Collaborative Research: Seasonal variability in refractory dissolved organic carbon fluxes associated with primary marine aerosol emitted from the oceans

合作研究：与海洋排放的初级海洋气溶胶相关的难熔溶解有机碳通量的季节变化

• 批准号: 2023110
• 负责人: Amanda Frossard
• 金额: $ 27.22万
• 依托单位: University of Georgia Research Foundation Inc
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2020
• 资助国家: 美国
• 起止时间: 2020-09-01 至 2024-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2023110&HistoricalAwards=false
• 关键词: Collaborative; Research; Seasonal; variability; refractory

Collaborative Research: Seasonal variability in refractory dissolved organic carbon fluxes associated with primary marine aerosol emitted from the oceansThe oceans hold a massive quantity of organic carbon that is greater than all terrestrial organic carbon biomass combined. Nearly all marine organic carbon is dissolved. On average, it is thousands of years old, chemically stable, and carried throughout the entire ocean several times before complete removal. However, little is known about the processes that produce and remove this old carbon, referred to as refractory dissolved organic carbon (RDOC). One potential removal pathway involves RDOC adhering onto the surfaces of rising bubbles produced by breaking waves. The bubbles ultimately burst at the sea surface, ejecting tiny particles (primary marine aerosol, “PMA”) that carry the RDOC into the atmosphere. Most of this PMA organic carbon is associated with the smallest particles (less than 1 μm diameter) that drift in the atmosphere for several days to weeks. During this time, RDOC in these particles can be degraded photochemically (by sunlight), partially transported landward, and/or returned to the sea. When this RDOC is converted to inorganic carbon (e.g., carbon dioxide) or degraded to more reactive constituents in the atmosphere, it is effectively removed from the marine RDOC reservoir. Based on preliminary results, the annual rate at which RDOC is removed from the ocean by this process is similar to all other known RDOC losses (interactions with particles, biological degradation, and hydrothermal circulation), except for photochemical degradation in seawater. Building on this prior research, this project will identify seasonal changes in the removal of RDOC from the oceans through this process during three research cruises to the northwestern Atlantic Ocean. Results from this project will provide important findings about the coupled ocean-atmosphere loss of RDOC and improve understanding of the role of RDOC in the global carbon cycle and Earth's climate. The research will involve two early career faculty, and will provide training for undergraduate, graduate, and postdoctoral researchers.Radiocarbon (C-14) measurements indicate that RDOC comprises 19 to 40 % of the organic carbon associated with PMA produced by bursting bubbles at the sea surface. Injection of RDOC into the atmosphere in association with PMA is a potentially important process that removes as much as 2 to 20 Tg RDOC yr-1 from the oceans. This project will measure seasonal variations in the PMA-mediated emission of marine RDOC to the atmosphere by quantifying: (1) the fraction of RDOC in PMA OC and (2) its relationship to the abundance of biologically produced labile and semi-labile dissolved organic matter in near surface seawater. These relationships will be evaluated at the Bermuda Atlantic Time-series Station during three research cruises (one in July, two in January). During the cruises, the investigators will measure: (1) the natural abundance C-14 values for PMA and its organic source materials in seawater; (2) the dynamic and equilibrium surface tension and physical properties of seawater, including bubble size distributions; (3) concentrations of major ions, organic carbon, carbohydrates, peptides and proteins, and surfactants in PMA; and (4) chromophoric dissolved organic matter (CDOM) and the concentrations of dissolved organic carbon, chlorophyll a, major ions, carbohydrates, peptides and proteins, and surfactants in near-surface seawater and in the sea-surface microlayer. Based on these chemical measurements and physical properties, this study will reveal the magnitude and potential controls on RDOC inputs into the atmosphere as a component of PMA.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

合作研究：与海洋排放的初级海洋气溶胶相关的难溶有机碳通量的季节变化海洋中含有大量的有机碳，其数量大于所有陆地有机碳生物量的总和。平均而言，几乎所有海洋有机碳都被溶解。它已有数千年的历史，化学性质稳定，在完全清除之前会在整个海洋中多次携带。然而，人们对这种旧碳（称为难熔溶解有机碳）的产生和清除过程知之甚少。 (RDOC) 一种潜在的去除途径涉及 RDOC 粘附在波浪破碎产生的上升气泡表面上，气泡最终在海面破裂，喷射出微小颗粒（初级海洋气溶胶，“PMA”），将 RDOC 携带到海洋中。大气中大部分 PMA 有机碳与最小的颗粒（直径小于 1 μm）相关，这些颗粒在大气中漂移数天至数周，在此期间，这些颗粒中的 RDOC 会被光化学降解（通过光化学反应）。当该 RDOC 转化为无机碳（例如二氧化碳）或在大气中降解为更具活性的成分时，它会被有效地从海洋 RDOC 储存库中去除。根据初步结果，除海水中的光化学降解外，通过该过程从海洋中去除 RDOC 的年速率与所有其他已知的 RDOC 损失（与颗粒相互作用、生物降解和热液循环）相似。在先前研究的基础上，该项目将通过在西北大西洋的三次研究航行期间确定海洋中 RDOC 去除的季节变化，该项目的结果将提供有关 RDOC 海洋-大气耦合损失的重要发现。并加深对 RDOC 在全球碳循环和地球气候中的作用的了解。该研究将涉及两名早期职业教师，并将为本科生、研究生和博士后研究人员提供培训。放射性碳 (C-14) 测量表明 RDOC。含有 19% 至 40% 的与 PMA 相关的有机碳，这些有机碳是通过海面气泡破裂而产生的。将与 PMA 相关的 RDOC 注入大气中是一个潜在的重要过程，可从 PMA 中去除多达 2 至 20 Tg RDOC yr-1。该项目将通过量化以下内容来测量 PMA 介导的海洋 RDOC 排放的季节变化：(1) PMA OC 中 RDOC 的比例以及 (2) 其含量。与近地表海水中生物产生的不稳定和半不稳定溶解有机物丰度的关系将在百慕大大西洋时间序列站的三次研究航行期间（一次在七月，两次在一月）进行评估。 ，研究人员将测量：（1）海水中PMA及其有机源材料的自然丰度C-14值；（2）海水的动态和平衡表面张力和物理性质，包括气泡尺寸分布； ) 主要浓度PMA 中的离子、有机碳、碳水化合物、肽和蛋白质以及表面活性剂；以及 (4) 发色溶解有机物 (CDOM) 以及溶解的有机碳、叶绿素 A、主要离子、碳水化合物、肽和蛋白质以及表面活性剂的浓度；基于这些化学测量和物理特性，本研究将揭示 RDOC 作为大气成分的输入量的大小和潜在控制。 PMA。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。