Study on the Long-term Dewatering Disturbance Pattern of Clayey Silt Composite Layer in Water-Rich Areas
The clayey silt composite layer is widely distributed in the Central Plains of China, especially in the eastern new urban area of Zhengzhou. The stratigraphic structure is generally a multi-layer system interbedded with clayey soil, silt, and fine silty sand, predominantly composed of clayey soil. The thickness of a single clayey soil layer can reach up to 68m. This considerable thickness implies that the creep process during foundation pit dewatering will persist continuously. The main structure of a metro station in the Zhengzhou Eastern Area is adjacent to high-speed railway bridge piles. Based on a comprehensive understanding of the engineering geological conditions of the study area and combined with monitoring data, this paper establishes a three-dimensional numerical model using ABAQUS finite element simulation software. The disturbance law of the clayey silt composite layer under long-term dewatering conditions and the impact of long-term dewatering on high-speed railway bridge piles are derived. The results show that long-term foundation pit dewatering forms a dewatering funnel-shaped settlement curve centered on the dewatering wells, which expands over time. The settlement impact is highest near the dewatering wells. Long-term dewatering affects nearby high-speed railway bridge piles, and pier settlement is very sensitive to the water level drawdown. Therefore, it is recommended that the pit water-stop curtain on the side adjacent to the high-speed railway be constructed as a double row of water-stop piles with increased length.
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