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LABORATORY EXPERIMENTS ON WATER MOVEMENT IN A LAYERED SOIL SAMPLE USING TDR METHOD

机译:TDR法研究层状土中水运动的实验研究

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摘要

There is a continuing need to study soil-water movement concepts because of its importance for agriculture considering its influence on plant growth and soil quality. The object of this paper is to study water movement into a layered soil sample packed in a transparent vertical column. The sample was subjected to a wetting from the bottom of the column and a drainage process was following. The column was instrumented with tensiometers (pressure transducers in porous plate housings) to measure pressure and matric water potential and with Time Domain Reflectometry (TDR) probes to measure the volumetric moisture content. The pressure transducers were arranged in four different locations into the column. At the same locations TDR probes of 5 cm in length were installed. Water potential and water content were varying by raising and lowering the water table in the column. Moisture and pressure profiles versus time as well as boundary characteristic curves of hysteresis loop were obtained. The last had good approximation with analytical relationships.
机译:考虑到水-水运移对植物生长和土壤质量的影响,对农业很重要,因此继续需要研究水-水运移的概念。本文的目的是研究水分运动成透明的垂直柱状填充的分层土壤样品。从柱的底部对样品进行润湿,然后进行排水过程。该色谱柱用张力计(多孔板外壳中的压力传感器)测量压力和基质水势,并用时域反射仪(TDR)探针测量体积水分含量。将压力传感器布置在色谱柱中的四个不同位置。在相同位置安装了5厘米长的TDR探针。通过升高和降低塔中的地下水位,可以改变水势和水含量。获得了湿度和压力随时间变化的曲线以及磁滞回线的边界特性曲线。最后一个具有良好的解析关系近似值。

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