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Yield strength at high pressure and temperature
160
Citations
14
References
1994
Year
Materials ScienceYield StrengthHigh Pressure ApparatusMantle GeochemistryEngineeringHigh Temperature MaterialsMechanical EngineeringApplied PhysicsHigh PressureYield OptimizationYield (Engineering)ThermodynamicsYield EngineeringHigh Temperature GeochemistryMechanics Of MaterialsMicrostructureStructural Materials
Macroscopic deviatoric stress manifests as a uniform deviatoric strain oriented by the pressurizing medium geometry, while microscopic deviatoric stress is identified by elastic broadening of diffraction lines. Yield strength is measured at high pressure and temperature using a large‑volume, high‑pressure apparatus (SAM85) with synchrotron radiation. The deviatoric stress reaches the yield point, evidenced by uniformity, saturation, and temperature dependence, and yield strengths for NaCl and MgO were determined up to 8 GPa and 1200 °C, consistent with room‑temperature diamond‑anvil studies and demonstrating pressure’s effect on yield strength and the feasibility of measuring high‑pressure, high‑temperature yield strengths for mantle phases.
Yield strength is measured at high pressure and temperature using a large volume, high pressure apparatus (SAM85) with synchrotron radiation. A macroscopic deviatoric stress is manifest as a uniform deviatoric strain that is oriented by the geometry of the pressurizing medium. Microscopic deviatoric stress is identified as the elastic broadening of diffraction lines. The deviatoric stress reaches the yield point as evidenced by the uniformity, the saturation, and the temperature dependence of the deviatoric stress. Yield strengths, which correspond to the stress saturation level at a few per cent strain, are determined for NaCl and MgO up to 8 GPa and 1200°C. The results are consistent at room temperature with previous diamond anvil studies and demonstrate the effect of pressure on yield strength. These data demonstrate the feasibility of determining high pressure, high temperature yield strengths for mantle phases.
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