概括
北极冬季的测量显示,大量的盐酸 (HCl) 损失与高一氧化物 (ClO) 水平相关. 这种转化发生在低温下,表明了对平流层分区的新见解.
科学领域:
- 大气化学 大气化学
- 石流层科学 石流层科学
背景情况:
- 极地平流层云 (PSC) 在平流层化学中起着至关重要的作用.
- 了解的激活和失活周期对于臭氧层研究至关重要.
研究的目的:
- 调查酸 (HCl) 和一氧化物 (ClO) 在北极冬季中之间的现场关系.
- 确定无机转化发生的条件.
主要方法:
- 同时在现场测量HCl和ClO.
- 分析空中飞行轨迹.
- 化学物种和温度的相关性分析.
主要成果:
- 观察到显著的HCl损失 (高达1ppbv),与高ClO度 (高达1.4ppbv) 相相关.
- 在低于196 +/- 4K的温度下发生的已识别的转换.
- 量化了HCl损失与ClO和Cl2O2度之间的关系.
结论:
- 在PSC颗粒上的异质反应HCl + ClONO2控制着分离.
- 平流层分离开始于过多的ClONO2,而不是HCl,挑战了以前的假设.
相关概念视频
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Precipitation of Ions
Predicting Precipitation
The equation that describes the equilibrium between solid calcium carbonate and its solvated ions is:
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