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Changes in thermal conductivity, suction and microstructure of a compacted lime-treated silty soil during curing

机译:固化过程中压实石灰处理的粉质土壤的导热系数,吸力和微观结构的变化

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摘要

An experimental study was conducted to investigate changes of thermal conductivity, suction and microstructure of a lime-treated silty soil during curing. The soil samples were prepared with 2% lime and compacted dry (17%) and wet (22%) of optimum. The thermal conductivity, total suction and pore size distribution were determined at various curing times. Results show that the thermal conductivity of samples compacted on the dry side decreases slightly with curing time, while the curing time effect on the samples compacted on the wet side is insignificant. The total suction generally increases with curing time even though the soil water content was kept constant. The pore size distribution characteristics are mainly related to its moulding water content. As the samples are compacted on the dry side, the pore size distribution shows typical bi-modal characteristics, with a population of macro-pores and a population of micro-pores. By contrast, as the samples are compacted on the wet side, the pore size distribution shows typical uni-modal characteristics. It is found that the modal size of both the large and small pores decrease with curing time. (c) 2016 Elsevier B.V. All rights reserved.
机译:进行了一项实验研究,以研究石灰处理的粉质土壤在固化过程中的导热系数,吸力和微观结构的变化。用2%的石灰和最适压实的干(17%)和湿(22%)压实土壤样品。在不同的固化时间下测定热导率,总吸力和孔径分布。结果表明,在干侧压实的样品的热导率随固化时间而略有降低,而在湿侧压实的样品的固化时间影响不明显。即使土壤水分保持恒定,总吸力通常会随着固化时间而增加。孔径分布特性主要与其成型含水量有关。当样品在干燥侧被压实时,孔径分布显示出典型的双峰特征,具有大量的大孔和大量的微孔。相反,当样品在潮湿的一侧压实时,孔径分布显示出典型的单峰特性。发现大孔和小孔的模态尺寸随固化时间减小。 (c)2016 Elsevier B.V.保留所有权利。

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