大地電磁數(shù)據(jù)非線性反演方法研究
[Abstract]:As an important geophysical exploration method, magnetotelluric method has been widely used to study the geological structure of crust and upper mantle, as well as deep mineral exploration. As a bridge between geophysical observation and interpretation, the research of inversion method has always been a hot topic. In this paper, an intelligent optimization algorithm, Drosophila optimization algorithm, is introduced to magnetotelluric data inversion, which avoids the disadvantages of computing partial derivative matrix and dependence on initial model in order to avoid linearization iteration. Drosophila optimization algorithm has the advantages of simple principle, few control parameters and easy programming. Through the analysis of the standard Drosophila optimization algorithm, it is found that the algorithm has slow convergence in dealing with high-dimensional and multi-peak objective functions. It is easy to fall into local extremum, so it is improved by adding the crossover operation and mutation operation of differential evolution algorithm to increase the diversity of Drosophila population and improve the ability of global optimization. At the same time, the variation scale factor is used. In order to achieve the goal of global and local optimization, the fixed search step of Drosophila was changed to a progressively decreasing search step. The improved Drosophila optimization algorithm is tested by several test functions and compared with the results of the standard Drosophila algorithm and the differential evolutionary algorithm. The results show that the improved algorithm has the advantages of fast searching and high precision. The advantage of not being easy to converge prematurely. On this basis, combined with the magnetotelluric inversion theory, the improved Drosophila optimization algorithm is used to inverse the magnetotelluric one-dimensional model, and the algorithm is tested by the model with different noise levels. The results show that the improved algorithm can deal with magnetotelluric data effectively, and the inversion results are accurate and robust. The statistical inversion method based on Bayesian theory is also studied in this paper. The basic principle of nonlinear Bayesian inversion and the common nonlinear numerical sampling methods are summarized and summarized. Bayesian inversion theory regards the parameters of the inversion model as random variables, and the result of inversion is a statistical posteriori probability distribution, which can directly evaluate the results. Based on the idea of variable dimensional inversion, the reversible jump Markov chain Monte Carlo method is used to inverse the one-dimensional magnetotelluric data. The result of Bayesian inversion is based on a large number of samples, so the speed of sampling has an important effect on the algorithm. In order to speed up the convergence of the algorithm, an improved parallel tempering technique is used. By replacing the adjacent exchange between replicas with random switching, the algorithm can quickly sample the whole space and obtain a large number of samples of the solution. The results show that the variable dimension inversion can effectively delaminate the layered media automatically and reduce the interference of human factors effectively. The parallel tempering technique can accelerate the convergence of the sampling process.
【學(xué)位授予單位】:中國地質(zhì)大學(xué)
【學(xué)位級別】:博士
【學(xué)位授予年份】:2017
【分類號】:P631.325
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