Development of a Stress Sensor for In-Situ High-Pressure Deformation Experiments Using Radial X-Ray Diffraction
Autor: | Shun-ichiro Karato, R. E. Silber, Haiyan Chen, Anwar Mohiuddin, Jennifer Girard |
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Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
Diffraction
Materials science lcsh:Mineralogy lcsh:QE351-399.2 010504 meteorology & atmospheric sciences Isotropy deformation Geology 02 engineering and technology stress sensor D-DIA 021001 nanoscience & nanotechnology Geotechnical Engineering and Engineering Geology 01 natural sciences d-dia Stress (mechanics) Pyrope high pressure in-situ X-ray crystallography Compression (geology) Composite material Deformation (engineering) 0210 nano-technology 0105 earth and related environmental sciences |
Zdroj: | Minerals, Vol 10, Iss 2, p 166 (2020) Minerals Volume 10 Issue 2 |
Popis: | We developed a stress sensor for in-situ deformation experiments using synchrotron radial X-ray diffraction. This stress sensor provided nearly diffraction-plane-independent stress that, when used in series with a sample, reduced the uncertainty of the average stress estimation acting on a sample. Here, we present the results of a study where pyrope was used as a stress sensor. Using a Deformation-DIA (D-DIA) high-pressure deformation apparatus, pyrope, olivine and alumina were deformed in the same run/cell assembly placed in series along the compression direction. Deformation experiments were conducted at pressures between 4 and 5 GPa and temperatures between 730 and 1273 K with strain-rates between 10&minus 5 and 10&minus 6 s&minus 1. Stresses estimated from various (hkl) planes in pyrope were nearly the same i.e., pyrope is plastically isotropic with &le 10 % variation with (hkl). However, stresses from various (hkl) planes in olivine and alumina varied by approximately a factor of 3. Comparisons between average stresses inferred from pyrope and those from different diffraction planes in olivine and alumina showed that the average stress in these materials evolved from low-end stress, estimated from various (hkl) planes at small strain, to high-end stress at a large strain. This suggests that the rate-controlling slip system in these materials changes from the soft to the hard slip system with strain. |
Databáze: | OpenAIRE |
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