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Determination of the Soil-Water Retention Curve and the Hydraulic Conductivity Function Using a Small Centrifuge

机译:用小型离心机测定土壤保水曲线和水导率函数

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An alternative methodology for direct determination of the soil-water retention curve (SWRC) and evaluation the hydraulic conductivity of the unsaturated soil was developed using a commercially available small centrifuge with a swinging type rotor assembly without inflight instrumentation. The testing procedure consists of spinning up four initially saturated soil specimens until constant water content is achieved for a given angular speed. The soil - suction relationship is determined by relating the respective water content to the suction magnitude induced by the ceramic plate at the specimen's base. The hydraulic conductivity of the unsaturated soil is estimated by dividing the cumulative flow rate measured at each angular speed by the respective hydraulic gradient applied at specimen's middle height. This methodology was applied for evaluating the SWRC of a residual gneissic soil profile using both, undisturbed and remolded soil specimens. The results show good agreement to other well established methodologies such as filter-paper method, porous plate funnel and suction plate extractor. The determined unsaturated hydraulic conductivities magnitudes were compared to the theoretical predicted values given by the Mualem - van Genuchten model (van Genuchten, 1980) indicating good agreement. Overall, it can be concluded that the methodology proposed ensures good agreement in determining the SWRC and the hydraulic conductivity of studied soils.
机译:使用市售的小型离心机和不带机上仪表的摆动式转子组件,开发了一种直接确定土壤保水曲线(SWRC)和评估不饱和土壤水力传导率的替代方法。测试程序包括旋转四个最初饱和的土壤样本,直到在给定的角速度下达到恒定的含水量为止。土壤-吸力关系是通过将各自的水含量与样品底部陶瓷板引起的吸力值相关联来确定的。不饱和土壤的水力传导率是通过将在每个角速度下测得的累积流量除以在试样中间高度处施加的相应水力梯度来估算的。该方法适用于使用未扰动和重塑的土壤样本评估残留片麻质土壤剖面的SWRC。结果表明与其他公认的方法学(如滤纸法,多孔板漏斗和吸板萃取器)具有良好的一致性。将确定的非饱和水力传导率幅度与Mualem-van Genuchten模型(van Genuchten,1980)给出的理论预测值进行比较,表明吻合良好。总的来说,可以得出结论,所提出的方法确保了在确定研究土壤的SWRC和水力传导率方面的良好一致性。

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