Collaborative Research: Paleoproxies and Benthic Fluxes - Establishing the Bottom Boundary Relationships for Ba, U, Mo and Ge

合作研究：古代理和底栖通量 - 建立 Ba、U、Mo 和 Ge 的底部边界关系

• 批准号: 0095064
• 负责人: Philip Froelich
• 金额: $ 13万
• 依托单位: Georgia Tech Research Corporation
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2001
• 资助国家: 美国
• 起止时间: 2001-05-15 至 2004-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0095064&HistoricalAwards=false
• 关键词: Collaborative; Research; Paleoproxies; Benthic; Fluxes

The PIs will measure trace elements (Ba, U, Mo, Mn, and Ge) in Jahnke's existing benthic flux chamber samples dating back to 1997. The goal is to establish bottom boundary conditions governing the regeneration and burial of several tracers used to interpret past ocean chemistry, circulation, productivity, carbon flux and redox conditions. Existing sites include a wide variety of oceanic environments. The samples will be screened with low-precision ICP-MS methods and subsets of selected samples will be analyzed with high-precision ID-ICP-MS. Selected pore water samples will also be screened and analyzed. These data will be used to understand processes controlling transfer across the sediment-water interface and quantitative relationships with other parameters.

PI将在Jahnke现有的底栖通量室样品中测量痕量元素（BA，U，MO，MN和GE），其历史可以追溯到1997年。目的是建立底部边界条件，用于处理几个示踪剂的底部边界条件，用于解释过去的几个示踪剂，用于解释过去的海洋化学，循环，生产力，碳通量和氧化还原条件。现有地点包括各种各样的海洋环境。样品将使用低精确的ICP-MS方法筛选，并且将使用高精度ID-ICP-MS分析所选样品的子集。选定的孔隙水样品还将进行筛选和分析。这些数据将用于了解控制跨沉积物 - 水接口转移的过程以及与其他参数的定量关系。