碳硫化物和二硫化碳来自圣海伦斯山喷发的喷发
概括
圣海伦斯山的火山灰释放出大量的硫化碳和二硫化碳气体. 这表明富含硫的气体吸附在灰颗粒上,在重大喷发后直接到达平流层.
科学领域:
- 地质化学 地质化学
- 大气化学 大气化学
- 火山学 火山学是一门学科.
背景情况:
- 众所周知,火山喷发会影响平流层的气溶层.
- 格硫酸盐层是平流层的一个关键组成部分.
- 爆发后将硫输送到平流层的精确机制需要进一步阐明.
研究的目的:
- 在环境温度下研究火山灰的气体释放特性.
- 为了确定碳硫化物和二硫化碳是否从圣赫伦斯山灰中释放出来.
- 通过火山灰提出一个通过火山灰直接运输平流层硫的机制.
主要方法:
- 对圣赫伦斯火山火山灰发出的气体进行分析.
- 室温实验测量释放的气体.
主要成果:
- 1980年圣海伦斯火山爆发的灰随时在室温下释放出大量的碳硫化物 (COS) 和二硫化碳 (CS2).
- 观察到这些气体被吸附在灰尘颗粒上.
结论:
- 在火山灰颗粒上吸附的硫化碳和二硫化碳可以直接运送到平流层.
- 这种机制为硫提供了一条途径,在重大火山爆发后增强Junge硫酸盐层.
相关概念视频
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