<abstract xmlns="http://www.w3.org/1999/xhtml">

<p>Clean drinking water supply is a major concern to the population of the urban municipality of Boké, Republic of Guinea. This study is aimed to investigate the favourable geological structure for the accumulation of groundwater in Boké. Apparent resistivity data was collected by using the Schlumberger-type vertical electrical sounding technique. The apparent resistivity values were obtained on a bi-logarithmic scale in which the distances AB/2 were plotted on the abscissa and the resistivities are on the ordinate. It found the number of terrains and their characteristics (resistivity and thickness) in the area and the behaviour of the current in the soil through a curve. The results show that the structures favourable to the accumulation of groundwater were fractured dolerites, cracked shales and cracked or crushed sandstones. The sandstones were the most important in terms of the amount of water. They are located at a depth of more than 100 metres. It was also found that dolerites and shales are located at shallower depths (less than 100 m).</p>
</abstract>

Clean drinking water supply is a major concern to the population of the urban municipality of Boké, Republic of Guinea. This study is aimed to investigate the favourable geological structure for the accumulation of groundwater in Boké. Apparent resistivity data was collected by using the Schlumberger-type vertical electrical sounding technique. The apparent resistivity values were obtained on a bi-logarithmic scale in which the distances AB/2 were plotted on the abscissa and the resistivities are on the ordinate. It found the number of terrains and their characteristics (resistivity and thickness) in the area and the behaviour of the current in the soil through a curve. The results show that the structures favourable to the accumulation of groundwater were fractured dolerites, cracked shales and cracked or crushed sandstones. The sandstones were the most important in terms of the amount of water. They are located at a depth of more than 100 metres. It was also found that dolerites and shales are located at shallower depths (less than 100 m).

Identification of favourable geological formations for the determination of groundwater

Materials and Geoenvironment

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Prepoznavanje geoloških formacij, ugodnih za akumulacijo podzemne vode

Clean drinking water supply is a major concern to the population of the urban municipality of Boké, Republic of Guinea. This study is aimed to investigate the...

Identification of favourable geological formations for the determination of groundwater

Article Category: Original Scientific Article

Pubblicato online: 04 set 2023

Pagine: 15 - 31

Ricevuto: 05 mar 2022

Accettato: 24 mar 2022

DOI: https://doi.org/10.2478/rmzmag-2021-0015

Parole chiave
Groundwater, geo-electric method, lithological section, fracture zones, Prefecture of Boké

© 2022 Moussa Diallo et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

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Identification of favourable geological formations for the determination of groundwater

Article Category: Original Scientific Article

Pubblicato online: 04 set 2023

Pagine: 15 - 31

Ricevuto: 05 mar 2022

Accettato: 24 mar 2022

DOI: https://doi.org/10.2478/rmzmag-2021-0015

Parole chiaveGroundwater, geo-electric method, lithological section, fracture zones, Prefecture of Boké

© 2022 Moussa Diallo et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Figure 1

Figure 2

Figure 3

Figure 4

Figure 5

Figure 6

Figure 7

Figure 8

Figure 9

Figure 10

Figure 11

Figure 12

Figure 13

Figure 14

Figure 15

Figure 16

Figure 17

Parole chiave
Groundwater, geo-electric method, lithological section, fracture zones, Prefecture of Boké