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Influence of Temperature on the Volume Change Behavior of Saturated Sand

机译:温度对饱和砂土体积变化行为的影响

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The effect of temperature on the volume change of sand is rarely reported but may be relevant to the performance of energy geostructures. This study involves an investigation of the thermal volume change behavior of saturated, dense sand through a series of temperature-controlled, isotropic hollow cylinder triaxial compression tests. Variables measured during a heating stage include the volume of water expelled from the sand specimen, the temperatures at the top, bottom, and inside of the specimen, and the axial and volumetric strains. The volumes were used along with thermo-elastic relationships for the pore water and soil skeleton to infer the axial and volumetric strains during drained heating. It was observed that the thermally induced axial and volumetric strains were negative, reflecting expansion. The pore water was observed to flow out of the sand specimen during heating, reflecting differential thermal expansion of the pore water and sand particles. The thermal volume changes were observed to be independent of the mean effective stress, as the dense sand specimens were all in normally consolidated conditions. Three linear equations incorporating the effects of temperature on the volume change behavior of dense sand were proposed and match well with the experimental data. The experimental approach proposed in this study can be used in the future to evaluate the role of sand density and stress state on the parameters of these equations.
机译:温度对沙粒体积变化的影响鲜有报道,但可能与能源地质结构的性能有关。这项研究涉及通过一系列温度控制的各向同性空心圆柱三轴压缩试验研究饱和致密砂子的热容变化行为。在加热阶段测得的变量包括从砂样品中排出的水量,样品顶部,底部和内部的温度以及轴向应变和体积应变。使用这些体积以及孔隙水和土壤骨架的热弹性关系来推断排水加热过程中的轴向应变和体积应变。观察到,热引起的轴向和体积应变为负,反映了膨胀。观察到在加热过程中孔隙水从砂样中流出,反映了孔隙水和砂粒的热膨胀差异。观察到热体积的变化与平均有效应力无关,因为致密的砂试样都处于正常固结状态。提出了三个考虑温度对致密砂体体积变化行为影响的线性方程,并与实验数据吻合。本研究中提出的实验方法可在将来用于评估砂密度和应力状态在这些方程式参数中的作用。

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