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宽带介电谱的空间检索。

Spatial Retrieval of Broadband Dielectric Spectra.

机构信息

Department Monitoring and Exploration Technologies, Helmholtz Centre for Environmental Research-UFZ, Permoserstrasse 15, 04318 Leipzig, Germany.

Department of Computational Hydrosystems, Helmholtz Centre for Environmental Research-UFZ, Permoserstrasse 15, 04318 Leipzig, Germany.

出版信息

Sensors (Basel). 2018 Aug 23;18(9):2780. doi: 10.3390/s18092780.

DOI:10.3390/s18092780
PMID:30142965
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6163374/
Abstract

A broadband soil dielectric spectra retrieval approach ( 1 MHz⁻ 2 GHz) has been implemented for a layered half space. The inversion kernel consists of a two-port transmission line forward model in the frequency domain and a constitutive material equation based on a power law soil mixture rule (Complex Refractive Index Model - CRIM). The spatially-distributed retrieval of broadband dielectric spectra was achieved with a global optimization approach based on a Shuffled Complex Evolution (SCE) algorithm using the full set of the scattering parameters. For each layer, the broadband dielectric spectra were retrieved with the corresponding parameters thickness, porosity, water saturation and electrical conductivity of the aqueous pore solution. For the validation of the approach, a coaxial transmission line cell measured with a network analyzer was used. The possibilities and limitations of the inverse parameter estimation were numerically analyzed in four scenarios. Expected and retrieved layer thicknesses, soil properties and broadband dielectric spectra in each scenario were in reasonable agreement. Hence, the model is suitable for an estimation of in-homogeneous material parameter distributions. Moreover, the proposed frequency domain approach allows an automatic adaptation of layer number and thickness or regular grids in time and/or space.

摘要

一种用于分层半空间的宽带土壤介电谱反演方法(1MHz-2GHz)已经实现。反演核由频域中的两端口传输线正向模型和基于幂律土壤混合规则(复折射指数模型-CRIM)的本构材料方程组成。使用基于 Shuffled Complex Evolution(SCE)算法的全局优化方法,利用散射参数的全集合实现了宽带介电谱的空间分布式反演。对于每个层,使用相应的参数厚度、孔隙度、水饱和度和水相孔隙溶液的电导率来反演宽带介电谱。为了验证该方法,使用网络分析仪测量了同轴传输线单元。在四个场景中对逆参数估计的可能性和局限性进行了数值分析。每个场景中预期和反演的层厚度、土壤特性和宽带介电谱都有较好的一致性。因此,该模型适用于不均匀材料参数分布的估计。此外,所提出的频域方法允许自动适应层数量和厚度或在时间和/或空间上的规则网格。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/5cb14b21649c/sensors-18-02780-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/4f466c673737/sensors-18-02780-g0A1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/2a38318934cd/sensors-18-02780-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/5cb14b21649c/sensors-18-02780-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/4f466c673737/sensors-18-02780-g0A1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/2a38318934cd/sensors-18-02780-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2b2/6163374/5cb14b21649c/sensors-18-02780-g002.jpg

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