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一种用于地质材料在高温高压下进行应力控制测试的 Griggs 仪器升级版。

A Griggs apparatus upgrade for stress-controlled testing of geological material at high temperature and pressure.

作者信息

Soleymani Hamid, Kidder Steven

机构信息

Department of Earth and Environmental Sciences, The Graduate Center, CUNY, 365 5th Ave, New York, NY 10016, United States.

Department of Earth and Atmospheric Sciences, City College of New York, CUNY, 160 Convent Ave, New York, NY 10031, United States.

出版信息

HardwareX. 2021 Jan 14;9:e00172. doi: 10.1016/j.ohx.2021.e00172. eCollection 2021 Apr.

DOI:10.1016/j.ohx.2021.e00172
PMID:35492033
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9041190/
Abstract

The Griggs apparatus is a triaxial piston-cylinder instrument used in deformation experiments of geological material at temperatures up to 1200 °C and confining pressures up to 3 GPa. Currently, most Griggs apparatuses can carry out deformation experiments only at constant displacement rate. As a result, few experimental studies have explored other geologically-relevant deformation scenarios. We present supplemental instrumentation and software that enables Griggs apparatus users to carry out deformation experiments at controlled differential stress conditions. The add-on instrument includes a feedback loop mechanism that regulates the imposed differential stress on the sample and a data acquisition system that allows for real-time display of mechanical data in units of stress and displacement. We demonstrate the application of this instrument through two deformation experiments at constant differential stress on (1) an aluminum cylinder at room temperature and (2) a quartz aggregate at 850 °C, both at ~1 GPa confining pressure. These experiments show that the instrument can reliably control the imposed differential stress on the sample throughout the deformation. Applications of the instrument can be extended beyond constant differential stress to more sophisticated stress paths (e.g., stress pulse, stress ramp) or to maintain true strain rates by accounting for anticipated geometrical changes in the sample during deformation.

摘要

格里格斯装置是一种三轴活塞-圆筒仪器,用于在高达1200℃的温度和高达3GPa的围压下对地质材料进行变形实验。目前,大多数格里格斯装置只能以恒定位移速率进行变形实验。因此,很少有实验研究探索其他与地质相关的变形情况。我们展示了一种补充仪器和软件,使格里格斯装置的用户能够在控制的差应力条件下进行变形实验。附加仪器包括一个反馈回路机制,用于调节施加在样品上的差应力,以及一个数据采集系统,允许以应力和位移单位实时显示力学数据。我们通过在室温下对一个铝圆柱体和在850℃下对一个石英聚集体进行的两个恒差应力变形实验,展示了该仪器的应用,两个实验的围压均约为1GPa。这些实验表明,该仪器在整个变形过程中能够可靠地控制施加在样品上的差应力。该仪器的应用可以扩展到恒差应力之外,应用于更复杂的应力路径(如应力脉冲、应力斜坡),或者通过考虑变形过程中样品预期的几何变化来维持真实应变率。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/7377a2c62616/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/5c75f53564a3/ga1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/6fdb8789157f/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/a7532de55a4b/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/32fab2146039/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/40b117a5911f/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/7377a2c62616/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/5c75f53564a3/ga1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/6fdb8789157f/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/a7532de55a4b/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/32fab2146039/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/40b117a5911f/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0411/9041190/7377a2c62616/gr7.jpg

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本文引用的文献

1
An ultrasound probe array for a high-pressure, high-temperature solid medium deformation apparatus.一种用于高压高温固体介质变形装置的超声探头阵列。
Rev Sci Instrum. 2020 Aug 1;91(8):085117. doi: 10.1063/5.0004035.
2
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J Vis Exp. 2018 Apr 3(134):56841. doi: 10.3791/56841.
3
Dehydration of lawsonite could directly trigger earthquakes in subducting oceanic crust.蓝片岩脱水可直接引发俯冲洋壳中的地震。
Nature. 2016 Feb 4;530(7588):81-4. doi: 10.1038/nature16501.