首页> 外文期刊>Quarterly Journal of Engineering Geology & Hydrogeology >Two-dimensional simulation of underground seepage in a dangerous piping zone of the Jingjiang Great Levee, the middle reach of the Yangtze River
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Two-dimensional simulation of underground seepage in a dangerous piping zone of the Jingjiang Great Levee, the middle reach of the Yangtze River

机译:长江中游靖江大堤危险管道带地下渗流的二维模拟

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摘要

This case study simulated the seepage field at Yangjiawan using Visual Modflow software. The Yangjiawan area shows potential for dangerous piping along the Jingjiang Great Levee, on the north bank of the Yangtze River. The levee foundation sits on loam and fine sand strata and is covered with a clay layer and artificial earthfill. Ponds are present behind the levee, where piping occurs frequently. The authors analysed several models to simulate actual situations and to provide guidance for piping control. Assuming that the potential for piping increases with seepage and groundwater velocities, the models allow various engineered control measures to be assessed under different natural conditions. Parameters and features of the models included: different water heads, pressure-relief wells, seepage-proof walls, surface coverage, different hydraulic conductivities of the artificial earthfill, and pond levels during high river water levels. The results demonstrate the effectiveness of pressure-relief wells in preventing piping and also show that a decrease of the hydraulic conductivities of the artificial earthfill would reduce infiltration and seepage damage significantly, especially during high river water levels. Furthermore, pressure-relief wells and the reduction of hydraulic conductivities of artificial earthfill should prevent piping if ponds are present.
机译:本案例研究使用 Visual Modflow软件模拟了杨家湾的渗流场。杨家湾地区在沿长江北岸的靖江大堤上显示出危险管道的潜力。堤防基础位于 壤土和细砂岩层上,并覆盖有粘土层和 人造土。堤坝后方有池塘, 管道经常出现。作者分析了几种模型 来模拟实际情况并为管道 控制提供指导。假设管道的潜力随着 渗水和地下水流速的增加而增加,这些模型允许在不同的自然 条件下评估各种 工程控制措施。模型的参数和特征包括: 不同的水头,泄压井,防渗 墙,表面覆盖率,不同的水力传导率 人工填土和高水位时的池塘水位。结果表明,泄压 井在防止管道运输方面是有效的,并且还表明,降低人工填土的 的水力传导率会 入渗和渗流破坏显着,尤其是在高河水位期间 。此外,如果有池塘,则泄压 井和人工 填土的水力传导率的降低应防止配管。

著录项

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  • 作者

    C. Yi; B. Wang; M. Jin; Z. Guo;

  • 作者单位

    Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China (e-mail: clyi@itpcas.ac.cn)|Key Laboratory of Cryosphere and Environment, CAS, Lanzhou 73000, China;

    Key Laboratory of Cryosphere and Environment, CAS, Lanzhou 73000, China;

    School of Environmental Studies, China University of Geosciences at Wuhan, Wuhan, 430073, China;

    Embankment Office, Bureau of Water Conservancy of Hubei Province, Wuhan, Hubei, 430071, China;

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