Comparative Hydrological and Geoelectrical Study on the Quaternary Aquifer in the Deltas of Wadi Badaa and Ghweiba, El Ain El Sukhna Area, Northwest Suez Gulf, Egypt
Table 2
The ranges of the resistivities and the corresponding thicknesses of the geoelectrical layers.
Geoelectrical layer
Resistivity range (Ohm·m)
Thickness range (m)
Lithological description
Minimum
Maximum
Minimum
Maximum
A
140
30605
0.9
3.1
Surface layer
B1
27
506.5
7
38.6
Dry Quaternary deposit (sand and gravels)
B2
21.02
45.8
78.4
101.7
Saturated Quaternary zone consist from clayey sand
