| 饱和软土成层地基一维非线性固结解析解 |
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| 引用本文： | 夏长青,胡安峰,崔军,吕文晓,谢康和.饱和软土成层地基一维非线性固结解析解[J].岩土力学,2018,39(8):2858-2864. |
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| 作者姓名： | 夏长青 胡安峰 崔军 吕文晓 谢康和 |
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| 作者单位： | 1. 浙江大学 滨海和城市岩土工程研究中心，浙江 杭州 310058； 2. 浙江大学 软弱土与环境土工教育部重点实验室，浙江 杭州 310058； 3. 杭州科技职业技术学院 城市建设学院，浙江 杭州，311402 |
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| 基金项目： | 国家自然科学基金资助项目（No. 51778572，No. 51278453）；教育部博士点基金资助项目（No. 20120101110029）。 |
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| 摘 要： | 假定土体在固结过程中压缩性和渗透性的变化成正比，基于 - 及 - 关系，推导出饱和软土成层地基一维非线性固结解析解，分别给出了按沉降定义和按有效应力定义的每层土平均固结度及整个土层总固结度的计算公式。采用Fortran语言编制了相应的计算程序，将计算得到的结果与已有双层地基一维非线性固结解析解计算结果进行比较，验证该解析解的正确性。利用该程序分析成层地基一维非线性固结性状，分别讨论了初始竖向渗透系数、初始体积压缩系数、荷载值及土层厚度对地基固结性状的影响。分析结果表明：在成层地基一维非线性固结过程中，初始竖向渗透系数对超静孔压的影响较为复杂，对上下层地基固结速率影响不同；初始体积压缩系数增大，超静孔压增大，固结速率变小；所加荷载值越大，超静孔压消散越慢，固结发展越慢；超静孔压消散速率不仅取决于土层厚度，同时取决于各层土渗透性的相对大小。
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| 关 键 词： | 饱和软土 成层地基 非线性固结 解析解 固结性状 |
| 收稿时间： | 2016-10-24 |
Analytical solutions for one-dimensional nonlinear consolidation of saturated soft layered soils |
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| XIA Chang-qing,HU An-feng,CUI Jun,Lü Wen-xiao,XIE Kang-he.Analytical solutions for one-dimensional nonlinear consolidation of saturated soft layered soils[J].Rock and Soil Mechanics,2018,39(8):2858-2864. |
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| Authors: | XIA Chang-qing HU An-feng CUI Jun Lü Wen-xiao XIE Kang-he |
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| Institution: | (1. Research Center of Coastal and Urban Geotechnical Engineering, Zhejiang University, Hangzhou, Zhejiang 310058, China; 2. Key Laboratory of Soft Soils and Geoenvironmental Engineering of Ministry of Education, Zhejiang University, Hangzhou, Zhejiang 310058, China; 3. Institute of Urban Construction, Hangzhou Polytechnic, Hangzhou, Zhejiang 311402, China |
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| Abstract: | Adopting the hypotheses that the variation of compressibility is proportional to permeability, and based on - and - relationships, analytical solutions are derived for one-dimensional nonlinear consolidation of saturated soft layered soils. The average degrees of consolidation of each layer and whole layered soils are defined in terms of settlement and effective stress respectively. A relevant computational program is developed by Fortran in this paper, and the solutions are verified by comparing with the existing analytical solutions for the one-dimensional nonlinear consolidation of double-layered soils. It is shown that in the process of the nonlinear consolidation of layered soils, the influence of the permeability is complex. The influence of permeability on the excess pore water pressure in the upper and the lower layers is different. The larger compressibility is, the greater the excess pore water pressure is, and the slower the rate of dissipation of the excess pore water pressure and greater the value of loading generate slow dissipation of the excess pore water pressure, and the slow consolidation process. The rate of dissipation of the excess pore water pressure depends not only on the layers thickness, but also the relative value of permeability of each layer soil. |
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| Keywords: | saturated soft soils layered soils nonlinear consolidation analytical solutions consolidation behavior |
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