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Device for laboratory determination of unsaturated hydraulic conductivity of porous material

机译:实验室测定多孔材料不饱和导水率的装置

摘要

The present invention relates to a device (Fig. 2) for the laboratory determination of unsaturated hydraulic conductivity of the porous material that is adapted to measure the time dependence of the impedance changes of a porous material (e.g., soil) at its saturation with water, and which is characterized in that it consists of at least one pair electrodes that are placed on the surface or just below the surface of the at least one soil sample (7) taken in the withdrawal rollers (2) and inserted into the chambers (4) and (5) to set the potential of moisture .FI..sub.1. n. and .FI..sub.2.n., whereby the device is accompanied by another electrical conductor (8), connecting the electrodes to the inputs of the multiplexer (9) and through to the inputs of a measuring bridge (11), when the periodic change of channel address (10) of the multiplexer (9) generated by the generator (14) cyclic addresses, which is controlled by the time generator (15) and data logger (13) monitors the impedance of the currently connected electrode pair i-th measured sample (7).
机译:本发明涉及一种用于实验室确定多孔材料的不饱和水力传导率的装置(图2),该装置适于测量多孔材料(例如土壤)在其饱和时的阻抗变化与时间的关系。 ,其特征在于,它由至少一对电极组成,这些电极放置在抽取辊(2)中的至少一个土壤样本(7)的表面上或表面正下方,并插入到腔室( 4)和(5)设置潜在的水分。 。和.FI.sub.2.n。,其中该设备随附有另一个电导体(8),将电极连接到多路复用器(9)的输入,并连接到测量电桥(11)的输入,当由时间发生器(15)和数据记录器(13)控制的,由发生器(14)生成的多路复用器(9)的通道地址(10)的周期性变化和循环地址监控时,配对第i个测量样本(7)。

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