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Comparison of direct and indirect measured soil-water characteristic curves for a silty sand

机译:粉砂直接和间接测得的土壤水特征曲线的比较

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摘要

It is time consuming and needs sophisticated testing apparatus to determine unsaturated soil properties such as hydraulic conductivity and shear strength. Therefore, engineers hesitate to use unsaturated soil properties in economical geotechnical problem solving. To promote the use of unsaturated soil properties in geotechnical engineering designs, numbers of methods have been developed to estimate/predict unsaturated soil properties. The Soil-water characteristic curve (SWCC) defines the relationship between the soil suction and water content. During past few decades, different measuring and estimation/prediction methods have been developed by researchers to ascertain SWCC of soils. Among them, direct and indirect methods are widely used to measure the SWCC of soil. Indirect methods such as axis-translation technique are commonly used in the laboratory to determine SWCC. It is important to understand how well the indirectly measured SWCC is related to actual soil-water retention properties of soil during drying and wetting process. Bridging that research gap, in this study, Soil water characteristic curve (SWCC) of sandy soil was measured using both indirect (Axis translation method using Tempe Pressure Cell) and direct methods. The direct measured SWCCs were obtained by subjecting the instrumented soil column and model embankment to wetting and drying cycles. When comparing SWCCs measured by direct and indirect methods, it was found that the indirect method provides a very close agreement with the outcomes of direct methods. This ensures that the SWCCs measured in the laboratory by using indirect methods can be used in Geotechnical Engineering practice.
机译:这是耗时的,并且需要复杂的测试设备来确定不饱和土壤的性质,例如水力传导率和剪切强度。因此,工程师不愿在经济的岩土工程问题解决中使用非饱和土的性质。为了促进在土力工程设计中使用非饱和土壤特性,已经开发了许多方法来估计/预测非饱和土壤特性。土壤水特征曲线(SWCC)定义了土壤吸力和含水量之间的关系。在过去的几十年中,研究人员开发了不同的测量和估计/预测方法来确定土壤的SWCC。其中,直接和间接方法被广泛用于测量土壤的SWCC。诸如轴平移技术之类的间接方法通常在实验室中用于确定SWCC。重要的是要了解间接测量的SWCC与干燥和湿润过程中土壤的实际土壤保水特性之间的关系。弥补这一研究空白,本研究使用间接方法(使用Tempe压力传感器的轴平移方法)和直接方法测量了沙质土壤的土壤水分特征曲线(SWCC)。通过对仪器化的土壤柱和模型路堤进行润湿和干燥循环,可以获得直接测量的SWCC。比较直接法和间接法测得的SWCC时,发现间接法与直接法的结果非常吻合。这确保了在实验室中通过间接方法测得的SWCC可以用于岩土工程实践中。

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