One-dimension consolidation of soil layer with the soil properties as a power function of depth
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摘要: 采用分離變量法,求解了任意荷載作用下滲透系數和體積壓縮系數隨深度按冪函數變化土層模型的一維固結問題,從而得到不同排水邊界條件下超孔隙水壓力和沉降等隨時間變化的解析表達式.通過計算分析,討論了該類非均質土固結時超孔隙水壓力、沉降的變化規律.Abstract: The analytical solution to the one-dimension consolidation governing equation of soil layer was deduced by use of separation of variables when the laws of permeability and compressibility coefficients with depth can be expressed as power functions. The analytical expressions of excess pore pressure isochrones and settlement-to-time relations were obtained for different drainage boundary conditions under arbitrary loading. A series of cases were presented for analyzing the law of the excess pore pressure isochrones and settlement-to-time relations when those non-homogeneous soil consolidated.
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