大气中的碳化合物,碳化合物和硫六化物:全球分布,来源和沉积点
概括
全球大气层的测量显示了碳的停留时间,表明没有缺失的水槽. 甲基甲酸盐数据表明基度较低,并突出其削弱平流层臭氧的潜力.
科学领域:
- 大气化学 大气化学
- 环境科学 环境科学
- 臭氧层研究 臭氧层研究
背景情况:
- 碳化合物,如碳-12和碳-11,是大气中的重要成分.
- 了解它们的分布和居住时间对于大气建模和臭氧消耗研究至关重要.
研究的目的:
- 为了确定碳-12和碳-11的半球间汇率和大气停留时间.
- 评估大气中基 (HO) 度及其分布.
- 评估甲基酸盐作为破坏臭氧层物质的作用,并确定甲基化物来源.
主要方法:
- 对碳-12和碳-11的全球分布数据的分析.
- 在大气中测量甲基化.
- 将观测数据与大气模型进行比较.
主要成果:
- 为碳化合物建立了一个半球间的1-1.2年汇率.
- 碳-12的确定大气停留时间为65-70年,碳-11的确定大气停留时间为40-45年.
- 表明全球平均基 (HO) 度 (3-4 x 10^5分子/cm3) 比模型预测的更低.
- 与北半球相比,在南半球观察到更高的HO水平.
- 确定海洋是大气中甲基化物的主要来源 (3 x 10^12 g/年).
结论:
- 碳化合物的确定的停留时间排除了显著的缺失水槽.
- 甲基甲的长期存在时间和生长速度对平流层臭氧层构成潜在威胁.
- 碳四化物海洋沉降是重要的,但平流层沉降更为重要.
- 海洋是大气中甲基化物的主要来源.
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