Collaborative Research: Methane efflux from river influenced coastal marine sediments

合作研究:河流甲烷外流影响沿海海洋沉积物

基本信息

项目摘要

Collaborative Research: Methane efflux from river influenced coastal marine sedimentsMethane is a strong greenhouse gas and the amount of methane in the atmosphere is increasing. Large amounts of methane are present in sediments. Thus, understanding how much methane is released from sediments is a key first step for improving estimates of methane emissions. Coastal sediments are thought to be large sources of methane to the overlying water and potentially the atmosphere. Yet, fluxes of methane from coastal environments are poorly known. This project will measure methane fluxes from coastal sediments into the waters of the Gulf of Mexico. Methane is produced in sediments when microorganisms break down organic matter and from geological sources. However, the amount of methane released from sediments can be reduced by microorganisms that oxidize methane near the sediment surface where oxygen is present (aerobic oxidation) and deep in the sediment where oxygen is not present (anaerobic oxidation). This study focuses on environments where the aerobic oxidation of methane is the key process that prevents its release to the water column. Results from this project will help identify areas of the coastal ocean that are significant sources of methane release. This work is timely, as river-influenced marine sediments are sensitive to anthropogenic activities and global climate change. Scientists involved in this study will translate the findings into useful information for carbon cycle scientists, policy makers, students, teachers, and the public. They will work with education and outreach programs at Louisiana Universities Marine Consortium, University of Georgia, and Louisiana State University, and provide training to scientists from undergraduate to postgraduate levels.High sedimentation rates, like those found near rivers, can drive methane efflux from sediments, as evidenced by elevated methane concentrations in bottom waters. Observational data suggest that sediments from river influenced shallow shelf regions with low dissolved oxygen concentrations in the water column emit more methane to the water column than typical continental shelf sediments. This project combines benthic flux measurements, geochemistry and rate analysis into a reaction-transport model that will evaluate environmental influences on benthic processes. The team of scientists will measure benthic fluxes of oxygen and methane using an in situ lander, and sediment micro-profiles of oxygen and sulfide. Sedimentation and mixing rates will be determined using naturally occurring radioisotopes. Sulfate reduction and methane oxidation rates will be determined using radiotracers and a broad suite of contextual geochemical analysis will be performed. During two cruises off the southeastern coast of Louisiana, a total of 5 sites will be targeted. The data synthesis will help refine our understanding of the interactions between rivers, marine sediments, and methane releases from marine sediments. The project supports the development of an early career investigator and will provide training for one postdoctoral associate, two graduate students, three research assistants. This effort will leverage the LUMCON REU site program to support at least one student per year. The education goals emphasize informal education through outreach, formal education in the classroom, and authentic research experiences for community college students. Many of the activities emphasize the importance of communicating information to the scientific community, students, policy makers, and the general public.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:河流甲烷外流影响沿海海洋沉积物甲烷是一种强温室气体,大气中甲烷的含量正在增加。沉积物中存在大量甲烷。因此,了解沉积物中释放了多少甲烷是改进甲烷排放估算的关键的第一步。沿海沉积物被认为是上覆水域和大气中甲烷的主要来源。然而,人们对沿海环境的甲烷通量却知之甚少。该项目将测量从沿海沉积物进入墨西哥湾水域的甲烷通量。当微生物分解地质来源的有机物时,沉积物中会产生甲烷。然而,微生物可以减少沉积物中释放的甲烷量,这些微生物在存在氧气的沉积物表面附近(有氧氧化)和不存在氧气的沉积物深处(厌氧氧化)氧化甲烷。这项研究的重点是甲烷有氧氧化是防止其释放到水体中的关键过程的环境。该项目的结果将有助于确定沿海海洋区域是甲烷释放的重要来源。这项工作是及时的,因为受河流影响的海洋沉积物对人类活动和全球气候变化很敏感。参与这项研究的科学家将把研究结果转化为对碳循环科学家、政策制定者、学生、教师和公众有用的信息。他们将与路易斯安那大学海洋联盟、乔治亚大学和路易斯安那州立大学的教育和外展项目合作,为本科生到研究生的科学家提供培训。高沉积率,比如在河流附近发现的沉积率,可以推动甲烷从沉积物中流出,正如底层水中甲烷浓度升高所证明的那样。观测数据表明,来自河流的沉积物影响了水体中溶解氧浓度较低的浅陆架区域,比典型的大陆架沉积物向水体排放更多的甲烷。该项目将底栖通量测量、地球化学和速率分析结合到反应输运模型中,该模型将评估环境对底栖过程的影响。科学家团队将使用原位着陆器测量底栖氧气和甲烷通量,以及氧气和硫化物的沉积物微观剖面。沉积和混合速率将使用天然存在的放射性同位素来确定。将使用放射性示踪剂确定硫酸盐还原率和甲烷氧化率,并将进行广泛的背景地球化学分析。在路易斯安那州东南海岸附近的两次巡航中,共有 5 个地点将成为攻击目标。数据综合将有助于加深我们对河流、海洋沉积物和海洋沉积物甲烷释放之间相互作用的理解。该项目支持早期职业研究者的发展,并将为一名博士后、两名研究生和三名研究助理提供培训。这项工作将利用 LUMCON REU 站点计划每年支持至少一名学生。教育目标强调通过外展进行非正式教育、课堂上的正式教育以及为社区学院学生提供真实的研究经验。许多活动强调了向科学界、学生、政策制定者和公众传达信息的重要性。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。

项目成果

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Christof Meile其他文献

Christof Meile的其他文献

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{{ truncateString('Christof Meile', 18)}}的其他基金

Ridge 2000 Postdoctoral Fellowship Program: Reactive Transport Modeling of Biogeochemical Processes in a Hydrothermal Vent Field
Ridge 2000 博士后奖学金计划:热液喷口场生物地球化学过程的反应输运模型
  • 批准号:
    1039431
  • 财政年份:
    2010
  • 资助金额:
    $ 19.93万
  • 项目类别:
    Standard Grant
Collaborative Research: Outwelling of Dissolved Organic Carbon from Salt Marshes
合作研究:盐沼中溶解有机碳的流出
  • 批准号:
    0928140
  • 财政年份:
    2009
  • 资助金额:
    $ 19.93万
  • 项目类别:
    Standard Grant
Collaborative Research: Macrofaunal community effects on benthic exchange fluxes
合作研究:大型动物群落对底栖交换通量的影响
  • 批准号:
    0751882
  • 财政年份:
    2008
  • 资助金额:
    $ 19.93万
  • 项目类别:
    Standard Grant

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  • 批准号:
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    52370117
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    2023
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    50 万元
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    面上项目
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    22372177
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    2023
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    50 万元
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基于星地协同观测的煤矿聚集区甲烷排放反演方法研究
  • 批准号:
    42305138
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    2023
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    30 万元
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    青年科学基金项目
积碳利用功能化载氧体构筑及其等温甲烷化学链重整循环反应机理研究
  • 批准号:
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  • 项目类别:
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Collaborative Research: Bridging the scale gap between local and regional methane and carbon dioxide isotopic fluxes in the Arctic
合作研究:缩小北极当地和区域甲烷和二氧化碳同位素通量之间的规模差距
  • 批准号:
    2427291
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    2024
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Collaborative Research: Using New Ice Cores from Dome C to Test the Assumption of a Constant Galactic Cosmic Ray Flux and Improve Understanding of the Holocene Methane Budget
合作研究:利用 Dome C 的新冰芯测试银河系宇宙射线通量恒定的假设并提高对全新世甲烷收支的理解
  • 批准号:
    2146132
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    2023
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    $ 19.93万
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Collaborative Research: Using New Ice Cores from Dome C to Test the Assumption of a Constant Galactic Cosmic Ray Flux and Improve Understanding of the Holocene Methane Budget
合作研究:利用 Dome C 的新冰芯测试银河系宇宙射线通量恒定的假设并提高对全新世甲烷收支的理解
  • 批准号:
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Collaborative Research: NSF OCE-BSF: Coupling organic nutrient cycling to methane production in the oligotrophic North Pacific Ocean
合作研究:NSF OCE-BSF:将有机养分循环与贫营养北太平洋甲烷生产耦合
  • 批准号:
    2241668
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Collaborative Research: Using New Ice Cores from Dome C to Test the Assumption of a Constant Galactic Cosmic Ray Flux and Improve Understanding of the Holocene Methane Budget
合作研究:利用 Dome C 的新冰芯测试银河系宇宙射线通量恒定的假设并提高对全新世甲烷收支的理解
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    2146133
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    2023
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    $ 19.93万
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