Studies of the Production of Molecular Halogens in Arctic Snowpacks and on Sea Ice Surfaces

北极积雪和海冰表面分子卤素产生的研究

• 批准号: 1107695
• 负责人: Paul Shepson
• 金额: $ 52.7万
• 依托单位: Purdue University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-09-01 至 2014-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1107695&HistoricalAwards=false
• 关键词: Studies; Production; Molecular; Halogens; Arctic

This project would involve field experiments at Barrow, AK, aimed at improving understanding of the oxidation of the sea salt halides, chloride and bromide, into the molecular halogens, Cl2, BrCl, and Br2. In the Arctic at spring time there is a dramatic phenomenon characterized by the complete loss of ozone from the lowest layer of the atmosphere, along with near-complete loss of atmospheric elemental mercury. The elemental mercury is oxidized to short-lived products that then deposit to the surface, where it can enter and damage sensitive ecosystems. These ozone depletion episodes (ODEs) and mercury depletion episodes (MDEs) are known to occur as a result of halogen atom chemistry. However, the details of the halogen reactions that lead to the ODEs and MDEs are still unknown, limiting the ability to develop models that describe these processes, and how they might change in the future. It is thought that the processes that release molecular halogens are related to the presence of seasonal, or first-year (relatively thin and relatively saline), sea ice. The Arctic is currently experiencing a rapid decrease in the extent of multi-year sea ice, with associated increases in the extent of first-year sea ice. Thus the investigator hypothesizes that this halogen chemistry, and the associated potential impacts on atmospheric composition and deposition of mercury, will increase to the extent that the current trend in sea ice loss continues. To improve understanding of the fundamental processes associated with the production of molecular halogens in the Arctic, the investigator proposes an experiment involving exposures of natural snow samples and excised sea-ice samples in a snow chamber to potentially important atmospheric oxidants and measurement of the product molecular halogens. The investigator would also simultaneously conduct measurements of the concentrations of these compounds within the natural snowpack. He would then construct a detailed photochemical model of the chemistry involved with ODEs and MDEs, that could then be incorporated into larger scale Earth System climate and chemistry models to help enable reliable simulations of the future state of the Arctic atmosphere. The project would support a postdoctoral researcher and a graduate student. Numerous outreach activities would be supported through the Purdue Climate Change Research Center, interactions with the local community in Barrow, visits to schools, and through collaboration with adventure and children's book writer Peter Lourie on the web site arcticstories.net.

该项目将涉及在阿拉斯加州巴罗进行的实地实验，旨在提高对海盐卤化物、氯化物和溴化物氧化成分子卤素、Cl2、BrCl和Br2的认识。在春季的北极，有一种引人注目的现象，其特征是大气最低层的臭氧完全消失，同时沿着的是大气中元素汞几乎完全消失。元素汞被氧化成寿命短的产物，然后存款到地表，进入并破坏敏感的生态系统。已知这些臭氧消耗事件（ODE）和汞消耗事件（MDE）是卤素原子化学的结果。然而，导致ODE和MDE的卤素反应的细节仍然是未知的，限制了开发描述这些过程的模型的能力，以及它们在未来可能如何变化。据认为，释放分子卤素的过程与季节性海冰或第一年海冰（相对较薄且相对含盐）的存在有关。北极目前正经历多年海冰范围的迅速减少，第一年海冰范围相应增加。因此，研究人员假设，这种卤素化学，以及对大气成分和汞沉积的相关潜在影响，将增加到目前海冰损失趋势继续的程度。为了更好地了解与北极分子卤素产生相关的基本过程，研究人员提出了一项实验，涉及将天然雪样品和雪室中的海冰样品暴露于潜在的重要大气氧化剂和测量产品分子卤素。调查人员还将同时对自然积雪中这些化合物的浓度进行测量。然后，他将构建一个详细的光化学模型，该模型涉及ODE和MDE，然后可以将其纳入更大规模的地球系统气候和化学模型，以帮助对北极大气的未来状态进行可靠的模拟。该项目将资助一名博士后研究员和一名研究生。将通过普渡大学气候变化研究中心、与巴罗当地社区的互动、访问学校以及通过与冒险和儿童读物作家Peter Lourie在arcticstories.net网站上的合作，支持许多外联活动。