Collaborative Proposal: Mineral Ballast and Organic Matter Compositions as Determinants of Particle Settling Velocities and Fluxes in the Sea (MedFlux)

合作提案：矿物压载物和有机物成分作为海洋中颗粒沉降速度和通量的决定因素 (MedFlux)

• 批准号: 0622754
• 负责人: Cindy Lee
• 金额: --
• 依托单位: SUNY at Stony Brook
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2006
• 资助国家: 美国
• 起止时间: 2006-09-01 至 2008-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0622754&HistoricalAwards=false
• 关键词: Collaborative; Proposal; Mineral; Ballast; Organic

ABSTRACTOCE-0622754 / OCE-0622930 / OCE-0623271With support from this grant, the members of the MedFlux research team at SUNY-Stony Brook, Skidaway Institute of Oceanography, and University of Washington will complete data analysis and informational synthesis their pioneering study of the fate of biogenic particles falling from the oceanic euphotic zone. The central focus of the MedFlux, which began with NSF support four years ago, is to develop a better mechanistic understanding of the "ballast hypothesis," which states that Particulate Organic Carbon (POC) fluxes to the deep ocean and sediments are directly proportional (3-7% OC by weight) to fluxes of "ballast minerals" produced by organisms (opal or carbonate minerals) or introduced into the surface ocean by physical processes. Earlier work (Armstrong et al. 2002; Klaas & Archer 2002) showed that the flux of organic carbon at depth can be predicted extremely well (85-90% explained variance) by ballast flux; the types and amounts of mineral ballast introduced to the surface ocean may therefore be critical determinants and predictors of the ocean's ability to take up and store carbon. To advance these studies, the research team also developed specialized sampling devices and protocols for measuring the two fundamental components of flux: particle concentration C(z) and average sinking velocity w ( z) at depth z. With funding under this grant, the team will be able to evaluate fully both the scientific output of the project as well as the performance of the new particulate sampling technology.This research has a number of broader impacts for for global carbon cycle and environmental change issues. For example, as pH decreases in response to the continued dissolution of anthropogenic carbon dioxide in the ocean, carbonate minerals may dissolve preferentially, affecting both ballasting and the average remineralization depth of POC in the ocean. This situation would necessitate a mechanism-based understanding of POC ballasting in the ocean. Additionally, MedFlux work will continue to foster international collaborations among three U.S. universities and colleagues in Monaco, France, Spain, and Geermany. The project also provides for the support and training of graduate students.

在这笔赠款的支持下，纽约州立大学石溪分校、斯基德韦海洋研究所和华盛顿大学的MedFlux研究小组成员将完成数据分析和信息合成，他们对从海洋真光带坠落的生物粒子的命运进行了开创性研究。MedFlux始于四年前NSF的支持，其中心焦点是更好地从机制上理解“压舱物假说”，该假说指出，进入深海和沉积物的颗粒有机碳(POC)通量与生物(蛋白石或碳酸盐矿物)产生的或通过物理过程引入表层海洋的“压舱物矿物”的通量成正比(有机碳重量的3-7%)。早期工作(阿姆斯特朗等人)2002年；Klaas&Amp；Archer 2002)表明，压载通量可以非常好地预测深海有机碳通量(解释方差的85-90%)；因此，引入表层海洋的矿物压载的类型和数量可能是海洋吸收和储存碳的能力的关键决定因素和预测因素。为了推进这些研究，研究小组还开发了专门的采样设备和方案，用于测量通量的两个基本组成部分：颗粒浓度C(Z)和深度z的平均下沉速度w(Z)。在这笔赠款的资助下，研究小组将能够充分评估项目的科学产出以及新颗粒采样技术的性能。这项研究对全球碳循环和环境变化问题具有许多更广泛的影响。例如，随着海洋中人为二氧化碳的持续溶解，pH下降，碳酸盐矿物可能优先溶解，从而影响海洋中POC的压载和平均再矿化深度。这种情况将需要对海洋中的压载POC进行基于机制的理解。此外，MedFlux的工作将继续促进摩纳哥、法国、西班牙和Geerany的三所美国大学和同事之间的国际合作。该项目还为研究生提供支持和培训。