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对地球物理数据进行成功的反演,依赖于反演方案的先验知识的合理选择,和对模型空间进行有效的参数化,比如模型表示是合理有效的。长期以来,电阻率数据的反演一直是作为非线性或准线性问题来认识的。二维电阻率反演历来是用试错法或线性和线性迭代法来实现的。由于需要事先知道准确的地下界面
The successful inversion of geophysical data depends on the reasonable choice of the prior knowledge of the inversion scheme and the effective parametrization of the model space, such as the model representation is reasonable and effective. For a long time, the inversion of resistivity data has always been recognized as a nonlinear or quasi-linear problem. Two-dimensional resistivity inversion has traditionally been done using trial and error or linear and linear iterations. Due to the need to know in advance accurate underground interface