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Novel evaluation method based on critical arch height as instability criterion for sustaining arch
Lijin Wang1, Hang Jia2, Tong Jiang3
1College of Geosciences and Engineering, North China University of Water Resources and Electric Power, Zhengzhou, 450046, China.
Natural soil arches are crucial for slope stability. This study reveals that the second-formed soil arch offers the best locking effect, enhancing slope resistance until critical failure is reached, aiding landslide early warning.
Area of Science:
- Geotechnical Engineering
- Soil Mechanics
- Geological Engineering
Background:
- Natural soil arches significantly influence the stability and evolution of sustaining arch locked-segment-type slopes.
- Understanding the formation and locking effect of these soil arches is critical for predicting slope behavior.
Purpose of the Study:
- To investigate the formation process and evolution of natural soil arches in sustaining arch locked-segment-type slopes.
- To analyze the locking control effect of soil arches on slope stability.
- To develop a mechanical model for slope stability analysis based on the soil arching effect.
Main Methods:
- Utilized a self-developed model test device to simulate slope deformation and evolution.
- Observed the continuous formation and progressive destruction of soil arches.
- Developed a critical arch height mechanical model integrating soil arching and limit equilibrium theory.
Main Results:
- The second-formed soil arch exhibited the most effective locking, leading to a peak anti-sliding force.
- The slope's stability was maintained by stress adjustment and the formation of a larger soil arch.
- Destabilization occurred when the ultimate shear strength of the arch foots was exceeded, reaching a critical arch height.
Conclusions:
- The developed critical arch height mechanical model accurately reflects slope stability based on physical tests and real-world data (Xintan slope).
- The findings provide valuable insights for early warning systems for landslides in similar geological conditions.
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