质反应的动力学和产物.
- 确定冰,酸 (HNO3) 冰和硫酸表面在这些反应中的作用.
- 评估这些反应对南极臭氧损耗的潜在贡献.
主要方法:
- 实验室实验模拟南极的平流层条件.
- 研究酸盐 (ClONO(2) 和水 (H(2) O) 或化 (HCl) 之间的反应.
- 在模仿PSC的表面进行反应:冰,HNO3冰和硫酸.
主要成果:
- ClONO(2) 很容易在冰面和HNO(3) 冰面上发生反应,在冰面上粘合系数为0.009 +/- 0.002.
- 反应产生了气相低酸 (HOCl) 和二氧化物 (Cl2) O,以及凝结相HNO3).
- ClONO(2) 与冰上的HCl发生反应,形成气相 (Cl(2) 和凝结相HNO(3),几乎完全消耗了HCl.
结论:
- 气态产物 (HOCl,Cl2O,Cl2) 可以通过光解产生活性,导致南极春季的臭氧层消耗.
- 凝结相HNO(3) 的形成起到气物种的沉积作用,阻止它们清理活性.
- 这些异质反应是对南极洲上空催化臭氧破坏周期的重要贡献者.
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