Low temperature hydrothermal vent fluxes as traced by radium isotopes

镭同位素追踪的低温热液喷口通量

• 批准号: 1829431
• 负责人: Matthew Charette
• 金额: $ 35.03万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2018
• 资助国家: 美国
• 起止时间: 2018-11-01 至 2023-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1829431&HistoricalAwards=false
• 关键词: Low; temperature; hydrothermal; vent; fluxes

Iron is one of the most abundant elements in fluids released from mid-ocean ridges, yet it has been thought to be mostly removed from seawater near to its hydrothermal vent source. Recent evidence has emerged showing this hydrothermally-derived iron can be transported great distances in the ocean, including toward the sunlit surface layer where it is an essential nutrient for phytoplankton growth. This study will use naturally-occurring radium isotopes, which are also enriched in hydrothermal fluids but are non-reactive compared to iron, as tracers of hydrothermal iron in the deep ocean. With a range of half-lives from days to centuries, radium isotopes can be used as "clocks" to measure the precise rates at which hydrothermal iron is carried by ocean currents toward the ocean interior. Such information can be incorporated into ocean models designed to determine the role of hydrothermal iron on ocean productivity, which has societal relevance due to its role in regulating the carbon dioxide concentrations of Earth's atmosphere. This project will support research opportunities for two students through the Woods Hole Partnership in Education Program, which seeks to increase diversity in ocean and environmental science by inviting college juniors and seniors to gain practical experience through a summer of classroom study and hands-on research activities.A scientist from Woods Hole Oceanographic Institution will quantify rates of iron (Fe) transport above a major ocean spreading center to evaluate the role of hydrothermal venting in supplying this essential micronutrient to the surface ocean. Special attention will be paid to the role of low-temperature hydrothermal Fe fluxes, which are hypothesized to arrive at the seafloor in a stable form that mitigates significant removal during transport. If true, low-temperature fluids may supply a disproportionate amount of the "transportable" dissolved Fe that has not been observed in large-scale deep ocean plumes. Assessment of process rates will be accomplished through concurrent measurements of Fe concentration and speciation and the radium (Ra) "quartet" (224Ra, 223Ra, 228Ra, 226Ra) during an expedition along the southern East Pacific Rise (EPR; 15-18 degrees South). Autonomous underwater vehicle and towed-CTD surveys will be used to identify locations of low- and high-temperature discharge. At selected target areas, the investigators will test the hypotheses that low-temperature hydrothermal inputs have a distinct radium isotopic ratio fingerprint, and that the relative rate of Fe scavenging removal is lower in low-temperature sources. Given their wide ranging half-lives, Ra isotopes have the unique ability to integrate over biogeochemically-relevant time scales of Fe transport in the deep ocean. The combination of concurrent Ra isotope and total dissolved Fe measurements will allow the investigators to quantify Fe residence time for any Fe phase that is transported on large horizontal scales, as has been observed previously along the EPR. Together, Fe loss and transport from Ra measurements will lead to improvements in the predictive capabilities of ocean circulation and biogeochemistry models that assess the importance of hydrothermal Fe in supporting primary productivity and carbon drawdown in overlying surface waters.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.

铁是大洋中脊释放的流体中含量最丰富的元素之一，但人们一直认为，铁主要是从热液喷口源附近的海水中去除的。最近的证据表明，这种水热衍生的铁可以在海洋中被运输到很远的地方，包括朝向阳光照射的表层，在那里它是浮游植物生长的必需营养素。这项研究将使用天然存在的镭同位素作为深海热液铁的示踪剂，镭同位素也在热液流体中富集，但与铁相比不起反应。镭同位素的半衰期从几天到几个世纪不等，可以用作“时钟”来测量热液铁被洋流带到海洋内部的精确速率。这些信息可以纳入海洋模型，以确定热液铁对海洋生产力的作用，由于其在调节地球大气层二氧化碳浓度方面的作用，这具有社会意义。该项目将通过伍兹霍尔教育项目伙伴关系为两名学生提供研究机会，该项目旨在通过邀请大学三年级和四年级学生通过暑期的课堂学习和实践研究活动来获得实践经验，从而增加海洋和环境科学的多样性。在一个主要的海洋扩张中心上方进行了一次迁移，以评估热液喷口在向海洋表面提供这种必需微量营养素方面的作用。将特别关注低温热液铁通量的作用，假设这些铁通量以稳定的形式到达海底，减少运输过程中的大量去除。如果这是真的，低温流体可能会提供不成比例的“可运输”溶解铁，这在大规模深海羽流中还没有观察到。在沿着南东太平洋海隆（EPR;南纬15-18度）进行考察期间，将通过同时测量铁浓度和形态以及镭（Ra）“四重态”（224 Ra、223 Ra、228 Ra、226 Ra）来完成对过程速率的评估。将使用自主水下航行器和拖曳式CTD勘测来确定低温和高温排放的位置。在选定的目标区域，研究人员将测试以下假设：低温热液输入具有明显的镭同位素比指纹，低温源中Fe清除去除的相对速率较低。鉴于其广泛的半衰期，Ra同位素具有独特的能力，可以整合深海中Fe运输的生物地球化学相关时间尺度。同时Ra同位素和总溶解铁测量的组合将允许调查人员量化铁停留时间的任何铁相，是在大的水平尺度上运输，如先前已观察到的沿着EPR。总的来说，Ra测量的铁损失和运输将导致海洋环流和海洋地球化学模型的预测能力的提高，这些模型评估热液铁在支持初级生产力和覆盖地表沃茨的碳下降方面的重要性。该奖项反映了NSF的法定使命，并被认为值得通过使用基金会的知识价值和更广泛的影响审查标准进行评估来支持。