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Application of instantaneous profile method to determine the hydraulic conductivity of unsaturated natural stiff clay

机译:瞬时谱法测定不饱和天然僵硬粘土的水力传导性的应用

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In the laboratory, the instantaneous profile method has been routinely applied to determine the hydraulic conductivity of unsaturated compacted clayey soils. But the application of this method is often limited by the large-dimensions of water content probes such as TDR (Time Domaine Reflectometry) probes. Indeed, the existing commercial TDR probes are too large to match the small dimensions of laboratory samples. Furthermore, this method is difficult to be applied to natural stiff clays or other stiff materials (lime/cement treated soils for instance) owing to the surface irregularity created during the sample preparation. The voids between soil surface and testing cell would give rise to side wall leakage during water infiltration under constant-volume condition. This paper attempts to solve these problems by using resistant cohesive filament tape to wrap the soil sample for sidewall leakage prevention and keep the specimen in constant-volume condition. A set of home-made miniature TDR probes were developed for volumetric water content monitoring, together with a set of relative humidity sensors for suction monitoring. As expected, the hydraulic conductivity of stiff Teguline clay which was taken from the area of Albian Paris Basin was found decreasing with the increase of suction. Moreover, the value of hydraulic conductivity at zero suction determined by extrapolation is very close to that determined directly by constant head method. This confirms the promising use of miniature TDR probes in water content monitoring, as well as the effectiveness of resistant filament tape in sidewall leakage prevention under constant-volume condition. The successful incorporation of miniature TDR probes and resistant filament tape extends the common instantaneous profile method to small laboratory samples and stiff materials.
机译:在实验室中,已经常规地应用瞬时轮廓方法以确定不饱和压实粘土土壤的液压导电性。但是该方法的应用通常受到水分概率的大尺寸,例如TDR(时域反射测量仪)探针。实际上,现有的商业TDR探针太大而无法匹配实验室样本的小尺寸。此外,由于在样品制备期间产生的表面不规则性,难以将该方法应用于天然硬壳或其他刚性材料(例如石灰/水泥处理的土壤)。在恒定体积条件下,土壤表面和检测细胞之间的空隙将引起侧壁泄漏过程中的渗透。本文试图通过使用耐粘性细丝带包裹侧壁泄漏预防的土壤样品来解决这些问题,并将样品保持在恒定体积状态下。为体积水含量监测开发了一套自制的微型TDR探针,以及一组相对湿度传感器,用于吸入监测。如所预期的,从吸入的增加时发现从阿尔美尼盆地面积取出的僵硬Teguline粘土的水力导电性。此外,通过外推确定的零抽吸处的液压导电性的值非常接近直接通过恒定的头部确定的。这证实了有希望在水含量监测中使用微型TDR探针,以及在恒定体积条件下侧壁泄漏预防抗性长丝带的有效性。成功掺入微型TDR探头和抗性长丝带将常见的瞬时轮廓方法扩展到小实验室样品和硬质材料。

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