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Determination of the spatial TDR-sensor characteristics in strong dispersive subsoil using 3D-FEM frequency domain simulations in combination with microwave dielectric spectroscopy

机译:确定强空间TDR传感器的空间特性   使用3D-FEm频域模拟组合的分散地基   用微波介电谱

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摘要

The spatial sensor characteristics of a 6cm TDR flat band cable sensorsection was simulated with finite element modelling (High Frequency StructureSimulator-HFSS) under certain conditions: (i) in direct contact to thesurrounding material (air, water of different salinities, different syntheticand natural soils (sand-silt-clay mixtures)), (ii) with consideration of adefined gap of different size filled with air or water and (iii) the cablesensor pressed at a borehole-wall. The complex dielectric permittivity orcomplex electrical conductivity of the investigated saturated and unsaturatedsoils was examined in the frequency range 50MHz-20GHz at room temperature andatmospheric pressure with a HP8720D- network analyser. Three soil-specificrelaxation processes are assumed to act in the investigatedfrequency-temperature-pressure range: one primary (main water relaxation) andtwo secondary processes due to clay-water-ion interactions (bound waterrelaxation and the Maxwell-Wagner effect). 3D finite element simulation isperformed with a 1/3 wavelength based adaptive mesh refinement at a solutionfrequency of 1MHz, 10MHz, 0.1GHz, 1GHz and 12.5GHz. The electromagnetic fielddistribution, S-parameter and step responses were examined.
机译:在某些条件下,采用有限元建模(High Frequency StructureSimulator-HFSS)模拟了6cm TDR扁平带电缆传感器部分的空间传感器特性:(i)直接接触周围的物质(空气,不同盐度的水,不同的合成土壤和天然土壤) (砂-粘土-粘土混合物),(ii)考虑到充满空气或水的不同尺寸的确定间隙,以及(iii)将电缆传感器压在井壁上。使用HP8720D网络分析仪,在室温和大气压下,在50MHz-20GHz的频率范围内,检查了所研究的饱和和不饱和土壤的复介电常数或复电导率。假定在所研究的频率-温度-压力范围内,三种土壤特定的松弛过程起作用:一个主要(主水弛豫)和两个次要过程,这是由于粘土-水-离子相互作用(结合水松弛和麦克斯韦-瓦格纳效应)引起的。使用基于1/3波长的自适应网格细化在1MHz,10MHz,0.1GHz,1GHz和12.5GHz的求解频率下执行3D有限元仿真。检查了电磁场分布,S参数和阶跃响应。

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