Improving the resolution of Non-Invasive Time Domain Reflectometry

I. Platt, I. Woodhead
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引用次数: 2

Abstract

Non invasive time domain reflectometry (TDR) may be used to estimate the volumetric moisture content, thetasv, with depth for a variety of sample materials. The forward physical model is couched in terms of a moments method where integration is performed over a discretised sample space to estimate the measured propagation time, tp down a pair of parallel transmission lines. We show that inverse solution to this, which recovers relative permittivity and thus thetasv, is greatly facilitated by a simplification of the system geometry via, 1) realistically modeling the prior density of the sample, 2) using this prior with the inherent system symmetry to reduce the number of required discretisation cells, and 3) determining a physically meaningful reduction operator to allow a coarse discretisation mesh to be used. The observational equation is expressed in the Bayesian paradigm with the most accurate and robust solution obtained using the conditional mean of the posterior distribution constructed via a Monte Carlo method. Results of simulation show that the method is capable of providing accurate estimates of the moisture density profile down to a depth of 100 mm with an error < 4%. Further, the reduction in the number of discretised cells required to accurately estimate these profiles means that the inversion procedure is quick enough to enable the real time application of the equipment, a fundamental requirement in the development.
提高非侵入式时域反射仪的分辨率
非侵入性时域反射法(TDR)可用于估计各种样品材料的体积水分含量,即随深度的tasv。正演物理模型以矩量方法表示,其中在离散样本空间上进行积分以估计测量的传播时间,沿着一对平行传输线。我们表明,通过简化系统几何结构,极大地促进了这一问题的逆解,它恢复了相对介电常数,从而恢复了tasv, 1)实际地模拟了样品的先验密度,2)使用该先验与固有的系统对称性来减少所需的离散单元的数量,以及3)确定一个物理上有意义的约简算子,以允许使用粗离散网格。观测方程用贝叶斯范式表示,用蒙特卡罗方法构造后验分布的条件均值得到最精确和鲁棒的解。仿真结果表明,该方法能够准确估计深度为100 mm的水分密度分布,误差< 4%。此外,准确估计这些剖面所需的离散单元数量的减少意味着反演过程足够快,可以实现设备的实时应用,这是开发中的基本要求。
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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