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Particle swarm optimization and least squares method for geophysical parameter inversion from magnetic anomalies data

机译:粒子群优化和最小二乘法从磁异常数据中的地球物理参数反演

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The geophysical parameter inversion from magnetic anomalies data usually faces a non-linear optimization problem with multi-variable, multi-objective function extremum, multi-solution and so on. Therefore, it is necessary that the more stable and efficient algorithms is used in the geophysical inversion. Particle swarm optimization (PSO) has been used in the geophysical inversion. However, for high-dimensional, multi-peak function problems in magnetic anomalies data inversion, the effect using PSO method is not good, and it easy to fall into the local minimum. In this paper, we propose PSO and least squares method (LS) to solve magnetic anomalies data parameter optimized inversion. This method exploited to initialize non-linear parameter estimation using by PSO, and LS is used for accurate local search. We compare the results from PSO and proposed PSO-LS to invert the synthesized potential field. The results show that PSO-LS outperform PSO in terms of accuracy.
机译:来自磁异常数据的地球物理参数反演通常面临着多变量,多目标函数极值,多解决方案等的非线性优化问题。因此,在地球物理反演中使用更稳定和高效的算法是必要的。粒子群优化(PSO)已用于地球物理反演。但是,对于磁异常数据反转中的高维,多峰值功能问题,使用PSO方法的效果不好,并且易于落入局部最小值。在本文中,我们提出了PSO和最小二乘法(LS)来解决磁异常数据参数优化的反演。这种方法利用PSO初始化非线性参数估计,LS用于准确的本地搜索。我们将PSO的结果与提出的PSO-LS进行比较,以反转合成的潜在领域。结果表明,PSO-LS在准确性方面优于PSO。

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