Abstract

Via two common earth resistivity measurment methods, i.e. the Wenner method and the driven rod method. This paper develops a new thesis on earth resistivity as a complex function which not only varies itself with the frequency w and the relaxation time contant , but also has its parameters σ and ε varying with  in the shape (j)= [σ() + j.()]-1. Results of the analysis are presented on diagrams and may be applied in a number of specific cases.