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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.
Issue: Vol 3 No 4 (2000)
Page No.: 22-30
Published: Apr 30, 2000
Section: Article
DOI: https://doi.org/10.32508/stdj.v3i4.3551
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