Abstract
An X-ray diffraction mineral composition test was conducted on the shear zone soil of the Guoyemoli landslide in Zhouqu County to analyze the deformation and strength characteristics of the shear zone soil under different stress states. A scanning electron microscope and a stereo microscope were used to observe the microstructure of the shear surface of the shear zone soil, revealing the microstructure evolution characteristics of the shear zone soil sample. The findings of this study provide a data basis for slope stability and risk assessment from a micro perspective.
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Schedule a callMore From: IOP Conference Series: Earth and Environmental Science
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