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Updated: Jun 20, 2025

Stress Distribution During Cold Compression of Rocks and Mineral Aggregates Using Synchrotron-based X-Ray Diffraction
Published on: May 20, 2018
Dynamic stress characterization and instability risk identification using multisource acoustic signals in
Longjun Dong1, Yihan Zhang1, Zhongjie Chen1,2
1The School of Resources and Safety Engineering, Central South University, Changsha, 410083, China.
Monitoring mining-induced stress changes is key for safety. This study uses wave velocity and b-value patterns to detect microseismic events and predict potential geotechnical disasters in complex stress environments.
Area of Science:
- Geotechnical Engineering
- Mining Seismology
- Rock Mechanics
Background:
- Quantitative characterization of rock mass and stress changes is vital for structural stability monitoring and disaster early warning in mining operations.
- Pillar-free large-area continuous extraction presents unique challenges for understanding rock mass behavior and stress evolution.
- Microseismic monitoring is essential for assessing the dynamic response of rock masses to mining activities.
Purpose of the Study:
- To investigate the spatiotemporal distribution of microseismic sources during pillar-free large-area continuous extraction.
- To develop and apply a method combining velocity field and spatial b-value patterns for identifying stress and structural changes in panel stopes.
- To enhance the identification of instability disasters by analyzing anomalous wave velocities and b-values.
Main Methods:
- Analysis of time-space-intensity distribution of microseismic sources.
- Collaborative evolution pattern analysis of velocity fields and spatial b-values.
- Identification of anomalous zones in wave velocities and b-values at critical geological structures and mining interfaces.
Main Results:
- Anomalous zones in wave velocities and b-values were identified at intersections of mining roadways and footwall ore-rock contacts, correlating with microseismic event nucleation.
- The synergistic use of velocity fields and spatial b-values effectively revealed stress migration and stope structure changes induced by mining.
- An instability disaster at a connection roadway and cross-drift intersection was successfully identified through increased wave velocity and abnormal b-value changes.
Conclusions:
- The combined analysis of wave velocity fields and spatial b-values provides a robust method for characterizing stress and structural changes in mining environments.
- This approach offers valuable insights for predicting geotechnical engineering disasters in complex stress conditions.
- The findings support the potential of this method for real-time risk identification and structural stability monitoring in underground mining.
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