Stochastic inversion of two-layer soil model parameters from electromagnetic induction data

D. Vasić, D. Ambruš, V. Bilas
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引用次数: 3

Abstract

Soil electrical conductivity and magnetic susceptibility are connected to a number of soil properties such as water content, salinity and clay content. Electromagnetic induction (EMI) sensors for geoelectric characterization and mapping of upper soil layers typically consist of a transmitter and several spatially distributed receiver coils. In this paper, we develop a stochastic approach to the inverse problem of determination of electrical conductivity and magnetic susceptibility of two-layered soil, and thickness of its upper layer. As a forward model, we use an analytical truncated-region EMI model with one transmitter and several receiver coils placed horizontally above the soil. For solving the stochastic inversion problem we employ Markov Chain Monte Carlo (MCMC) approach. We illustrate the application of the inversion procedure on a synthetic single-frequency data set obtained from the model of an EMI sensor. Furthermore, we investigate the measurement uncertainty requirements for the sensor. The model and the stochastic inversion approach are suitable for design of EMI sensors and off-line analysis of the EMI data.
基于电磁感应数据的两层土壤模型参数随机反演
土壤电导率和磁化率与土壤的许多性质有关,如含水量、盐度和粘土含量。用于土壤表层地电表征和测绘的电磁感应(EMI)传感器通常由一个发射器和几个空间分布的接收器线圈组成。本文提出了一种求解两层土壤电导率、磁化率及其上层厚度反演问题的随机方法。作为正演模型,我们使用一个解析截断区域电磁干扰模型,其中一个发射器和几个接收器线圈水平放置在土壤上方。为了解决随机反演问题,我们采用了马尔可夫链蒙特卡罗(MCMC)方法。我们举例说明了反演过程在从电磁干扰传感器模型中获得的合成单频数据集上的应用。此外,我们还研究了传感器的测量不确定度要求。该模型和随机反演方法适用于电磁干扰传感器的设计和电磁干扰数据的离线分析。
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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