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DOI	10.1126/science.215.4533.665
	Carbonyl sulfide and carbon disulfide from the eruptions of Mount St. Helens
	Rasmussen R.A.; Khalil M.A.K.; Dalluge R.W.; Penkett S.A.; Jones B.
发表日期	1982
ISSN	0036-8075
起始页码	665
结束页码	667
卷号	215 期号:4533
英文摘要	Ash from the massive 18 May 1980 eruption of Mount St. Helens readily gave off large amounts of carbonyl sulfide and carbon disulfide gases at room temperature. These findings suggest that the sulfur that enhances the Junge sulfate layer in the stratosphere after volcanic eruptions could be carried directly to the upper atmosphere as carbonyl sulfide and carbon disulfide adsorbed on ash particles from major volcanic eruptions. Copyright © 1982 AAAS.
语种	英语
来源期刊	Science
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/245179
作者单位	Department of Environmental Science, Oregon Graduate Center, 19600 N. W. Walker Road, Beaverton, OR 97006, United States; Environmental and Medical Sciences Division, Atomic Energy Research Establishment, Harwell, Oxon OX11 ORA, United Kingdom
推荐引用方式 GB/T 7714	Rasmussen R.A.,Khalil M.A.K.,Dalluge R.W.,et al. Carbonyl sulfide and carbon disulfide from the eruptions of Mount St. Helens[J],1982,215(4533).
APA	Rasmussen R.A.,Khalil M.A.K.,Dalluge R.W.,Penkett S.A.,&Jones B..(1982).Carbonyl sulfide and carbon disulfide from the eruptions of Mount St. Helens.Science,215(4533).
MLA	Rasmussen R.A.,et al."Carbonyl sulfide and carbon disulfide from the eruptions of Mount St. Helens".Science 215.4533(1982).