3D-FEM modeling of F/TDR sensors for clay-rock water content measurement in combination with broadband dielectric spectroscopy

T. Bore, N. Wagner, S. Delepine-Lesoille, F. Taillade, G. Six, F. Daout, D. Placko
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引用次数: 3

Abstract

The use of electromagnetic sensors such as Time Domain Reflectometry (TDR) probes has gained increasing importance for long term monitoring of the water content in radioactive waste repositories. TDR probes are sensitive to changes in electromagnetic properties of the surrounding material, a clay rock in our case. Prior to the in situ application, it is mandatory to have an accurate relationship between the electromagnetic properties of the intact host clay rock and the water content. For this purpose, the dielectric properties of intact clay rock samples were systematically studied at frequencies from 1 MHz to 10 GHz with network analyzer technique in combination with coaxial transmission line cells. Samples were conditioned to achieve a water saturation range from 16 % to nearly saturation. The relaxation behavior was quantified based on a generalized fractional relaxation model under consideration of an apparent direct current conductivity assuming three relaxation processes: a high-frequency water process and two interfacial processes which are related to interactions between the aqueous pore solution and mineral particles (adsorbed/hydrated water relaxation, counter ion relaxation and Maxwell-Wagner effects). In a second step, these data are introduced in 3-D numerical frequency domain finite element field calculations to model the one port broadband frequency or time domain transfer function for a three rode based TDR-probe embedded in the clay rock. The results are analyzed with classical travel time analysis (onset/inflection) which under/overestimates the value of the permittivity compared to effective permittivity at 1 GHz. Indeed, apparent permittivity contains not only the water-content contribution but also effects due to water-mineral interaction processes. The results demonstrate the capabilities of a combined TD/FD analysis procedure for the monitoring of physical and chemical properties of materials with high frequency electromagnetic sensor techniques.
结合宽带介电光谱的F/TDR粘土-岩石含水量传感器三维有限元建模
电磁传感器的使用,如时域反射(TDR)探针,对于放射性废物储存库中水含量的长期监测越来越重要。TDR探头对周围材料的电磁特性变化很敏感,在我们的例子中是粘土岩石。在原位应用之前,必须准确了解完整的宿主粘土岩石的电磁特性与含水量之间的关系。为此,利用网络分析仪技术结合同轴传输线单元,系统地研究了完整粘土岩石样品在1 MHz至10 GHz频率范围内的介电特性。样品被调节到水饱和度范围从16%到接近饱和。基于广义分数弛豫模型,在考虑表观直流电导率的情况下,假设三个弛豫过程:一个高频水过程和两个与水孔溶液与矿物颗粒相互作用有关的界面过程(吸附/水合水弛豫、反离子弛豫和麦克斯韦-瓦格纳效应),对弛豫行为进行了量化。第二步,将这些数据引入到三维数值频域有限元场计算中,对嵌入粘土岩石中的三探针的单端口宽带频域或时域传递函数进行建模。用经典的旅行时间分析(起始/拐点)对结果进行了分析,该分析低估/高估了1 GHz时的介电常数与有效介电常数的值。事实上,视介电常数不仅包含水含量的贡献,还包含水-矿物相互作用过程的影响。结果表明,结合TD/FD分析程序可以利用高频电磁传感器技术监测材料的物理和化学性质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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