However, the inversion parameters can be modified by the user. The program will automatically choose the optimum inversion parameters for a data set. It supports the Wenner, Schlumberger, pole-pole, pole-dipole, dipole-dipole, multiple gradient and non-conventional arrays. On a modern PC, the inversion of a single pseudosection is usually completed within seconds to minutes. It is completely automatic and the user does not even have to supply a starting model. The RES2DINV圆4 programs use the smoothness-constrained Gauss-Newton least-squares inversion technique (Sasaki 1992) to produce a 2D model of the subsurface from the apparent resistivity data. Two-dimensional (2D) electrical imaging surveys are now widely used to map areas of moderately complex geology where 1D resistivity sounding surveys are inadequate. RES2DINV圆4 - 2D RESISTIVITY & IP INVERSION software.
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