In the aim of supporting the implementation of basic community infrastructure (drinking water, schools, hospitals), ten hydraulic boreholes with human-powered pumps (HPP) were built in the districts of Kayes and Loudima in the Bouenza department in the southwest of the Republic of Congo. However, there is no study that has assessed the quality of groundwater in this area. The electrical train profiles carried out in the study area revealed several anomalies which are mainly of type (V). The interpretation of the anomalies along the electrical drilling profiles yield to characterize the variation of the thicknesses of the potential aquiferous horizons in units of the Schisto-calcaire Group. Therefore, eight positive drillings having been implemented in the carbonates layers of the Schisto Calcaire Group. The physico-chemical analyses of the groundwater showed that the waters are weakly to moderately mineralize with electrical conductivity values lower than 1000 µS/cm. These waters are divided into two chemical families of waters: chloride sulfate calcic and magnesian and bicarbonate calcic and magnesian. Also, pH and saturation values obtained indicate that the groundwater of the area is aggressive. The major elements of the groundwater in the Madingou-Nkayi-Loudima area have levels below the maximum allowable concentrations defined for drinking water by the WHO. Furthermore, all the sampled water hadvery high levels of heavy metals such as cadmium, and their levels of minor elements (iron, fluorine, copper, aluminum and manganese) at some water points exceed the maximum allowable concentrations defined for drinking water by the World Health Organization. In addition, the study of water suitability for irrigation using the USSL Richards diagram, showed that the groundwater has good quality (class C1-S1) and can be used for irrigation for all types of plants and soils.
Published in | American Journal of Water Science and Engineering (Volume 7, Issue 4) |
DOI | 10.11648/j.ajwse.20210704.13 |
Page(s) | 150-164 |
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Copyright © The Author(s), 2021. Published by Science Publishing Group |
Geophysical and Hydrochemical Study for the Implantation of Ten Boreholes in the Schisto-Limestone Group: Nkayi-Loudima Zone (Bouenza Department)
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APA Style
Essouli Olivier Florent, Malanda Nimy Edmond Nicaise, Miyouna Timothée, Samba Prefina Risiany Rachelle, Matini Laurent, et al. (2021). Geophysical and Hydrochemical Study for the Implantation of Ten Boreholes in the Schisto-Limestone Group: Nkayi-Loudima Zone (Bouenza Department). American Journal of Water Science and Engineering, 7(4), 150-164. https://doi.org/10.11648/j.ajwse.20210704.13
ACS Style
Essouli Olivier Florent; Malanda Nimy Edmond Nicaise; Miyouna Timothée; Samba Prefina Risiany Rachelle; Matini Laurent, et al. Geophysical and Hydrochemical Study for the Implantation of Ten Boreholes in the Schisto-Limestone Group: Nkayi-Loudima Zone (Bouenza Department). Am. J. Water Sci. Eng. 2021, 7(4), 150-164. doi: 10.11648/j.ajwse.20210704.13
AMA Style
Essouli Olivier Florent, Malanda Nimy Edmond Nicaise, Miyouna Timothée, Samba Prefina Risiany Rachelle, Matini Laurent, et al. Geophysical and Hydrochemical Study for the Implantation of Ten Boreholes in the Schisto-Limestone Group: Nkayi-Loudima Zone (Bouenza Department). Am J Water Sci Eng. 2021;7(4):150-164. doi: 10.11648/j.ajwse.20210704.13
@article{10.11648/j.ajwse.20210704.13, author = {Essouli Olivier Florent and Malanda Nimy Edmond Nicaise and Miyouna Timothée and Samba Prefina Risiany Rachelle and Matini Laurent and Boudzoumou Florent and Faye Serigne}, title = {Geophysical and Hydrochemical Study for the Implantation of Ten Boreholes in the Schisto-Limestone Group: Nkayi-Loudima Zone (Bouenza Department)}, journal = {American Journal of Water Science and Engineering}, volume = {7}, number = {4}, pages = {150-164}, doi = {10.11648/j.ajwse.20210704.13}, url = {https://doi.org/10.11648/j.ajwse.20210704.13}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajwse.20210704.13}, abstract = {In the aim of supporting the implementation of basic community infrastructure (drinking water, schools, hospitals), ten hydraulic boreholes with human-powered pumps (HPP) were built in the districts of Kayes and Loudima in the Bouenza department in the southwest of the Republic of Congo. However, there is no study that has assessed the quality of groundwater in this area. The electrical train profiles carried out in the study area revealed several anomalies which are mainly of type (V). The interpretation of the anomalies along the electrical drilling profiles yield to characterize the variation of the thicknesses of the potential aquiferous horizons in units of the Schisto-calcaire Group. Therefore, eight positive drillings having been implemented in the carbonates layers of the Schisto Calcaire Group. The physico-chemical analyses of the groundwater showed that the waters are weakly to moderately mineralize with electrical conductivity values lower than 1000 µS/cm. These waters are divided into two chemical families of waters: chloride sulfate calcic and magnesian and bicarbonate calcic and magnesian. Also, pH and saturation values obtained indicate that the groundwater of the area is aggressive. The major elements of the groundwater in the Madingou-Nkayi-Loudima area have levels below the maximum allowable concentrations defined for drinking water by the WHO. Furthermore, all the sampled water hadvery high levels of heavy metals such as cadmium, and their levels of minor elements (iron, fluorine, copper, aluminum and manganese) at some water points exceed the maximum allowable concentrations defined for drinking water by the World Health Organization. In addition, the study of water suitability for irrigation using the USSL Richards diagram, showed that the groundwater has good quality (class C1-S1) and can be used for irrigation for all types of plants and soils.}, year = {2021} }
TY - JOUR T1 - Geophysical and Hydrochemical Study for the Implantation of Ten Boreholes in the Schisto-Limestone Group: Nkayi-Loudima Zone (Bouenza Department) AU - Essouli Olivier Florent AU - Malanda Nimy Edmond Nicaise AU - Miyouna Timothée AU - Samba Prefina Risiany Rachelle AU - Matini Laurent AU - Boudzoumou Florent AU - Faye Serigne Y1 - 2021/12/24 PY - 2021 N1 - https://doi.org/10.11648/j.ajwse.20210704.13 DO - 10.11648/j.ajwse.20210704.13 T2 - American Journal of Water Science and Engineering JF - American Journal of Water Science and Engineering JO - American Journal of Water Science and Engineering SP - 150 EP - 164 PB - Science Publishing Group SN - 2575-1875 UR - https://doi.org/10.11648/j.ajwse.20210704.13 AB - In the aim of supporting the implementation of basic community infrastructure (drinking water, schools, hospitals), ten hydraulic boreholes with human-powered pumps (HPP) were built in the districts of Kayes and Loudima in the Bouenza department in the southwest of the Republic of Congo. However, there is no study that has assessed the quality of groundwater in this area. The electrical train profiles carried out in the study area revealed several anomalies which are mainly of type (V). The interpretation of the anomalies along the electrical drilling profiles yield to characterize the variation of the thicknesses of the potential aquiferous horizons in units of the Schisto-calcaire Group. Therefore, eight positive drillings having been implemented in the carbonates layers of the Schisto Calcaire Group. The physico-chemical analyses of the groundwater showed that the waters are weakly to moderately mineralize with electrical conductivity values lower than 1000 µS/cm. These waters are divided into two chemical families of waters: chloride sulfate calcic and magnesian and bicarbonate calcic and magnesian. Also, pH and saturation values obtained indicate that the groundwater of the area is aggressive. The major elements of the groundwater in the Madingou-Nkayi-Loudima area have levels below the maximum allowable concentrations defined for drinking water by the WHO. Furthermore, all the sampled water hadvery high levels of heavy metals such as cadmium, and their levels of minor elements (iron, fluorine, copper, aluminum and manganese) at some water points exceed the maximum allowable concentrations defined for drinking water by the World Health Organization. In addition, the study of water suitability for irrigation using the USSL Richards diagram, showed that the groundwater has good quality (class C1-S1) and can be used for irrigation for all types of plants and soils. VL - 7 IS - 4 ER -