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妙尔尼尔:用于四维同步加速器X射线显微断层扫描的微型三轴岩石变形装置。

Mjölnir: a miniature triaxial rock deformation apparatus for 4D synchrotron X-ray microtomography.

作者信息

Butler Ian, Fusseis Florian, Cartwright-Taylor Alexis, Flynn Michael

机构信息

School of Geosciences, University of Edinburgh, James Hutton Road, The King's Buildings, Edinburgh EH9 3FE, United Kingdom.

出版信息

J Synchrotron Radiat. 2020 Nov 1;27(Pt 6):1681-1687. doi: 10.1107/S160057752001173X. Epub 2020 Oct 16.

DOI:10.1107/S160057752001173X
PMID:33147194
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7642963/
Abstract

An X-ray transparent experimental triaxial rock deformation apparatus, here named `Mjölnir', enables investigations of brittle-style rock deformation and failure, as well as coupled thermal, chemical and mechanical processes relevant to a range of Earth subsurface environments. Designed to operate with cylindrical samples up to 3.2 mm outside-diameter and up to 10 mm length, Mjölnir can attain up to 50 MPa confining pressure and in excess of 600 MPa axial load. The addition of heaters extends the experimental range to temperatures up to 140°C. Deployment of Mjolnir on synchrotron beamlines indicates that full 3D datasets may be acquired in a few seconds to a few minutes, meaning full 4D investigations of deformation processes can be undertaken. Mjölnir is constructed from readily available materials and components and complete technical drawings are included in the supporting information.

摘要

一种X射线透明的实验性三轴岩石变形装置,这里命名为“雷神锤”,能够研究脆性岩石变形与破坏,以及与一系列地球地下环境相关的热、化学和力学耦合过程。“雷神锤”设计用于外径达3.2毫米、长度达10毫米的圆柱形样品,可实现高达50兆帕的围压和超过600兆帕的轴向载荷。添加加热器可将实验温度范围扩展至高达140°C。将“雷神锤”部署在同步加速器光束线上表明,可在几秒到几分钟内获取完整的三维数据集,这意味着可以对变形过程进行完整的四维研究。“雷神锤”由易于获取的材料和部件制成,完整的技术图纸包含在补充信息中。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/099327409945/s-27-01681-fig5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/6e8f0cd67f82/s-27-01681-fig1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/75885e0cde1c/s-27-01681-fig2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/7303c366c9b8/s-27-01681-fig3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/8c0aaecee665/s-27-01681-fig4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/099327409945/s-27-01681-fig5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/6e8f0cd67f82/s-27-01681-fig1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/75885e0cde1c/s-27-01681-fig2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/7303c366c9b8/s-27-01681-fig3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/8c0aaecee665/s-27-01681-fig4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c974/7642963/099327409945/s-27-01681-fig5.jpg

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Rev Sci Instrum. 2018 Apr;89(4):045101. doi: 10.1063/1.5030204.
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