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Microstructural Study of Hydromechanical Behavior of Slurry Sample

机译:矿浆样品水力行为的微观结构研究

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Some tropical soils have distinct behavior due to their structure. In the last decades, new techniques improved the analysis of soil structure and enabled the correlation between the mentioned structure and the hydromechanical behavior of soils. In this work, a hydromechanical and microstructural characterization of slurry state of Brasilia soil was performed. The hydromechanical characterization was made with consolidation and water retention curve tests. The analysis of the structural characteristics of these soils was obtained from mercury intrusion porosimetry (MIP) test. It is assumed that different samples such as undisturbed soil, compacted soil and slurry have the initial structure affected in a distinct way by external loading. Thus, the main objective was to evaluate how the slurry sample had its structure affected by external loading and, also compare with undisturbed and compacted samples. Furthermore, the results showed that both the water retention curve and the pore size distribution curve are bimodal and that microstructure remained virtually unchanged. Moreover, as loading was increased there was a reduction of the macro pores, either in saturated and unsaturated samples.
机译:一些热带土壤由于其结构而具有不同的行为。在过去的几十年中,新技术改进了土壤结构的分析,并使上述结构与土壤的水力力学行为之间具有相关性。在这项工作中,对巴西利亚土壤的浆态进行了水力机械和微观结构表征。通过固结和保水曲线测试对流体力学进行了表征。这些土壤的结构特征分析是通过压汞法(MIP)进行的。假设不同的样本(如原状土壤,压实土壤和淤浆)的初始结构会受到外部载荷的不同影响。因此,主要目的是评估浆料样品的结构如何受到外部载荷的影响,并与未扰动和压实的样品进行比较。此外,结果表明保水曲线和孔径分布曲线都是双峰的,并且微观结构实际上保持不变。此外,随着载荷的增加,在饱和和不饱和样品中,大孔的数量都会减少。

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