On the role of the J-E constitutive relationship in applied geoelectromagnetism
Main Article Content
Abstract
In current applications of the Induced Polarization (IP) method, the Debye and Cole-Cole models are used to study
relaxation and dispersion properties of rocks, though it is believed that this type of modelisation is confused and
vague, because of the lack of a background physical description. In this paper, we show that the Debye model
can physically be deduced as a consequence of the electrodynamic behaviour of a mixture of bound and unbound
charged particles immersed in an external electric field. We also clarify that the Cole-Cole model is a synthetic
model, which can physically be explained as a continuous distribution of Debye terms.
relaxation and dispersion properties of rocks, though it is believed that this type of modelisation is confused and
vague, because of the lack of a background physical description. In this paper, we show that the Debye model
can physically be deduced as a consequence of the electrodynamic behaviour of a mixture of bound and unbound
charged particles immersed in an external electric field. We also clarify that the Cole-Cole model is a synthetic
model, which can physically be explained as a continuous distribution of Debye terms.
Article Details
How to Cite
1.
Patella D. On the role of the J-E constitutive relationship in applied geoelectromagnetism. Ann. Geophys. [Internet]. 2003Dec.25 [cited 2022Aug.14];46(3). Available from: https://www.annalsofgeophysics.eu/index.php/annals/article/view/3430
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