Collaborative Research: Linking 3He/4He with eruptive behavior: A time series analysis of recent Kilauea, Iceland, and La Palma eruptions

约有8亿人生活在直接遭受火山灾害的地区，但火山爆发仍然难以预测。在某些情况下，地震和地面膨胀被用来预测即将发生的火山爆发。在其他情况下，火山气体排放的变化被用来推断火山活动的变化，因为气体排放被认为与火山爆发前火山下岩浆的上升有关。该项目探讨了火山气体化学可能包含有关岩浆补给的重要线索的可能性，这些线索可以帮助预测火山爆发的开始和过程。来自地球深处的岩浆富含3 He（一种氦的同位素，与4 He相比非常罕见）。因此，岩浆补给事件可能导致3 He相对于4 He的增加（即，高3 He/4 He）。这一假设将通过测量最近在夏威夷，冰岛和加那利群岛爆发的熔岩中的3 He/4 He值进行测试。通过将3 He/4 He与其他火山指标进行比较，包括熔岩排放率，熔岩成分，地震频率和震级以及卫星检测到的火山气体的其他化学特征，该团队将试图将3 He/4 He的变化与火山活动联系起来。如果氦的系统学因潜在危险的火山过程而改变，那么对火山进行实时氦监测可能是合理的。该项目不仅旨在扩大我们对火山系统的理解，还强调高中，本科和研究生教育。科学小组将与马萨诸塞州的布罗克顿新高地特许学校合作，开展与火山学有关的讲座和活动。伍兹霍尔海洋学研究所的两名本科生暑期研究员将从纽约城市大学（CUNY）招募，该大学拥有多样化的学生群体。另外两名纽约市立大学的本科生将通过开展独立的研究项目参加。一名就读于马萨诸塞州理工学院-伍兹霍尔海洋研究所联合项目的研究生将为研究的各个阶段做出贡献。这项工作将通过一个促进残疾人康复的伙伴组织为一名自闭症妇女提供就业机会。火山灾害预测仍然是火山学界面临的一个紧迫而难以捉摸的挑战。地震活动和地面变形监测往往很难与岩浆过程联系起来。综合监测方法最有希望，特别是那些用地球化学监测补充现有技术的方法。氦同位素在这方面显示出巨大的潜力，因为它们（i）对补给事件敏感，（ii）在火山喷发和休眠期间可以监测火山灰、土壤、地热沃茨和熔岩。此外，以前的工作表明，氦同位素（3 He/4 He）是敏感的岩浆补给事件从地幔。该项目的目标是在数周至数月的时间尺度上评估3 He/4 He变化的原因，以确定昂贵的实时氦同位素监测工作是否会改善火山灾害预测。这项研究将为最近的三次喷发产生岩浆3 He/4 He时间序列记录：夏威夷的Kallauea东部裂谷带（2018），冰岛的Fagradalsfjall（2021）和加那利群岛的Cumbre Vieja（2021）。岩浆氦将从单斜辉石和橄榄石矿物分离的熔岩样品跨越每次喷发。熔岩3 He/4 He，主要和微量元素丰度，放射性同位素和遥感数据，包括地面变形，地震活动，基于卫星的二氧化硫排放量和熔岩排放率的比较，将建立是否岩浆补给主要负责3 He/4 He的变化。或者，源的异质性或岩石圈氦同化可能占主导地位。通过调查多个监测良好的火山爆发，该项目将有可能确定火山爆发期间氦同位素变化的常见原因。该奖项反映了NSF的法定使命，并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，被认为值得支持。

Approximately 800 million people live in regions that are directly exposed to volcanic hazards, yet eruptions remain difficult to forecast. In some cases, earthquakes and ground swelling have been used to predict imminent volcanic eruptions. In other instances, changes in volcanic gas emissions have been used to infer changes in volcanic activity because gas emissions are thought to be linked to the ascent of magmas beneath volcanoes preceding eruptions. This project explores the possibility that volcanic gas chemistry might hold vital clues about magma recharge that could help forecast the onset and course of volcanic eruptions. Magmas from the deep Earth are rich in 3He (an isotope of helium that is very rare compared to 4He). Thus, magma recharge events may cause increases in 3He relative to 4He (i.e., higher 3He/4He). This hypothesis will be tested by measuring 3He/4He values in lavas from recent eruptions in Hawai’i, Iceland, and the Canary Islands. By comparing 3He/4He to other volcanic indicators, including lava discharge rate, lava composition, earthquake frequency and magnitude, and other chemical features of volcanic gases detected by satellites, the team will attempt to link changes in 3He/4He to volcanic activity. If helium systematics change in response to potentially hazardous volcanic processes, real-time helium monitoring of volcanoes may be justified. Not only does this project aim to broaden our understanding of volcanic systems, it also emphasizes high school, undergraduate, and graduate education. In partnership with the New Heights Charter School, in Brockton Massachusetts, the science team will develop lectures and activities relating to volcanology. Two undergraduate summer student fellows at Woods Hole Oceanographic Institution will be recruited from City University of New York (CUNY), which has a diverse student population. Two additional CUNY undergraduate students will participate by conducting independent study projects. One graduate student enrolled in the Massachusetts Institute of Technology-Woods Hole Oceanographic Institution Joint Program will contribute to all stages of the research. And this work will provide employment for an autistic woman through a partner organization that facilitates rehabilitation for individuals with disabilities.Volcanic hazard forecasting remains a pressing and elusive challenge for the volcanology community. Seismic activity and ground deformation monitoring are often difficult to link with magmatic processes. Integrative monitoring approaches show the most promise, especially those that supplement established techniques with geochemical monitoring. Helium isotopes show great potential in this regard because they (i) are sensitive to recharge events and (ii) can be monitored—in fumaroles, soils, geothermal waters, and lavas—during eruptions and during periods of repose. Furthermore, previous work indicates that helium isotopes (3He/4He) are sensitive to magma recharge events from the mantle. The goal of this project is to assess the causes of 3He/4He variability on timescales of weeks to months in order to determine whether costly real-time helium isotope monitoring efforts would improve volcanic hazard forecasting. This study will produce magmatic 3He/4He time series records for three recent eruptions: the Lower Eastern Rift Zone of Kīlauea in Hawaii (2018), Fagradalsfjall in Iceland (2021), and Cumbre Vieja in the Canary Islands (2021). Magmatic helium will be extracted from clinopyroxene and olivine mineral separates from lava samples spanning each eruption. Comparison of lava 3He/4He, major and trace element abundances, radiogenic isotopes, and remote sensing data—including ground deformation, seismicity, satellite-based SO2 emissions, and lava discharge rates—will establish whether magma recharge is principally responsible for 3He/4He variability. Alternatively, source heterogeneity or lithospheric helium assimilation might be dominant. By investigating multiple well-monitored eruptions, this project will potentially identify common causes of helium isotopic variability during volcanic eruptions.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.