Collaborative Research: Salt Rock Microstructure and Deformation

合作研究:盐岩微观结构与变形

基本信息

  • 批准号:
    1361996
  • 负责人:
  • 金额:
    $ 19.95万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Standard Grant
  • 财政年份:
    2014
  • 资助国家:
    美国
  • 起止时间:
    2014-09-01 至 2018-08-31
  • 项目状态:
    已结题

项目摘要

Salt rock is used for secure storage of oil, high-pressure gas, and nuclear waste because of its ability to creep and form barriers to gas and fluid flow. However, creep processes near subsurface storage facilities can lead to crack debonding, opening, closure and rebonding that compromise the integrity of flow barriers and stability of engineered structures. Mathematical descriptions of cracking and healing are incompletely developed. This award will support fundamental rock physics and mechanics research to link deformation by crack debonding, opening and rebonding to microstructures and mechanical variables that govern the time-dependent behavior of salt rock over geological space and time scales. Deformation of salt occurs rapidly at laboratory conditions making it a good analog to study damage and healing in other crystalline materials and porous media. Project findings are expected to advance quantitative relations enabling accurate modeling and prediction of behaviors in engineering projects. The work will advance fundamental understanding of cracking and healing in other rocks that deform by the same processes, especially around earthquake faults and zones of induced seismicity. The team of geoscience and engineering researchers will collaborate with other programs to broaden the participation of women and other under-represented groups in research and engineering.Most continuum damage models for salt are based on the concept of dilatancy boundary, and do not account for crack-induced anisotropy of elastic properties. Micro-mechanics and homogenization principles were successfully employed to model salt rock elastoplastic behavior, but were not used to test scale invariance of microstructure to transitions in deformation regimes. The goal of this project is to link salt deformation regimes and rheological behaviors with the density and orientation distribution of microstructures. Deformation regimes at the scale of a Representative Elementary Volume will be decomposed into independent processes (e.g., cracking), each related to different microstructure descriptors (e.g., grain aspect ratio). Macroscopic thermodynamic variables will be formally related to the microstructure descriptors to test the space and time scale invariance of transition points in deformation regimes. Specific research objectives are to: (1) Identify topological components and subcomponents of salt microstructure; (2) Determine the energy cost of intra- and inter-granular crack debonding, opening, closure and rebonding; (3) Compute energy thresholds associated with transitions between deformation regimes at the grain and REV scales; (4) Test the time and scale dependence of microstructure organization during transitions; (5) Design rock salt microstructural systems that optimize healing properties in subsurface storage environments.
盐岩用于石油、高压气体和核废料的安全储存,因为它具有蠕变能力,并对气体和流体流动形成屏障。 然而,地下储存设施附近的蠕变过程可能导致裂纹脱粘、打开、闭合和重新粘结,从而损害流动屏障的完整性和工程结构的稳定性。 对裂纹和愈合的数学描述还不完全。 该奖项将支持基础岩石物理和力学研究,将裂缝脱粘,打开和重新粘合的变形与微观结构和力学变量联系起来,这些变量控制着盐岩在地质空间和时间尺度上的时间依赖行为。 盐的变形在实验室条件下迅速发生,使其成为研究其他晶体材料和多孔介质中损伤和愈合的良好模拟物。 预计项目结果将推进定量关系,使工程项目中的行为准确建模和预测。 这项工作将促进对其他岩石中通过相同过程变形的开裂和愈合的基本理解,特别是在地震断层和诱发地震活动区周围。 地球科学和工程研究人员团队将与其他项目合作,以扩大妇女和其他代表性不足的群体在研究和工程中的参与。大多数盐的连续介质损伤模型都是基于非线性边界的概念,并且没有考虑裂纹引起的弹性属性的各向异性。细观力学和均匀化原理被成功地用于模拟盐岩弹塑性行为,但没有被用来测试变形机制中微观结构的尺度不变性。该项目的目标是将盐变形机制和流变行为与微观结构的密度和取向分布联系起来。在代表性基本体积的尺度下的变形机制将被分解成独立的过程(例如,开裂),每种都与不同的微结构描述符有关(例如,晶粒纵横比)。宏观热力学变量将正式相关的微观结构描述符,以测试变形制度的转变点的空间和时间尺度的不变性。具体的研究目标是:(1)确定盐微观结构的拓扑成分和子成分;(2)确定晶内和晶间裂纹脱粘、张开、闭合和再结合的能量消耗;(3)计算与晶粒和REV尺度下变形状态之间转变相关的能量阈值;(4)测试转变过程中微观结构组织的时间和尺度依赖性;(5)设计岩盐微结构系统,优化地下储存环境中的愈合性能。

项目成果

期刊论文数量(10)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Coupled Brittle and Viscous Micromechanisms Produce Semibrittle Flow, Grain‐Boundary Sliding, and Anelasticity in Salt‐Rock
  • DOI:
    10.1029/2020jb021261
  • 发表时间:
    2021-01
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Ji-hui Ding;F. Chester;J. Chester;Xianda Shen;C. Arson
  • 通讯作者:
    Ji-hui Ding;F. Chester;J. Chester;Xianda Shen;C. Arson
Mechanisms of Anisotropy in Salt Rock Upon Microcrack Propagation
  • DOI:
    10.1007/s00603-020-02096-1
  • 发表时间:
    2020-04
  • 期刊:
  • 影响因子:
    6.2
  • 作者:
    Xianda Shen;C. Arson;Ji-hui Ding;F. Chester;J. Chester
  • 通讯作者:
    Xianda Shen;C. Arson;Ji-hui Ding;F. Chester;J. Chester
Mechanical behavior and microstructure development in consolidation of nominally dry granular salt
名义干燥颗粒盐固结的力学行为和微观结构发展
Experimental characterization of microstructure development for calculating fabric and stiffness tensors in salt rock
用于计算盐岩中的织物和刚度张量的微观结构开发的实验表征
Micro-mechanical analysis of salt creep tests with a joint-enriched Finite Element model
使用联合丰富的有限元模型对盐蠕变试验进行微观力学分析
  • DOI:
  • 发表时间:
    2016
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Zhu, C.;Pouya, A.;Arson, C.;Ding, J.;Chester, F.M.;Chester, J.S.
  • 通讯作者:
    Chester, J.S.
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Frederick Chester其他文献

Evidence for high frictional heat at a shallow portion of the faults, Tonankai earthquake rupture area
东南海地震破裂区断层浅部存在高摩擦热的证据
  • DOI:
  • 发表时间:
    2010
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Arito Sakaguchi;Frederick Chester;Daniel Curewitz et al
  • 通讯作者:
    Daniel Curewitz et al
Frictional high heat at shallow portion of the mega-splay fault and frontal thrust : Core analysis of IODP NanTroSEIZE stage 1
大张断层浅部摩擦高热和锋面逆冲:IODP NanTroSEIZE 阶段 1 的核心分析
  • DOI:
  • 发表时间:
    2010
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Arito Sakaguchi;Frederick Chester;Daniel Curewitz et al
  • 通讯作者:
    Daniel Curewitz et al
Trace element and isotope characteristics of core samples from the Japan Trench Fast Drilling Project (JFAST)
日本海沟快速钻探项目(JFAST)岩心样品的微量元素和同位素特征
  • DOI:
  • 发表时间:
    2014
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Tsuyoshi Ishikawa;Jun Matsuoka;Jun Kameda;James Mori;Frederick Chester
  • 通讯作者:
    Frederick Chester
北太平洋の回帰線水の形成域における塩分の季節・経年変動とそのメカニズム
北太平洋回归线水形成区盐度的季节和年际变化及其机制
  • DOI:
  • 发表时间:
    2011
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Arito Sakaguchi;Frederick Chester;Daniel Curewitz et al;桂将太・岡英太郎
  • 通讯作者:
    桂将太・岡英太郎
太陽風プロトンの月面散乱における散乱角依存性
月球表面太阳风质子散射的散射角依赖性
  • DOI:
  • 发表时间:
    2011
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Arito Sakaguchi;Frederick Chester;Daniel Curewitz;Olivier Fabbri;David Goldsby;Gaku Kimura;Chun-Feng Li;Yuka Masaki;Elizabeth Screnton;Akito Tsutsumi;Kohtaro Ujiie;Asuka Yamaguchi;上村洸太,齋藤義文,西野真木,横田勝一郎,浅村和史,綱川秀夫
  • 通讯作者:
    上村洸太,齋藤義文,西野真木,横田勝一郎,浅村和史,綱川秀夫

Frederick Chester的其他文献

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{{ truncateString('Frederick Chester', 18)}}的其他基金

MRI: Development of a high pressure and temperature, biaxial deformation apparatus for earthquake and landslide studies
MRI:开发用于地震和滑坡研究的高压高温双轴变形装置
  • 批准号:
    1126762
  • 财政年份:
    2011
  • 资助金额:
    $ 19.95万
  • 项目类别:
    Standard Grant
Experimental and Petrofabric Study of Hybrid Fractures and the Transition From Joints to Faults
混合裂缝以及节理到断层转变的实验和岩石组构研究
  • 批准号:
    0310284
  • 财政年份:
    2003
  • 资助金额:
    $ 19.95万
  • 项目类别:
    Continuing Grant
Collaborative Research: Seismic Failure Processes of Intersecting Intraplate Faults Using Microearthquake Clusters
合作研究:利用微震群研究板内相交断层的地震破坏过程
  • 批准号:
    9614463
  • 财政年份:
    1997
  • 资助金额:
    $ 19.95万
  • 项目类别:
    Standard Grant
Upgrading the Rock Mechanics Laboratory at Saint Louis University
升级圣路易斯大学岩石力学实验室
  • 批准号:
    9117415
  • 财政年份:
    1992
  • 资助金额:
    $ 19.95万
  • 项目类别:
    Standard Grant
COLLABORATIVE RESEARCH: Weakening and Slip Mechanisms in Large-Displacement Faults of the San Andreas System; Characterization and Experimental Investigations
合作研究:圣安德烈亚斯系统大位移断层的弱化和滑动机制;
  • 批准号:
    9205973
  • 财政年份:
    1992
  • 资助金额:
    $ 19.95万
  • 项目类别:
    Standard Grant
Paleostress and Mechanisms of Slip on the San Gabriel Fault,San Andreas Fault System, California
加利福尼亚州圣安德烈亚斯断层系圣盖博断层的古应力和滑动机制
  • 批准号:
    8817346
  • 财政年份:
    1989
  • 资助金额:
    $ 19.95万
  • 项目类别:
    Standard Grant

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合作研究:植被同化作为盐沼生态系统中汞的来源以及对土壤和潮汐水暴露的影响
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