Ingassing of Hydrogen in the Interiors of Sub-Neptunes and Gas Giants
亚海王星和气态巨行星内部的氢气吸收
基本信息
- 批准号:2108129
- 负责人:
- 金额:$ 32.06万
- 依托单位:
- 依托单位国家:美国
- 项目类别:Continuing Grant
- 财政年份:2021
- 资助国家:美国
- 起止时间:2021-08-01 至 2024-07-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
The interiors of large planets such as Jupiter, Saturn, or Neptune are at very high temperatures and pressures. The behavior at the boundary between hydrogen-rich atmospheres and mineral-rich cores under these conditions is not well understood. This project will perform experiments on Earth using high-pressure and high-temperature conditions to determine how hydrogen interacts and is possibly absorbed into the materials of the core. The results will help answer questions about the interiors and history of giant planets. The project will share their results through education at the university level as well as through public outreach events at Arizona State University.The project will use diamond anvil cells to subject silicates and iron metal alloys in hydrogen media to pressures up to 100 GPa and temperatures put to 4,600 K. The resulting reactions will be analyzed using time-resolution X-ray diffraction. The data from these experiments will help answer these key questions: (1) Can hydrogen be ingassed to the interiors through chemical reactions? (2) If ingassed, in what type of chemical forms would H exist (water, metal alloys, or hydrides)? (3) Can H ingassing alter the mass-radius relations of planets? and (4) Can such reactions be affected by the metallization of dense liquid hydrogen and therefore be planet size dependent? The project includes an undergraduate research program. Teaching modules for calculating mass-radius relations of planets will be developed and shared as an open-source teaching resource in public code repositories. Public outreach presentations will be made and campus-wide outreach events at Arizona State University.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.
木星、土星或海王星等大型行星的内部温度和压力都很高。在这些条件下,富氢大气和富矿岩芯之间的边界处的行为还没有得到很好的理解。该项目将利用高压和高温条件在地球上进行实验,以确定氢如何相互作用并可能被吸收到核心的材料中。这些结果将有助于回答有关巨行星内部和历史的问题。该项目将通过大学教育以及亚利桑那州立大学的公共宣传活动分享他们的成果。该项目将使用金刚石砧座单元使氢介质中的硅酸盐和铁金属合金承受高达100 GPa的压力和4,600 K的温度。将使用时间分辨率X射线衍射分析所产生的反应。这些实验的数据将有助于回答这些关键问题:(1)氢可以通过化学反应进入内部吗?(2)如果被吸入,氢会以什么样的化学形式存在(水、金属合金或氢)?(3)吸氢能改变行星的质量-半径关系吗?以及(4)这些反应是否会受到稠密液态氢金属化的影响,从而取决于行星的大小?该项目包括一个本科生研究计划。将开发用于计算行星质量-半径关系的教学模块,并将其作为公共代码库中的开放源码教学资源共享。公共宣传演讲将在亚利桑那州立大学进行,并在校园范围内开展宣传活动。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。
项目成果
期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Reaction between Hydrogen and Ferrous/Ferric Oxides at High Pressures and High Temperatures—Implications for Sub-Neptunes and Super-Earths
- DOI:10.3847/psj/acab03
- 发表时间:2023-02
- 期刊:
- 影响因子:0
- 作者:H. W. Horn;V. Prakapenka;S. Chariton;S. Speziale;S. Shim
- 通讯作者:H. W. Horn;V. Prakapenka;S. Chariton;S. Speziale;S. Shim
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Sang-Heon Shim其他文献
Continent-sized anomalous zones with low seismic velocity at the base of Earth's mantle
地幔底部具有低地震波速的大陆规模异常区
- DOI:
10.1038/ngeo2733 - 发表时间:
2016-06-20 - 期刊:
- 影响因子:16.100
- 作者:
Edward J. Garnero;Allen K. McNamara;Sang-Heon Shim - 通讯作者:
Sang-Heon Shim
Post-perovskite at ten
后钙钛矿在十
- DOI:
10.1038/ngeo2237 - 发表时间:
2014-08-28 - 期刊:
- 影响因子:16.100
- 作者:
Sang-Heon Shim;Thorne Lay - 通讯作者:
Thorne Lay
Raman spectroscopy and x-ray diffraction of phase transitions in Cr 2 O 3 to 61 GPa
- DOI:
10.1103/physrevb.69.144107 - 发表时间:
2004-04 - 期刊:
- 影响因子:3.7
- 作者:
Sang-Heon Shim - 通讯作者:
Sang-Heon Shim
Sang-Heon Shim的其他文献
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{{ truncateString('Sang-Heon Shim', 18)}}的其他基金
EA: Upgrade of the Laser Heating System in the High-Pressure Diamond-Anvil Cell Laboratory at Arizona State University
EA:亚利桑那州立大学高压金刚石砧室实验室激光加热系统升级
- 批准号:
2335071 - 财政年份:2024
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Collaborative Research: From Silicate Melts Properties to the Dynamics and Evolution of an Early Basal Magma Ocean
合作研究:从硅酸盐熔体特性到早期基底岩浆洋的动力学和演化
- 批准号:
2153968 - 财政年份:2022
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Upgrade of the Raman Spectroscopy System at the High-Pressure Lab of Arizona State University
亚利桑那州立大学高压实验室拉曼光谱系统升级
- 批准号:
2140416 - 财政年份:2022
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Possible Storage of H2O in Mantle Ca(Ti,Si)O3 Perovskite
地幔 Ca(Ti,Si)O3 钙钛矿中 H2O 的可能储存
- 批准号:
2019565 - 财政年份:2020
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Effect of Hydrogen on the Sulfur-rich Martian Core
氢对富含硫的火星核心的影响
- 批准号:
2005567 - 财政年份:2020
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Effect of Hydrogen on the Properties of Fe alloys in the Earth's Core
氢对地核铁合金性能的影响
- 批准号:
1921298 - 财政年份:2019
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Calcium in Bridgmanite in the Deep Mantle
深部地幔布里奇曼石中的钙
- 批准号:
1725094 - 财政年份:2017
- 资助金额:
$ 32.06万 - 项目类别:
Standard Grant
Understanding the complexity of the 660-km seismic discontinuity
了解 660 公里地震间断面的复杂性
- 批准号:
1316007 - 财政年份:2012
- 资助金额:
$ 32.06万 - 项目类别:
Continuing Grant
The Perovskite to Post-Perovskite Phase Boundary in Mantle Rocks
地幔岩石中的钙钛矿到后钙钛矿相边界
- 批准号:
1301813 - 财政年份:2012
- 资助金额:
$ 32.06万 - 项目类别:
Continuing Grant
CSEDI Collaborative Research: Valence state of iron in the lower mantle
CSEDI合作研究:下地幔铁的价态
- 批准号:
1316022 - 财政年份:2012
- 资助金额:
$ 32.06万 - 项目类别:
Continuing Grant
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