ABR: Field, Laboratory, and Numerical Studies of Geyser Eruptions

ABR:间歇泉喷发的现场、实验室和数值研究

基本信息

  • 批准号:
    1724986
  • 负责人:
  • 金额:
    $ 26.42万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Standard Grant
  • 财政年份:
    2017
  • 资助国家:
    美国
  • 起止时间:
    2017-09-01 至 2022-08-31
  • 项目状态:
    已结题

项目摘要

Geysers are springs that intermittently erupt mixtures of steam and liquid water. They are popular tourist attractions, with a few million people watching geysers erupt in Yellowstone National Park each year. Geysers are the surface expression of geothermal systems and provide insight into heat and fluid flow in volcanically active areas. Geysers also provide a natural laboratory to study eruption processes and the geophysical and hydrological signals that can be measured before, during, and after an eruption. Because they are smaller than volcanic eruptions, and erupt more frequently, they provide an opportunity to collect abundant data and develop approaches for integrating and interpreting measurements. Geysers and their deposits have been studied to understand life in extreme environments. Geyser-like behavior of water and hydrocarbons has also been observed on the ocean floor and at mud volcanoes. Thus improved understanding of geyser behavior may yield understanding into other self-organized, intermittent processes in nature that result from localized input of energy and mass. Despite two centuries of scientific study, explanations for geysering phenomena are limited or lacking. This project will integrate field measurements, laboratory studies, and numerical simulations of multiphase flow in geyser systems to address the following basic questions about the geysering process: Why are geysers so rare? How does conduit plumbing affect eruption initiation and the interval between eruptions? Why and how do geysers interact with each other? Which external processes (e.g., tides, variations in barometric pressure, temperature variations, wind speed, earthquakes) and internal dynamics (e.g., duration of preceding eruption, plumbing geometry) influence the interval between and duration of eruptions? Answers to these questions may offer new insight into triggered seismicity, hydrothermal explosions, and volcanic eruptions.
间歇泉是间歇性喷出蒸汽和液态水混合物的泉水。它们是受欢迎的旅游景点,每年有数百万人在黄石国家公园观看间歇泉喷发。间歇泉是地热系统的地表表现形式,为了解火山活动区的热量和流体流动提供了依据。间歇泉也提供了一个自然实验室来研究喷发过程和地球物理和水文信号,这些信号可以在喷发之前、期间和之后测量。由于它们比火山喷发规模小,而且爆发频率更高,因此它们为收集大量数据和开发整合和解释测量结果的方法提供了机会。间歇泉及其沉积物已被研究以了解极端环境下的生命。在海底和泥火山上也观察到类似间歇泉的水和碳氢化合物的行为。因此,对间歇泉行为的更好理解可能会产生对自然界中其他自组织的间歇过程的理解,这些过程是由局部能量和质量输入引起的。尽管经过了两个世纪的科学研究,对间歇泉现象的解释仍然有限或缺乏。该项目将整合间歇泉系统中多相流的现场测量、实验室研究和数值模拟,以解决以下关于间歇泉过程的基本问题:为什么间歇泉如此罕见?管道管道如何影响火山爆发的开始和喷发之间的间隔?间歇泉为什么会相互作用,又是如何相互作用的?哪些外部过程(如潮汐、气压变化、温度变化、风速、地震)和内部动力学(如喷发前的持续时间、管道几何形状)会影响喷发的间隔和持续时间?这些问题的答案可能会为引发地震活动、热液爆炸和火山爆发提供新的见解。

项目成果

期刊论文数量(9)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Radiocarbon Dating of Silica Sinter and Postglacial Hydrothermal Activity in the El Tatio Geyser Field
El Tatio 间歇泉区二氧化硅烧结体和冰后热液活动的放射性碳测年
  • DOI:
    10.1029/2020gl087908
  • 发表时间:
    2020
  • 期刊:
  • 影响因子:
    5.2
  • 作者:
    Munoz‐Saez, Carolina;Manga, Michael;Hurwitz, Shaul;Slagter, Silvina;Churchill, Dakota M.;Reich, Martin;Damby, David;Morata, Diego
  • 通讯作者:
    Morata, Diego
The structure and volume of large geysers in Yellowstone National Park, USA and the mineralogy and chemistry of their silica sinter deposits
  • DOI:
    10.1016/j.jvolgeores.2021.107391
  • 发表时间:
    2021-09
  • 期刊:
  • 影响因子:
    2.9
  • 作者:
    D. Churchill;M. Manga;S. Hurwitz;S. Peek;D. Damby;R. Conrey;J. R. Wood;R. McCleskey;William E. Ke
  • 通讯作者:
    D. Churchill;M. Manga;S. Hurwitz;S. Peek;D. Damby;R. Conrey;J. R. Wood;R. McCleskey;William E. Ke
Dating silica sinter (geyserite): A cautionary tale
Origin and Properties of Hydrothermal Tremor at Lone Star Geyser, Yellowstone National Park, USA
美国黄石国家公园孤星间歇泉热液震颤的起源和特性
  • DOI:
    10.1029/2020jb019711
  • 发表时间:
    2020
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Nayak, Avinash;Manga, Michael;Hurwitz, Shaul;Namiki, Atsuko;Dawson, Phillip B.
  • 通讯作者:
    Dawson, Phillip B.
The Alpehue geyser field, Sollipulli Volcano, Chile
智利索利普利火山 Alpehue 间歇泉区
  • DOI:
    10.1016/j.jvolgeores.2020.107065
  • 发表时间:
    2020
  • 期刊:
  • 影响因子:
    2.9
  • 作者:
    Munoz-Saez, Carolina;Perez-Nuñez, Carolina;Martini, Sebastian;Vargas-Barrera, Alonso;Reich, Martin;Morata, Diego;Manga, Michael
  • 通讯作者:
    Manga, Michael
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Michael Manga其他文献

Exposed columns in the Valles Caldera ignimbrites as records of hydrothermal cooling, Jemez Mountains, New Mexico, USA
  • DOI:
    10.1016/j.jvolgeores.2022.107536
  • 发表时间:
    2022-06-01
  • 期刊:
  • 影响因子:
  • 作者:
    Stephen Self;Noah Randolph-Flagg;John E. Bailey;Michael Manga
  • 通讯作者:
    Michael Manga
A gas-tight shock tube apparatus for laboratory volcanic lightning under varying atmospheric conditions
用于不同大气条件下实验室火山闪电的气密激波管装置
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
  • 作者:
    ∗. ChristinaSpringsklee;B. Scheu;Christoph Seifert;Michael Manga;C. Cimarelli;Damian Gaudin;Oliver Trapp;Donald Bruce Dingwell
  • 通讯作者:
    Donald Bruce Dingwell
Fracture penetration in planetary ice shells
  • DOI:
    10.1016/j.icarus.2008.10.010
  • 发表时间:
    2009-02-01
  • 期刊:
  • 影响因子:
  • 作者:
    Maxwell L. Rudolph;Michael Manga
  • 通讯作者:
    Michael Manga
Strike-slip fault patterns on Europa: Obliquity or polar wander?
  • DOI:
    10.1016/j.icarus.2010.11.002
  • 发表时间:
    2011-01-01
  • 期刊:
  • 影响因子:
  • 作者:
    Alyssa Rose Rhoden;Terry A. Hurford;Michael Manga
  • 通讯作者:
    Michael Manga
The challenges of driving Charon's cryovolcanism from a freezing ocean
  • DOI:
    10.1016/j.icarus.2022.115391
  • 发表时间:
    2023-03-01
  • 期刊:
  • 影响因子:
  • 作者:
    Alyssa Rose Rhoden;Maxwell L. Rudolph;Michael Manga
  • 通讯作者:
    Michael Manga

Michael Manga的其他文献

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{{ truncateString('Michael Manga', 18)}}的其他基金

Particle clustering in dilute pyroclastic density currents and plumes
稀火山碎屑密度流和羽流中的颗粒聚集
  • 批准号:
    2042173
  • 财政年份:
    2021
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Continuing Grant
Collaborative Research: Subsurface plumbing, tremor migration, and eruption cycle of Yellowstone Geysers
合作研究:黄石间歇泉的地下管道、震颤迁移和喷发周期
  • 批准号:
    2116573
  • 财政年份:
    2021
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Standard Grant
EAGER Collaborative Research: Testing a new sensor for short term and long term measurement of heat flow in lakes
EAGER 协作研究:测试用于短期和长期测量湖泊热流的新传感器
  • 批准号:
    2041397
  • 财政年份:
    2020
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Standard Grant
Collaborative Research: Exploring the Magmatic, Crustal, and Conduit Conditions Required for Mafic, Plinian Volcanism
合作研究:探索镁铁质、普林尼式火山活动所需的岩浆、地壳和管道条件
  • 批准号:
    1831213
  • 财政年份:
    2018
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Standard Grant
Collaborative Research: Residual Stress Preserved in Crystals from Volcanic Eruptions
合作研究:火山喷发晶体中保存的残余应力
  • 批准号:
    1724469
  • 财政年份:
    2017
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Standard Grant
Collaborative Research: Flood volcanism and environmental impacts -- A multidisciplinary investigation of the Deccan Traps and events at the Cretaceous-Paleogene boundary
合作研究:洪水火山活动和环境影响——对德干地盾和白垩纪-古近纪边界事件的多学科调查
  • 批准号:
    1615203
  • 财政年份:
    2016
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Continuing Grant
Collaborative Proposal: Experimental Studies of Dilute Pyroclastic Density Currents
合作提案:稀火山碎屑密度流的实验研究
  • 批准号:
    1447559
  • 财政年份:
    2015
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Standard Grant
RAPID: Hydrological responses to the August, 2014, Napa earthquake
RAPID:2014 年 8 月纳帕地震的水文响应
  • 批准号:
    1463997
  • 财政年份:
    2015
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Standard Grant
Collaborative research: Origin of hydrologic responses to earthquakes: constraints from New Zealand, Taiwan, Chile, and USA
合作研究:地震水文响应的起源:新西兰、台湾、智利和美国的限制
  • 批准号:
    1344424
  • 财政年份:
    2014
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Continuing Grant
Collaborative Research: ABR: Multiscale Dynamics in Explosive Volcanic Eruptions
合作研究:ABR:火山喷发的多尺度动力学
  • 批准号:
    1144198
  • 财政年份:
    2012
  • 资助金额:
    $ 26.42万
  • 项目类别:
    Continuing Grant

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REU 站点:香农角海洋中心沿海海洋过程的现场和实验室研究
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