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    低温环境下非饱和大坝混凝土毛细吸水饱和度分布研究

    Study of Capillary Saturation Distribution of Unsaturated Dam Concrete in Low-Temperature Environment

    • 摘要: 冰冻前的饱和度是影响运行期大坝下游面区域混凝土冻融劣化的重要因素,但现有报导混凝土毛细吸水试验研究一般针对烘干的富胶凝材料试件且未考虑重力和低温的影响.首先采用高压PE平口袋设计提出了一种侧吸法和上吸法的毛细吸水方法,然后制备3种水胶比、3种环境低温、2种养护龄期的二级配大坝混凝土试件,探索试件毛细吸水14d后距吸水面不同深度处的饱和度分布规律.试验结果表明,非饱和大坝混凝土毛细吸水14d后,饱和度随深度增加而明显下降后稳定在某一水平,饱和度随水胶比、环境温度和龄期变化的关系为θ0.41<θ0.50<θ0.60θ2℃>θ8℃>θ5℃θ28d>θ90d,上吸法测得的饱和度大于侧吸法,但上吸法和侧吸法测得的水分扩散深度均不超过17.5cm.

       

      Abstract: During dam operation, saturation before freezing strongly affects the freeze-thaw deterioration of concrete in the downstream zone.However, previous experimental studies of capillary water absorption by concrete generally involve drying rich cementitious material specimens without considering gravity and low temperature.A capillary water absorption method for horizontal absorption and infiltration absorption is proposed by using high-pressure PE flat pocket design.Next, secondary aggregate grading dam-concrete specimens are prepared with three water-cement ratios, three low temperatures, and two curing ages to explore the saturation distribution of specimens at different depths with respect to the suction surface after 14 days of capillary water absorption.The test results show that, after 14 days of capillary water absorption by unsaturated dam concrete, the saturation decreases significantly with increasing depth and then stabilizes at a certain level.The relationship between saturation and water-binder ratio, ambient temperature, and age is θ0.41<θ0.50<θ0.60, θ2℃>θ8℃>θ5℃, and θ28d>θ90d.The saturation measured by the infiltration absorption method exceeds that measured by the horizontal absorption method, but the water diffusion depth measured by the infiltration absorption method and the horizontal absorption method does not exceed 17.5cm.

       

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