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Collaborative Research: Investigation Atomospheric Chemisty and Dynamics Through Oxygen and Sulfur Isotopes in Volcanic Sulfate from South Pole Ice Cores

Collaborative Research: Investigation Atomospheric Chemisty and Dynamics Through Oxygen and Sulfur Isotopes in Volcanic Sulfate from South Pole Ice Cores
合作研究:通过南极冰芯火山硫酸盐中的氧和硫同位素研究大气化学和动力学
批准号:
0338363
负责人:
Mark Thiemens
金额:
$8.69万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2004
资助国家:
美国
项目状态:
已结题
起止时间:
2004-05-01 至 2006-05-01

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中文摘要
翻译
该奖项支持南达科他州立大学(SDSU)和加州大学圣地亚哥分校(UCSD)之间的一项合作研究,以调查过去1000年来一些大型火山喷发中硫酸盐的氧和硫同位素组成。该项目的目标是在南极钻探一些浅冰芯,并将它们送回南加州大学和加州大学圣地亚哥分校的实验室进行化学和同位素分析。对南极冰雪几次火山喷发的硫酸盐样品的同位素测量的初步结果表明,火山硫酸盐的同位素组成包含了丰富的关于大气化学和动力学过程的有价值的信息,这些信息是以前没有研究过的。一个初步的结论是,与质量无关的分馏硫同位素表明,大气中硫化物的光解发生在比太古代大气更长的紫外线波长上,这可能反映了大气中的臭氧和/或氧气浓度。这表明,大气硫酸盐的同位素组成可用于了解紫外线辐射在大气中二氧化硫转化中的作用,并跟踪大气的演化(即氧化作用)和地球上生命的起源。其他主要研究目标包括了解大规模火山喷发对大气层的氧化能力有什么影响,在平流层将火山二氧化硫氧化或转化为硫酸盐涉及哪些氧化剂和机制,以及可用什么同位素标准来区分平流层喷发和对流层喷发的冰芯信号。通过为深南理工大学和加州大学圣迭戈分校的研究生和本科生提供教育和研究机会,拟议的项目将促进研究和教育的融合,并有助于科学和工程领域的人力资源开发。该项目将对SDSU拟议的REU化学现场计划做出贡献。此次合作将利用两个实验室的互补优势,促进两个机构之间的交流。国际合作将加强法国和美国之间的科学合作。
英文摘要
This award supports a collaborative study between South Dakota State University (SDSU) and University of California, San Diego (UCSD) to investigate the oxygen and sulfur isotope composition of sulfates from a number of large volcanic eruptions in the past 1000 years. The project aims to drill a number of shallow ice cores at South Pole and return them to SDSU and UCSD lab for chemical and isotope analysis. Preliminary results from measurements of isotopes in sulfate samples from several volcanic eruptions in Antarctic snow and ice indicate that isotopic composition of volcanic sulfate contains abundant valuable information on atmospheric chemical and dynamic processes that have not been previously investigated. One tentative conclusion is that mass-independently fractionated sulfur isotopes reveal that atmospheric photolysis of sulfur compounds occurs at longer UV wavelengths than those in the Archean atmosphere, possibly reflecting the atmospheric ozone and/or oxygen concentration. This suggests that isotopic composition of atmospheric sulfate may be used to understand the role of UV radiation in sulfur dioxide conversion in the atmosphere and to track the evolution (i.e., oxygenation) of the atmosphere and the origin of life on Earth. Other major research objectives include understanding what impact massive volcanic eruptions have on the oxidative capacity of the atmosphere, what oxidants and mechanisms are involved in the oxidation or conversion of volcanic sulfur dioxide to sulfate in the stratosphere and what isotopic criteria may be used to differentiate ice core signals of stratospheric eruptions from those of tropospheric eruptions. By providing educational and research opportunities to graduate and undergraduate students at both SDSU and UCSD, the proposed project will promote the integration of research and education and contribute to human resource development in science and engineering. The project will contribute to a proposed REU chemistry site program at SDSU. This collaboration will utilize the complementary strengths of both labs and promote exchange between the two institutions. International collaboration will enhance scientific cooperation between France and US.
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