GEOELECTRICAL ASSESSMENT OF GROUNDWATER POTENTIAL OF KEANA AREA NORTHCENTRAL NIGERIA
- 1. University of Nigeria
 - 2. University of Maiduguri
 - 3. Federal University Lafia
 
Description
This work was undertaken to unravel the hydro geophysical characteristics of Keana metropolis Nasarawa State, northcentral Nigeria. This study aims to assess and determine the sustainability of groundwater resources in Keana Town by using geoelectric techniques to collect data and analyze subsurface characteristics that can assist identify suitable sites for groundwater extraction. Once accomplished, it will give useful information for groundwater resource management and contribute to Keana's long-term growth. Fifteen (15) Vertical Electrical Sounding (VES) data with a maximum electrode spacing of (AB/2) of 200 meters were acquired using the Schlumberger electrode configuration. The VES data were interpreted using the conventional partial curve matching technique to obtain initial model parameters, which were used as input for computer iterative modelling using the IPI2WINTM software. The study revealed three (3) to six (6) geo-electric layers with underlying indurated sandstone and shale beds in some areas. In the study area, the apparent resistivity of the aquifer ranges from 32.4 to 407 m, with a depth ranging from 30 to 120m. Information extracted from iso-resistivity models and geoelectric cross sections revealed sandy strata with an exception around the northern portion i.e., around Federal Government Girls College Keana (FGGC) where a thick layer of shale is envisaged, extending to over 150 m depth with an average apparent resistivity value of 35Ω m. Thus, making the section fair to poor groundwater potential. However, this research has aided in delineating the groundwater potential of the area into three distinct zones.
Translated Descriptions
Translated Description (Arabic)
تم تنفيذ هذا العمل لكشف الخصائص الجيوفيزيائية المائية لمدينة كيانا بولاية ناساراوا، شمال وسط نيجيريا. تهدف هذه الدراسة إلى تقييم وتحديد استدامة موارد المياه الجوفية في مدينة كيانا باستخدام التقنيات الكهربائية الأرضية لجمع البيانات وتحليل الخصائص تحت السطحية التي يمكن أن تساعد في تحديد المواقع المناسبة لاستخراج المياه الجوفية. وبمجرد الانتهاء من ذلك، سيوفر معلومات مفيدة لإدارة موارد المياه الجوفية والمساهمة في نمو كيانا على المدى الطويل. تم الحصول على خمسة عشر (15) بيانات السبر الكهربائي العمودي (VES) مع تباعد أقصى للإلكترود يبلغ (AB/2) 200 متر باستخدام تكوين إلكترود شلمبرجير. تم تفسير بيانات VES باستخدام تقنية مطابقة المنحنى الجزئي التقليدية للحصول على معلمات النموذج الأولية، والتي تم استخدامها كمدخل للنمذجة التكرارية للكمبيوتر باستخدام برنامج IPI2WINTM. كشفت الدراسة عن ثلاث (3) إلى ست (6) طبقات جيولوجية كهربائية مع طبقات رملية وصخرية متجذرة في بعض المناطق. في منطقة الدراسة، تتراوح المقاومة الظاهرية لطبقة المياه الجوفية من 32.4 إلى 407 م، بعمق يتراوح من 30 إلى 120 م. كشفت المعلومات المستخرجة من نماذج المقاومة المتساوية والمقاطع العرضية الجيوكهربية عن طبقات رملية مع استثناء حول الجزء الشمالي، أي حول كلية البنات التابعة للحكومة الفيدرالية (FGGC) حيث يتم تصور طبقة سميكة من القشرة، تمتد إلى عمق أكثر من 150 مترًا بمتوسط قيمة مقاومة واضحة تبلغ 35 Ω م. وبالتالي، فإن جعل القسم عادلًا لإمكانات المياه الجوفية الضعيفة. ومع ذلك، فقد ساعد هذا البحث في تحديد إمكانات المياه الجوفية للمنطقة إلى ثلاث مناطق متميزة.Translated Description (English)
This work was undertaken to unravel the hydro geophysical characteristics of Keana metropolis Nasarawa State, northcentral Nigeria. This study aims to assess and determine the sustainability of groundwater resources in Keana Town by using geoelectric techniques to collect data and analyse subsurface characteristics that can assist identify suitable sites for groundwater extraction. Once accomplished, it will give useful information for groundwater resource management and contribute to Keana's long-term growth. Fifteen (15) Vertical Electrical Sounding (VES) data with a maximum electrode spacing of (AB/2) of 200 meters were acquired using the Schlumberger electrode configuration. The VES data were interpreted using the conventional partial curve matching technique to obtain initial model parameters, which were used as input for computer iterative modelling using the IPI2WINTM software. The study revealed three (3) to six (6) geo-electric layers with underlying indurated sandstone and shale beds in some areas. In the study area, the apparent resistivity of the aquifer ranges from 32.4 to 407 m, with a depth ranging from 30 to 120 m. Information extracted from iso-resistivity models and geoelectric cross sections revealed sandy strata with an exception around the northern portion i.e., around Federal Government Girls College Keana (FGGC) where a thick layer of shell is envisaged, extending to over 150 m depth with an average apparent resistivity value of 35Ω m. Thus, making the section fair to poor groundwater potential. However, this research has aided in delineating the groundwater potential of the area into three distinct zones.Translated Description (French)
This work was undertaken to unravel the hydro geophysical characteristics of Keana metropolis Nasarawa State, northcentral Nigeria. Cette étude vise à évaluer et à déterminer la durabilité des ressources en eau souterraine dans la ville de Keana en utilisant des techniques géoélectriques pour collecter des données et analyser les caractéristiques de la surface de substitution qui peuvent aider à identifier les sites appropriés pour l'extraction de l'eau souterraine. Une fois accompli, il fournira des informations utiles pour la gestion des ressources en eau du sol et contribuera à la croissance à long terme de Keana. Fifteen (15) Vertical Electrical Sounding (VES) data with a maximum electrode spacing of (AB/2) of 200 meters were acquired using the Schlumberger electrode configuration. The VES data were interpreted using the conventional partial curve matching technique to obtain initial model parameters, which were used as input for computer itérative modelling using the IPI2WINTM software. The study revealed three (3) to six (6) geo-electric layers with underlying indurated sandstone and shale beds in some areas. Dans la zone d'étude, la résistivité apparente des gammes d'aquifères de 32,4 à 407 m, avec un rang profond de 30 à 120 m. Informations extraites des modèles iso-résistifs et des sections transversales géoélectriques révélées strates sablonneuses avec une exception autour de la portion nord de l'unité centrale, autour du Federal Government Girls College Keana (FGGC) où une couche épaisse de l'étendue est envisagée, étendant jusqu'à plus de 150 m de profondeur avec une valeur moyenne de résistivité apparente de 35Ω m. Thus, rendant la section équitable au potentiel d'eau de fond pauvre. However, this research has aidd in delineating the groundwater potential of the area into three distinct zones.Translated Description (Spanish)
This work was undertaken to unravel the hydro geophysical characteristics of Keana metropolis Nasarawa State, northcentral Nigeria. This study aims to assess and determine the sustainability of groundwater resources in Keana Town by using geoelectric techniques to collect data and analyze subsurface characteristics that can assist identify suitable sites for groundwater extraction. Once accomplished, it will give useful information for groundwater resource management and contribute to Keana 's long-term growth. Fifteen (15) Vertical Electrical Sounding (ves) data with a maximum electrode spacing of (AB/2) of 200 meters were acquired using the Schlumberger electrode configuration. The ves data were interpreted using the conventional partial curve matching technique to obtain initial model parameters, which were used as input for computer iterative modelling using the IPI2WINTM software. The study revealed three (3) to six (6) geo-electric layers with underlying indurated sandstone and shale beds in some areas. In the study area, the apparent resistivity of the aquifer ranges from 32.4 to 407 m, with a depth ranging from 30 to 120m. Information extracted from iso-resistivity models and geoelectric cross sections revealed sandy strata with an exception around the northern portion i.e., around Federal Government Girls College Keana (FGGC) where a thick layer of shale is envisaged, extending to over 150 m depth with an average apparent resistivity value of 35Ω m. Thus, making the section fair to poor groundwater potential. However, this research has aided in delineating the groundwater potential of the area into three distinct zones.Additional details
Additional titles
- Translated title (Arabic)
 - التقييم الجيولوجي لإمكانات المياه الجوفية في منطقة كيانا الشمالية في نيجيريا
 - Translated title (English)
 - GEOELECTRICAL ASSESSMENT OF GROUNDWATER POTENTIAL OF KEANA AREA NORTHCENTRAL NIGERIA
 - Translated title (French)
 - GEOELECTRICAL ASSESSMENT OF GROUNDWATER POTENTIAL OF KEANA AREA NORTHCENTRAL NIGERIA
 - Translated title (Spanish)
 - GEOELECTRICAL ASSESSMENT OF GROUNDWATER POTENTIAL OF KEANA AREA NORTHCENTRAL NIGERIA
 
Identifiers
- Other
 - https://openalex.org/W4393907383
 - DOI
 - 10.26480/mjg.02.2023.126.133