原状Q_3黄土具有显著的结构性与湿陷性,其结构性对力学性状的影响非常复杂。为揭示原状Q_3黄土在三轴剪切试验过程中的细观结构变化,构建描述原状黄土Q_3剪切破坏细观结构破损演化规律的本构方程,揭示其结构性对力学性状的影响,采用了...原状Q_3黄土具有显著的结构性与湿陷性,其结构性对力学性状的影响非常复杂。为揭示原状Q_3黄土在三轴剪切试验过程中的细观结构变化,构建描述原状黄土Q_3剪切破坏细观结构破损演化规律的本构方程,揭示其结构性对力学性状的影响,采用了应力控制式CT–三轴仪对非饱和原状Q_3黄土进行围压为50,100,200,400 k Pa的固结排水三轴剪切试验,同时利用CT机将试样的5个断面分别按固结完成时、微裂纹产生时、剪切破损发展演化Ⅰ,Ⅱ,Ⅲ和剪切破坏时6种损伤状态进行实时无损量测。结合三轴剪切试验时应力应变状态、对应的CT扫描CT数及方差的物理意义定义了原状黄土破损结构势参数与破损率,建立了破损率与轴向应变、偏应力的演化方程,充分利用CT图像上的细观物理信息研究了原状Q_3黄土结构破损演化过程及力学行为。试验结果表明:在峰值偏应力前后弱软化型试样随轴向应变的增大CT数先增大后减小、方差先减小后增大,而硬化型试样则CT数单调增大、方差单调减小;剪切破坏时软化型试样破损结构势参数先小幅增长后快速减小,硬化型试样其值变化不大;根据定义的破损率与轴向应变、偏应力函数关系将不同围压下破损前和破损后分段拟合进行归一化处理建立的本构方程可以很好地表述原状黄土剪切破坏细观结构破损演化全过程。展开更多
In order to study the deterioration characteristics of the microscopic structure of sandstones in freeze-thaw cycles, tests of180 freeze-thaw cycles were performed on sandstone specimens. The nuclear magnetic resonan...In order to study the deterioration characteristics of the microscopic structure of sandstones in freeze-thaw cycles, tests of180 freeze-thaw cycles were performed on sandstone specimens. The nuclear magnetic resonance （NMR） technique was applied tothe measurement of sandstone specimens and analysis of the magnetic resonance imaging. Then, the fractal theory was employed tocompute the fractal dimension values of pore development of rocks after different freeze-thaw cycles. The results show that the massand porosity of rocks grow with the increase of freeze-thaw cycles. According to the NMR T2 distribution of sandstones, the poresizes of rock specimens increase after 180 freeze-thaw cycles, especially that of the medium-sized and small-sized pores. The spatialdistribution of sandstone pores after freeze-thaw cycles has fractal features within certain range, and the fractal dimension ofsandstones tends to increase gradually.展开更多
文摘原状Q_3黄土具有显著的结构性与湿陷性,其结构性对力学性状的影响非常复杂。为揭示原状Q_3黄土在三轴剪切试验过程中的细观结构变化,构建描述原状黄土Q_3剪切破坏细观结构破损演化规律的本构方程,揭示其结构性对力学性状的影响,采用了应力控制式CT–三轴仪对非饱和原状Q_3黄土进行围压为50,100,200,400 k Pa的固结排水三轴剪切试验,同时利用CT机将试样的5个断面分别按固结完成时、微裂纹产生时、剪切破损发展演化Ⅰ,Ⅱ,Ⅲ和剪切破坏时6种损伤状态进行实时无损量测。结合三轴剪切试验时应力应变状态、对应的CT扫描CT数及方差的物理意义定义了原状黄土破损结构势参数与破损率,建立了破损率与轴向应变、偏应力的演化方程,充分利用CT图像上的细观物理信息研究了原状Q_3黄土结构破损演化过程及力学行为。试验结果表明:在峰值偏应力前后弱软化型试样随轴向应变的增大CT数先增大后减小、方差先减小后增大,而硬化型试样则CT数单调增大、方差单调减小;剪切破坏时软化型试样破损结构势参数先小幅增长后快速减小,硬化型试样其值变化不大;根据定义的破损率与轴向应变、偏应力函数关系将不同围压下破损前和破损后分段拟合进行归一化处理建立的本构方程可以很好地表述原状黄土剪切破坏细观结构破损演化全过程。
基金Projects(41502327,51474252)supported by the National Natural Science Foundation of ChinaProject(2013YQ17046310)supported by the National Key Scientific Instrument and Equipment Development Project of China+1 种基金Project(20130162120012)supported by the Special Research Fund for the Doctoral Program of Higher Education of ChinaProject(2015CX005)supported by Innovation Driven Plan of Central South University,China
文摘In order to study the deterioration characteristics of the microscopic structure of sandstones in freeze-thaw cycles, tests of180 freeze-thaw cycles were performed on sandstone specimens. The nuclear magnetic resonance （NMR） technique was applied tothe measurement of sandstone specimens and analysis of the magnetic resonance imaging. Then, the fractal theory was employed tocompute the fractal dimension values of pore development of rocks after different freeze-thaw cycles. The results show that the massand porosity of rocks grow with the increase of freeze-thaw cycles. According to the NMR T2 distribution of sandstones, the poresizes of rock specimens increase after 180 freeze-thaw cycles, especially that of the medium-sized and small-sized pores. The spatialdistribution of sandstone pores after freeze-thaw cycles has fractal features within certain range, and the fractal dimension ofsandstones tends to increase gradually.
