1887

Abstract

We are presenting in this paper the relative distributions<br>of horizontal and vertical components of current<br>density in a vertical section of synthetic aquifer<br>simulating different geoelectrical settings. These<br>computations are made using a recently derived general<br>equation for potential field due to a direct current<br>source arbitrarily located in a non-uniform layered<br>medium. On the basis of comparative analysis of<br>computed data we conclude that in case of fresh water<br>saturation, the horizontal current density within the<br>aquifer is greater than the vertical component, for a<br>substratum of resistive nature, and vice-versa for a<br>substratum of conductive nature.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.217.107
2001-10-28
2024-03-28
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.217.107
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error