3-D CONSOLIDATION ANALYSIS OF LAYERED SOIL WITH ANISOTROPIC PERMEABILITY USING ANALYTICAL LAYER-ELEMENT METHOD

Starting with governing equations of a saturated soil with anisotropic permeability and based on multiple integral transforms, an analytical layer-element equation is established explicitly in the Laplace-Fourier transformed domain. A global matrix of layered soil can be obtained by assembling a set of analytical layer-elements, which is further solved in the transformed domain by considering boundary conditions. The numerical inversion of LaplaceFourier trans- form is employed to acquire the actual solution. Numerical analysis for 3-D consolidation with anisotropic permeability of a layered soil system is presented, and the influence of anisotropy of permeability on the consolidation behavior is discussed.

考虑应力历史的饱和黏土一维固结渗透试验研究

为研究固结应力比和应力历史对饱和黏土一维固结渗透的影响,利用GDS三轴仪进行了一系列一维固结-渗透联合试验。研究结果表明,在不同固结应力比相同应力历史条件下,正常固结和超固结饱和黏土在一维固结渗透过程中试样的渗透系数和孔隙比均随固结应力比的增大而减小,试样的最终压缩量均随固结应力比的增大而增大。在相同固结应力比不同应力历史条件下,超固结饱和黏土的最终压缩量小于正常固结饱和黏土。将固结应力σ与土层自重应力σcz的差值σdv与试样最终压缩量sf进行拟合,得出应力差值σdv与各固结应力下的最终压缩量sf间呈良好的线性关系。通过研究发现,同时考虑固结应力比和应力历史对饱和黏土一维固结渗透的影响是有必要的,同时在得到土体自重应力后可较为准确地预测土体最终压缩量。

考虑软土流变特性和应力历史的一维固结与渗透试验

利用GDS先进固结试验系统对萧山软土进行了常规分级加载固结与渗透试验、分级加载流变固结与渗透试验、压缩—回弹—再压缩流变固结与渗透试验,绘制了沉降曲线、孔压消散曲线以及孔隙比和渗透系数的变化曲线,通过回归分析得到了萧山软土的压缩指数、回弹指数、渗透指数、次固结系数。试验结果表明:萧山软土具有明显的流变特性,对于正常固结萧山软土,土样底部超静孔压消散大约在加载后5h左右完成,而超固结土孔压消散速度比正常固结土快,应力历史和超固结比对次固结系数有显著的影响。