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Inferring soil salinity in a drip irrigation system from multi-configuration EMI measurements using adaptive Markov chain Monte Carlo

机译:使用自适应马尔可夫链蒙特卡洛从多配置EMI测量中推断滴灌系统中的土壤盐度

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A substantial interpretation of electromagnetic induction (EMI) measurements requires quantifying optimal model parameters and uncertainty of a nonlinear inverse problem. For this purpose, an adaptive Bayesian Markov chain Monte Carlo (MCMC) algorithm is used to assess multi-orientation and multi-offset EMI measurements in an agriculture field with non-saline and saline soil. In MCMC the posterior distribution is computed using Bayes' rule. The electromagnetic forward model based on the full solution of Maxwell's equations was used to simulate the apparent electrical conductivity measured with the configurations of EMI instrument, the CMD Mini-Explorer. Uncertainty in the parameters for the three-layered earth model are investigated by using synthetic data. Our results show that in the scenario of non-saline soil, the parameters of layer thickness as compared to layers electrical conductivity are not very informative and are therefore difficult to resolve. Application of the proposed MCMC-based inversion to field measurements in a drip irrigation system demonstrates that the parameters of the model can be well estimated for the saline soil as compared to the non-saline soil, and provides useful insight about parameter uncertainty for the assessment of the model outputs.
机译:电磁感应(EMI)测量的基本解释要求量化最佳模型参数和非线性逆问题的不确定性。为此,使用自适应贝叶斯马尔可夫链蒙特卡罗(MCMC)算法来评估在非盐碱土壤和盐渍土壤农业领域中的多方向和多偏移EMI测量。在MCMC中,后验分布是使用贝叶斯规则计算的。使用基于麦克斯韦方程组完全解决方案的电磁正向模型来模拟使用EMI仪器CMD Mini-Explorer的配置测量的视在电导率。通过使用合成数据研究了三层地球模型参数的不确定性。我们的结果表明,在非盐渍土的情况下,与层的电导率相比,层厚度的参数不是非常有用,因此难以解析。提议的基于MCMC的反演在滴灌系统中的现场测量结果表明,与非盐渍土相比,该模型的参数对于盐渍土可以得到很好的估计,并为评估参数不确定性提供了有用的见解模型输出的数量。

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