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Updated: Jul 2, 2025

Measuring and Modeling Contractile Drying in Human Stratum Corneum
Published on: March 1, 2017
Experimental study on damage of slope under drying and wetting cycle based on DC electric method
Ensheng Kang1, Zexi Zhao2, Haidong Meng1
1School of mining and coal, Inner Mongolia University of Science and Technology, Baotou, Inner Mongolia, 014010, China.
Investigating dump slope stability, this study reveals how resistivity changes indicate water content and crack development. Sudden resistivity drops in saturated slopes signal cracks, enabling early instability prediction.
Area of Science:
- Geotechnical Engineering
- Environmental Science
- Geophysics
Background:
- Dump slopes face stability challenges due to cyclic drying and wetting.
- Understanding seepage and crack propagation is crucial for slope safety.
Purpose of the Study:
- To investigate dump slope seepage laws and crack development under simulated rainfall.
- To analyze the impact of these processes on slope stability.
- To establish geoelectric field characteristics for damage assessment.
Main Methods:
- Constructed a simulation test slope system in a controlled rainfall environment.
- Derived apparent resistivity response formulas using three-phase medium theory and Maxwell's conductivity formula.
- Monitored geoelectric field characteristics during simulated slope damage.
Main Results:
- A negative correlation exists between resistivity and water content; resistivity increases with cracks and decreases with water infiltration.
- Crack formation progresses through three stages: saturation, capillary zone/waterway development, and crack expansion.
- Sudden resistivity changes in saturated slopes indicate cracks and weak surfaces, signifying irreversible damage.
Conclusions:
- Apparent resistivity monitoring can effectively detect cracks and weak surfaces in dump slopes.
- Geoelectric field analysis provides a valuable tool for early prediction of slope instability.
- The findings enhance understanding of dump slope behavior under hydro-thermal cycles.
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