Laboratory study on the relationship between soilmass deformation and water seepage in North China |
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Authors: | Xiu Yan Wang Jiang Chen Lin Sun Shuang Ping Han Yu Hong Fei Jin Zhe Wang Chang Li Liu and Yun Zhang |
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Institution: | (1) Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, 050061, China |
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Abstract: | The study on the relationship between the soilmass deformation and water seepage under certain stress in North China was conducted
through combined tests of the consolidation deformation and water seepage. The results showed that the actual deformation
of the clay soil under stress is greater than the deformation induced by the seepage. On average, the deformation induced
by seepage was about 60% of the actual clay deformation under stress. The actual deformation of sandy soil, however, is less
than the deformation induced by seepage. On average, the seepage-induced deformation was approximately 125% of the actual
sandy soil deformation. These results indicated that the sandy soil did not have complete plasticity. Clay had the highest
amount of water seepage and deformation, while silty soil, calcareous highly cemented clayed soil and sandy soil had less
water seepage and deformation. The underlying mechanisms were also discussed. The results of this study contribute to the
understanding of land subsidence mechanism and rough estimation of groundwater exploitation. |
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