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Fe Behavior and Bioavailability in Sub-aerial Runoff into the Ross Sea

Fe Behavior and Bioavailability in Sub-aerial Runoff into the Ross Sea
进入罗斯海的地下径流中铁的行为和生物利用度
批准号:
1841228
负责人:
W. Berry Lyons
金额:
$36.77万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2019
资助国家:
美国
项目状态:
已结题
起止时间:
2019-07-15 至 2024-06-30

项目摘要

项目成果

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中文摘要
翻译
浮游植物,或微小的海洋藻类,是碳循环的重要组成部分,可以通过将大气中的碳转移到海洋中来降低大气中二氧化碳的速率。南大洋浮游植物的浓度通常受到海洋铁的可用性的限制。这反过来又影响了从大气到海洋的碳转移速率。南大洋铁的主要来源是侵蚀的大陆岩石。了解目前和未来的铁的来源,南大洋的陆地冰川融化的结果增加是必要的,以预测未来的南大洋浮游植物的浓度和随后对碳循环的影响。对南大洋铁的一个知之甚少的来源是来自南极洲麦克默多干谷等无冰地区的水流输入。如果冰川退缩,这种铁的来源可能会变得更大。本研究调查的来源和数量的铁运输的麦克默多干谷流直接进入南大洋。由于并非所有形式的铁都能被浮游植物利用,因此将进行实验以确定浮游植物如何利用铁以及铁如何与海水混合。该项目的360度沉浸式视频、信息图表和教育视频将在社交媒体、学校和科学活动中以及城市科学中心分享。南大洋(SO)的大量营养素过剩,但由于铁的存在,区域初级生产受到限制或共同限制。海洋中加入铁会影响生物化学循环,增加初级生产力,并影响SO中浮游植物群落的结构和组成。铁通量的SO是全球性的显着,增加铁施肥导致增加碳封存,作为一个负反馈,增加大气pCO 2。SO沿海地区潜在的生物可利用铁的一个来源是南极洲无冰区的直接地下溪流排放,如果陆地冰川退缩,这一来源可能变得更加重要。如果要开发更好的碳循环和大气化学预测模型,就必须了解铁的来源、性质、潜在命运和通量。该项目将调查控制溶解铁排入罗斯海的流中过程和特征,包括光还原、温度和与有机物的络合。这项新的研究将量化颗粒铁的生物利用度和溶解铁的生物利用度,在南极洲的河流排入SO。将对溶解的铁物种进行现场形态测量,将使用高分辨率光谱法确定颗粒铁形态,将对沿海海水进行混合实验,并将通过海洋生物测定法确定铁的生物利用度。该项目将为两名学生提供宝贵的南极实地考察经验,并通过与K-12学校、公共STEM活动、城市科学中心和强大的社交媒体存在的现有合作关系接触数千人。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力审查标准进行评估,被认为值得支持。
英文摘要
Phytoplankton, or microscopic marine algae, are an important part of the carbon cycle and can lower the rates of atmospheric carbon dioxide by transferring the atmospheric carbon into the oceans. The concentration of phytoplankton in the Southern Ocean is regularly limited by the availability of marine iron. This in turn influences the rate of carbon transfer from the atmosphere to the ocean. The primary source of iron in the Southern Ocean is eroded continental rock. Understanding the current and future sources of iron to the Southern Ocean as a result of increased melting of terrestrial glaciers is necessary for predicting future concentrations of Southern Ocean phytoplankton and the subsequent influence on the carbon cycle. A poorly understood source of iron to the Southern Ocean is stream input from ice-free regions such as the McMurdo Dry Valleys in Antarctica. This source of iron is likely to become larger if glaciers retreat. This study investigates the sources and amount of iron transported by McMurdo Dry Valley streams directly into the Southern Ocean. Because not all forms of iron can be used by phytoplankton, experiments will be performed to determine how available iron is to phytoplankton and how iron mixes with seawater. Immersive 360-degree video, infographics, and educational videos of findings from this project will be shared on social media, at schools and science events, and in an urban science center.In the Southern Ocean (SO) there is an excess of macronutrients but regional primary production is limited or co-limited due to iron. An addition of iron to the ocean will affect biochemical cycles, increase primary production, and affect the structure and composition of phytoplankton communities in the SO. Iron flux to the SO is globally significant, as increased Fe fertilization leads to increased carbon sequestration which acts as a negative feedback to increased atmospheric pCO2. One source of potentially bioavailable iron to the coastal regions of the SO is from direct sub-aerial stream discharge in ice-free areas of Antarctica, a source that may become more important if terrestrial glaciers retreat. It is imperative to understand the source, nature, potential fate, and flux of iron to the SO if better predictive models for the carbon cycle and atmospheric chemistry are to be developed. This project will investigate in-stream processes and characteristics controlling dissolved iron draining into the Ross Sea including photoreduction, temperature, and complexation with organic matter. The novel study will quantify bioavailability of particulate iron and bioavailability of dissolved iron in Antarctic in streams draining into the SO. On-site speciation measurements will be performed on dissolved iron species, particulate iron speciation will be determined using high-resolution spectroscopy, mixing experiments will be performed with coastal marine water, and the bioavailability of Fe will be determined through marine bioassays. This project will provide two students with valuable Antarctic field experience and reach thousands of individuals through existing partnerships with K-12 schools, public STEM events, an urban science center, and a strong social media presence.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.
期刊论文(1)
专著(0)
科研奖励(0)
会议论文
Isotopic signature of massive, buried ice in eastern Taylor Valley, Antarctica: Implications for its origin
南极洲泰勒谷东部大量埋冰的同位素特征:对其起源的影响
DOI: 10.1080/15230430.2022.2102510
发表时间: 2022
期刊: and Alpine Research
影响因子: --
作者: [Gardner, Christopher B., Diaz, Melisa A., Smith, Devin F., Fountain, Andrew G., Levy, Joseph S., Lyons, W. Berry]
通讯作者: Lyons, W. Berry
U.S.-Ireland R&D Partnership: Sensor Application to Peatland Hydrology in Remote Environments (SAPHIRE)
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    2114028
  • 项目类别:
    Standard Grant
  • 资助金额:
    $34.98万
  • 财政年份:
    2021
  • 负责人:
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  • 项目类别:
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  • 负责人:
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    1543453
  • 项目类别:
    Standard Grant
  • 资助金额:
    $9.22万
  • 财政年份:
    2016
  • 负责人:
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  • 依托单位:
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  • 批准号:
    1341631
  • 项目类别:
    Standard Grant
  • 资助金额:
    $9.69万
  • 财政年份:
    2016
  • 负责人:
    W. Berry Lyons
  • 依托单位:
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  • 项目类别:
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  • 负责人:
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  • 依托单位:
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  • 批准号:
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  • 项目类别:
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  • 资助金额:
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  • 负责人:
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  • 依托单位: