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Updated: Sep 7, 2025

Stress Distribution During Cold Compression of Rocks and Mineral Aggregates Using Synchrotron-based X-Ray Diffraction
Published on: May 20, 2018
Microstructural Origin of Propagating Compaction Patterns in Porous Media
Lars Blatny1, Paul Berclaz1, François Guillard2
1School of Architecture, Civil and Environmental Engineering, Swiss Federal Institute of Technology, Lausanne (EPFL), CH-1015 Lausanne, Switzerland.
Compaction patterns in porous materials like rocks and snow arise from a universal pore collapse process. Material strength and loading rate determine diverse compaction behaviors, unifying disparate observations.
Area of Science:
- Geophysics
- Materials Science
- Physics of Complex Systems
Background:
- Diverse porous materials (rocks, foams, cereals, snow) exhibit common compaction patterns, such as propagating or stationary bands.
- The origins of these patterns are debated, with current models relying on material-specific empirical laws.
Purpose of the Study:
- To identify a universal mechanism underlying diverse compaction patterns in porous materials.
- To develop a unified model applicable across different structured porous geometries.
Main Methods:
- Development of a generic model for inelastic structured porous geometries.
- Analysis of pore collapse dynamics within this generalized framework.
Main Results:
- Demonstration that a universal process of pore collapse drives the observed compaction patterns.
- Identification of two dimensionless numbers (material strength and loading rate) that map the diversity of observed patterns.
- Mapping of pattern diversity within a phase space defined by these two dimensionless numbers.
Conclusions:
- Compaction patterns in porous materials are governed by a universal pore collapse mechanism, not material-specific processes.
- The observed diversity in patterns can be systematically explained and predicted using a simple phase space based on material strength and loading rate.
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