Development of New Techniques for Rock Deformation Using the Large Volume Torsion Apparatus

大体积扭转装置岩石变形新技术开发

基本信息

  • 批准号:
    2149427
  • 负责人:
  • 金额:
    $ 30.56万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    2022
  • 资助国家:
    美国
  • 起止时间:
    2022-07-01 至 2025-06-30
  • 项目状态:
    未结题

项目摘要

The field of rock deformation uses experimental devices to simulate the conditions in Earth’s interior by generating tremendous pressures, temperatures, and stresses. Deforming rocks in a laboratory setting allows researchers to control precisely the conditions that they impose, and test systematically the responses of rocks and minerals to these conditions. The data that are collected are used to better understand Earth’s structure, dynamics, and geologic hazards. For example, using rock deformation experiments scientists can determine the viscosity of rocks in Earth’s interior. These data, in turn, help us to understand why plate tectonics is found on Earth, but is absent on the other rocky planets of our solar system. This project supports development of a new type of rock deformation apparatus, in which specimens are subjected to torsional deformation. The particular capabilities of the Large Volume Torsion Apparatus (LVT2) enable experiments that reproduce conditions similar to those along boundaries between Earth’s tectonic plates.The LVT2 will be a uniquely capable tool for investigating the microphysics of rock deformation, rheology at plate boundaries, and the origins of seismic anisotropy in the crust and upper mantle. Previous support made possible the design and construction of the LVT2. This current project will allow the investigators, including a postdoctoral scholar, to (1) develop calibrations, techniques, and standard operating procedures, and (2) conduct preliminary experiments of scientific merit to evaluate the efficacy these procedures. Precise calibrations and robust standard operating procedures will yield a high level of safety and reliability, making rock deformation experiments more accessible to undergraduate students, external collaborators, and other short-term visitors. Support of a postdoctoral scholar will provide training to an early career scientists. Preliminary experiments to investigate the development of crystallographic preferred orientation will be used to better interpret seismic anisotropy in the mantle.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.
岩石变形领域使用实验设备,通过产生巨大的压力、温度和应力来模拟地球内部的条件。在实验室环境中使岩石变形使研究人员能够精确地控制他们施加的条件,并系统地测试岩石和矿物对这些条件的反应。收集的数据用于更好地了解地球的结构、动力学和地质灾害。例如,通过岩石变形实验,科学家可以确定地球内部岩石的粘度。反过来,这些数据帮助我们理解为什么在地球上发现了板块构造,而在我们太阳系的其他岩石行星上却没有。该项目支持开发一种新型的岩石变形装置,在该装置中,试件受到扭转变形。大体积扭转装置(LVT2)的特殊能力使实验能够重现类似于地球构造板块之间边界的条件。LVT2将是研究岩石变形、板块边界流变学以及地壳和上地幔地震各向异性起源的唯一有能力的工具。之前的支持使LVT2的设计和建造成为可能。这个目前的项目将允许研究人员,包括一名博士后学者,(1)开发校准、技术和标准操作程序,以及(2)进行具有科学价值的初步实验,以评估这些程序的有效性。精确的校准和强大的标准操作程序将产生高水平的安全性和可靠性,使本科生、外部合作者和其他短期访问者更容易接触到岩石变形实验。博士后学者的支持将为早期职业科学家提供培训。调查晶体择优取向发展的初步实验将被用来更好地解释地幔中的地震各向异性。这一奖项反映了NSF的法定使命,并通过使用基金会的智力优势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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Philip Skemer其他文献

Spatially-variable carbonation reactions in polycrystalline olivine
  • DOI:
    10.1016/j.gca.2017.02.003
  • 发表时间:
    2017-05-01
  • 期刊:
  • 影响因子:
  • 作者:
    Rachel K. Wells;Wei Xiong;Erika Sesti;Jinlei Cui;Daniel Giammar;Philip Skemer;Sophia E. Hayes;Mark S. Conradi
  • 通讯作者:
    Mark S. Conradi
Rheology of hydrous minerals in the subduction multisystem
  • DOI:
    10.1016/j.epsl.2024.119171
  • 发表时间:
    2025-02-01
  • 期刊:
  • 影响因子:
  • 作者:
    Charis M. Horn;Philip Skemer
  • 通讯作者:
    Philip Skemer

Philip Skemer的其他文献

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{{ truncateString('Philip Skemer', 18)}}的其他基金

REU Site: Collaborative Research: Research Opportunities in Rock Deformation
REU 网站:合作研究:岩石变形的研究机会
  • 批准号:
    2050372
  • 财政年份:
    2022
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
Collaborative Research: CSEDI: Integrating Seismic Anisotropy, Mantle Flow, and Rock Deformation in Subduction Zone Settings
合作研究:CSEDI:在俯冲带环境中整合地震各向异性、地幔流和岩石变形
  • 批准号:
    2153910
  • 财政年份:
    2022
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Continuing Grant
Acquisition of a Rock Deformation Apparatus to Study Rheology and Microstructure
购买岩石变形装置来研究流变学和微观结构
  • 批准号:
    1945763
  • 财政年份:
    2020
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
Collaborative Research: Theoretical and Experimental Investigation of Grain Damage and the Formation of Plate Boundaries
合作研究:颗粒损伤和板块边界形成的理论和实验研究
  • 批准号:
    1853155
  • 财政年份:
    2019
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
Rheology and microstructural evolution of serpentine
蛇纹石的流变学和微观结构演化
  • 批准号:
    1848824
  • 财政年份:
    2019
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
EarthCube Data Infrastructure: Collaborative Proposal: A unified experimental-natural digital data system for analysis of rock microstructures
EarthCube数据基础设施:协作提案:用于分析岩石微观结构的统一实验自然数字数据系统
  • 批准号:
    1639641
  • 财政年份:
    2017
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
Using Micromechanical Experiments to Investigate the Rheology of Geologic Materials
利用微观力学实验研究地质材料的流变性
  • 批准号:
    1726165
  • 财政年份:
    2017
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Continuing Grant
Conference on Experimental Studies of Subduction Zone Processes
俯冲带过程实验研究会议
  • 批准号:
    1757791
  • 财政年份:
    2017
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
Early Career: Development of a New Rock Deformation Apparatus for Investigating Earth's Upper Mantle
早期职业生涯:开发用于研究地球上地幔的新型岩石变形装置
  • 批准号:
    1360584
  • 财政年份:
    2014
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Standard Grant
CAREER: Microphysical evolution of highly sheared polymineralic rocks
职业:高剪切多矿物岩石的微物理演化
  • 批准号:
    1352306
  • 财政年份:
    2014
  • 资助金额:
    $ 30.56万
  • 项目类别:
    Continuing Grant

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