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| Cementation characteristics of clay gravel layer and erosion failure mode of slope in Anqing Formation |
| DUAN Haipeng1,YU Fei2,HUANG Kang2,DAI Zhangjun2,CHEN Shanxiong2 |
| (1. Anhui Transportation Holding Group Co.,Ltd.,Hefei,Anhui 230088,China;2. State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan,Hubei 430071,China) |
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Abstract The clay gravel layer of the Anqing Formation is widely distributed in the upper reaches along the Yangtze River in Anhui Province. It is a special engineering geological body composed of gravel and clay. After the excavation of the project,it is very easy to cause slope collapse. In this paper,the clay gravel bed of the Anqing Formation was studied. Firstly,the type and composition of cement in the clay gravel bed were analyzed by X-ray diffraction method,and the cementation characteristics of the clay gravel layer were clarified,including matrix cementation and soil-stone interface cementation. Then,the experiment of artificial rain erosion model in the slope of clay gravel bed was carried out,and the variation law of slope destruction instability pattern of clay gravel layer with different gravel content was studied. The results show that when the gravel content is small (30%),the slope failure is mainly dominated by gully,and its failure form is mainly controlled by the clay layer. When the gravel content increases to 50%,the gravel skeleton effect is gradually reflected,and the slope failure form is greatly different from the soil slope. The slope failure is manifested as the evolution of erosion hole - erosion pit - shallow layer collapse. When the gravel content is large (70%),the gravel skeleton structure is relatively stable. Even if the clay particles are washed away in large quantities,the overall stability of the slope is better. Finally,the variation of substrate moisture content and wet peak migration depth of slopes with different gravel content were analyzed,and the internal mechanism of slope failure of clay gravel layer was further explained.
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