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Updated: May 22, 2026

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Stress Distribution During Cold Compression of Rocks and Mineral Aggregates Using Synchrotron-based X-Ray Diffraction
Published on: May 20, 2018
X-ray diffraction evaluation of stress in high pressure deformation experiments
Summary
X-ray diffraction can measure stress in high-pressure deformation experiments. However, elastic models may not fully capture plastic deformation effects, requiring careful interpretation of lattice strain data.
Area of Science:
- Materials Science
- Geophysics
- Solid Mechanics
Background:
- X-ray diffraction (XRD) is a powerful technique for analyzing material structures.
- Understanding stress in materials under high pressure is crucial for various scientific and engineering fields.
Purpose of the Study:
- To evaluate the use of X-ray diffraction for measuring stress in high-pressure deformation experiments.
- To model elastic lattice strains in different experimental setups.
Main Methods:
- Modeling elastic lattice strains for axial and rotational deformation apparatus.
- Inverting stress from X-ray diffraction data.
- Comparing model results with experimental data.
Main Results:
- Stress can be successfully inverted from X-ray diffraction data in most high-pressure deformation scenarios.
- Elastic models of lattice strains may not adequately account for the influence of plastic deformation.
- Experimental data suggests plastic deformation impacts lattice strain measurements.
Conclusions:
- X-ray diffraction is applicable for stress determination in high-pressure deformation.
- Caution is advised when interpreting lattice strain data, as plastic deformation effects need further consideration.
- Refined models incorporating plasticity are needed for accurate stress analysis.
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