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Relationship between soil structure and water retention properties in a residual compacted soil

机译:残余压实土壤中土壤结构与保水性能的关系

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Soil structure, especially the soil pore size distribution, is a fundamental property that describes the hydro mechanical behavior of soils. The volume change behavior, shear strength, water retention capacity and hydraulic conductivity of soil are controlled by the pore size distribution. However, research on soil structure has been limited due to the associated expenses and specialized instruments, such as environmental scanning electron microscopes and mercury intrusion porosimeters (MIPs). In this study, the relationship between the soil water retention curve (WRC) along a drying path and the pore size distribution obtained through an MIP method was reviewed. The WRC for a compacted tropical soil was converted into a soil air injection curve and then used to estimate the pore size density (PSD) function. Relative to the data collected from MIP methods, the results showed an acceptable prediction of the PSD function based on a soil air injection curve. Finally, a series of adjustments to the air injection curve were performed to improve the accuracy of the PSD prediction based on the water retention curve. (C) 2016 Published by Elsevier B.V.
机译:土壤结构,特别是土壤孔径分布,是描述土壤水力力学行为的基本特性。土壤的体积变化行为,抗剪强度,保水能力和水力传导率受孔径分布的控制。然而,由于相关费用和专用仪器(例如环境扫描电子显微镜和压汞仪)的研究,土壤结构的研究受到了限制。在这项研究中,回顾了沿干燥路径的土壤保水曲线(WRC)与通过MIP方法获得的孔径分布之间的关系。将压实的热带土壤的WRC转换为土壤空气注入曲线,然后用于估算孔径密度(PSD)函数。相对于从MIP方法收集的数据,结果显示基于土壤空气注入曲线的PSD函数的可接受预测。最后,对注气曲线进行了一系列调整,以提高基于保水曲线的PSD预测的准确性。 (C)2016由Elsevier B.V.发布

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