大地电磁测深数据一维自动反演

One-dimensional Magnetotelluric Automatic Inversion

在学科实践中,反演是一种相当普遍的手段。地球物理反演则是通过对地面、地下、空间,甚至海洋上的观测(地震仪、重力仪、地电及地磁仪)资料进行分析计算,来推断地球内部介质的地震波速度、密度、电导率等参数的分布,从而得到地球内部介质分布的二维或三维结构图像。本文根据阮百尧教授在其"电阻率激发极化法测深数据的一维最优化反演方法"一文中所述,导出了在大地电磁测深中与电阻率测深一维最优反演相似的反演方法,通过自动迭代反演出地下模型参数。计算表明,这是一种快速和实用的自动反演方法。

In practice, inversion is a method used widely. Geophysics inversion deduces the distribution of seismic-wave speed, density, conductivity and so on in earth interior, then obtains the 2D or 3D structure images for the distribution of earth interior medium, by analyzing the observed date on surface, in subsurface and in space, even on the sea. Referring to the correlate articles by Profession Ruan B.Y, Derived in the magnetotelluric sounding and resistivity sounding similar to the one-dimensional inversion method optimal inversion, Inverted through the automatic iterative model parameters. Calculations show that this is a fast and practical method for the automatic inversion.