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Research on the Impact of the Morphological Variation of Mineral Fragments on Soil Hydraulic Properties

机译:矿物碎片形态变化对土壤水力特性影响的研究

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This paper aims to highlight the relationship between soil particles morphology (shape, size and surface area) and hydraulic properties (hydraulic conductivity (saturated and unsaturated) and soil suction). Determination of morphological characteristics of soil particles was achieved by: a) size analysis and b) SEM microscopic analysis type. Determination of soil hydraulic properties was performed by laboratory methods: for hydraulic conductivity was used the constant-head method and the falling head method and suction was determined using the sandbox, sand/kaolin box and pressure membrane apparatus.
机译:本文旨在强调土壤颗粒形态(形状,大小和表面积)与水力特性(水力传导率(饱和和不饱和)和土壤吸力)之间的关系。通过以下方法测定土壤颗粒的形态特征:a)尺寸分析和b)SEM显微镜分析类型。通过实验室方法确定土壤的水力特性:对于水力传导率,使用恒压头法和落头法,并使用沙箱,沙/高岭土箱和压力膜设备确定吸力。

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