非饱和原状Q2黄土屈服硬化过程的细观结构演化分析
Analysis on Meso-structure evolution of unsaturated natural Q2 loess during yield hardening
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摘要: 利用和CT机配套的多功能土工三轴仪,对非饱和原状Q2黄土在三轴剪切过程中内部结构的变化进行了动态、定量和无损地量测,得到了屈服硬化土样内部结构演化的CT图像和相应的CT数据,从细观上解释了屈服硬化过程。试验结果表明:原状Q2黄土内部存在大量孔隙、裂隙、姜石等结构缺陷,初始结构具有各向异性,姜石的存在对CT数和方差影响较大。非饱和原状Q2黄土屈服硬化细观变形可大致分为微压密阶段、结构微调整阶段和压密快速发展阶段3个阶段。剪切过程呈现良好的以均匀变形为主的细观变形特点。提出利用CT数随偏应变或偏应力的关系确定屈服应力的新方法。宜用CT数来描述原状Q2黄土屈服硬化过程的结构演化规律,相同吸力下,随着固结净围压的增大,CT数变化率越大;相同净围压下,随着吸力的增大,CT数变化率越小。Abstract: The variation of interior structure of unsaturated natural Q2 loess in triaxial tests was monitored instantaneously,quantitatively and nondestructively by means of computerized tomography(CT) technology.The clear CT images and relevant data reflecting the structure evolution of yield hardening soil samples were attained.The course of yield hardening was explained.It was shown that some structure damages such as pore,flow,ginger nut,etc.existed in natural Q2 loess.The initial structure of Q2 loess was inhomogeneous.The CT data was prominently affected by ginger nut.The meso-deformation of unsaturated natural Q2 loess could be divided into three stages,i.e.,slightly dense stage,stage of slight adjust-ment of structure,and rapidly dense stage.The meso-deformation during the test process was manifested by uniform deformation.A new method to identify the field stress of natural Q2 loess using curves of CT-number versus deviatoric stress or deviatoric strain was suggested.It was suitable to adopt CT-number to describe structure evolution of yield hardening of natural Q2 loess.The variation of CT-number increased with the increase of net consolidation pressure under the same suction;while the variation of CT-number decreased with the increase of suction under the same net consolidation pressure.