Thermal shakedown in granular materials with irregular particle shapes
Yize Pan1, Xiaohui Gong1, Alessandro F Rotta Loria2
1Department of Civil and Environmental Engineering, Subsurface Opportunities and Innovations Laboratory, Northwestern University, Evanston, USA.
Cyclic temperature variations cause irreversible deformation in granular materials like sand. This thermal shakedown effect, influenced by particle shape and stress, leads to significant compaction over multiple cycles.
Area of Science:
- Geotechnical Engineering
- Materials Science
- Thermodynamics
Background:
- Granular materials experience diverse temperature fluctuations in natural and engineered settings.
- The mechanical response of granular materials to cyclic temperature variations is not well understood.
- Key factors like particle shape, stress, density, and temperature amplitude are under-explored.
Purpose of the Study:
- To investigate the impact of cyclic temperature variations on the mechanics of granular materials, specifically sands.
- To quantify the influence of particle shape, stress level, relative density, and temperature amplitude on this response.
Main Methods:
- Advanced laboratory experiments were conducted on granular materials, focusing on sands.
- Cyclic temperature variations were applied to samples under controlled conditions.
- Deformations and microstructural changes were monitored.
Main Results:
- Cyclic temperature variations induce 'thermal shakedown' in sands, causing irreversible bulk deformations.
- These deformations result from microstructural rearrangements due to particle thermal expansion and contraction.
- The extent of deformation is dependent on particle shape, stress, density, and temperature amplitude.
Conclusions:
- Thermal shakedown leads to significant cumulative compaction in sands and other granular materials over multiple cycles.
- This phenomenon can have substantial implications for the performance of natural and engineered systems.
- Understanding thermal shakedown is crucial for predicting the long-term behavior of granular materials under thermal cycling.
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