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Temperature Effects on the Unsaturated Hydraulic Properties of Two Fine-Grained Soils and Their Influence on Moisture Movement under an Airfield Test Facility

机译:温度对两种细颗粒土壤非饱和水力特性的影响及其对水分测试的影响

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The influence of temperature on soil engineering properties is a major concern in the design of engineering systems such as radioactive waste disposal barriers, ground source heat pump systems and pavement structures. In particular, moisture redistribution under pavement systems might lead to changes in unbound material stiffness that will affect pavement performance. Accurate measurement of thermal effects on unsaturated soil hydraulic properties may lead to reduction in design and construction costs. This paper presents preliminary results of an experimental study aimed at determining the effect of temperature on the soil water characteristic curve (SWCC) and the unsaturated hydraulic conductivity function (k_(unsat)). Pressure plate devices with volume change control were used to determine the SWCC and the instantaneous profile method was used to measure k_(unsat). These properties were obtained for two fine-grained materials subjected to controlled temperatures of 5°C, 25°C and 40°C. The results were used to perform a sensitivity analysis of the effect of temperature changes on the prediction of moisture movement under a covered area. The findings were compared to field measured water content data obtained on the subgrade of FAA William Hughes test facility located in Atlantic City. Results indicated that temperature affected the unsaturated hydraulic properties of the two fine-grained materials used in the study. For the DuPont soil, the water retention at 5°C was higher than that for higher temperatures for suction levels lower than about 10,000 kPa; while the k_(unSat) functions were not statistically different. The County soil holds around 10% more moisture at 5°C than at 40°C for suction levels higher than about 1,000 kPa and the k_(unsat) function at 40°C was slightly higher than the function at 5°C. The finding from sensitivity analysis showed that the most accurate modeling was the modeling with unsaturated material properties at 40°C and the difference in unsaturated hydraulic properties did lead to some variations in modeling results.
机译:温度对土壤工程特性的影响是工程系统设计中的主要问题,例如放射性废物处置屏障,地源热泵系统和路面结构。特别是,路面系统下的水分重新分布可能会导致未结合的材料刚度发生变化,从而影响路面性能。准确测量对不饱和土壤水力特性的热效应可能会导致设计和建造成本的降低。本文介绍了旨在确定温度对土壤水分特征曲线(SWCC)和非饱和导水系数(k_(unsat))的影响的实验研究的初步结果。使用具有体积变化控制的压板设备确定SWCC,并使用瞬时轮廓法测量k_(unsat)。这些性能是针对两种细粒材料在5°C,25°C和40°C的受控温度下获得的。该结果用于对覆盖区域下温度变化对水分运动预测的影响进行敏感性分析。将该结果与在位于大西洋城的FAA William Hughes测试设施的路基上获得的现场测得的含水量数据进行了比较。结果表明温度影响了研究中使用的两种细粒材料的不饱和水硬性。对于杜邦土壤,在低于10,000 kPa的吸力条件下,在5°C下的保水率高于在更高温度下的保水率;而k_(unSat)函数在统计学上没有差异。对于高于1000 kPa的吸力水平,该县的土壤在5°C时比40°C时的水分含量高出约10%,并且在40°C时的k_(unsat)函数略高于5°C时的k_(unsat)函数。敏感性分析的结果表明,最准确的建模是在40°C下使用不饱和材料特性进行建模,并且不饱和水力学特性的差异确实导致了建模结果的某些变化。

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