Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers

Groundwater flow of the basement terrains of the Ibarapa region was studied by carrying out pumping test and measurement of borehole inventory. The view was to identify the associated aquifer systems from the time-drawdown curves, quantify the estimable hydraulic properties and develop hypothetical...

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Main Authors: Akanbi Olanrewaju Akinfemiwa, Tijani Moshood ‘Niyi
Format: Article
Language:English
Published: Sciendo 2019-06-01
Series:Materials and Geoenvironment
Subjects:
Online Access:https://doi.org/10.2478/rmzmag-2019-0016
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spelling doaj-063c62567ab4460dbddc2fde101d5c0f2021-09-05T14:01:28ZengSciendoMaterials and Geoenvironment1854-74002019-06-01662879810.2478/rmzmag-2019-0016rmzmag-2019-0016Sustainability and Conceptual Groundwater Hydraulic Models of Basement AquifersAkanbi Olanrewaju Akinfemiwa0Tijani Moshood ‘Niyi1Department of Earth Sciences, Ajayi Crowther University Oyo, Oyo Town, NigeriaDepartment of Geology, University of Ibadan, Ibadan, NigeriaGroundwater flow of the basement terrains of the Ibarapa region was studied by carrying out pumping test and measurement of borehole inventory. The view was to identify the associated aquifer systems from the time-drawdown curves, quantify the estimable hydraulic properties and develop hypothetical models for the understanding of the groundwater flow in the area underlain by diverse crystalline bedrocks. Three aquifer types were identified namely, dual, leaky and regolith. The yield of groundwater in dual and leaky aquifers that dominated terrains underlain by amphibolite and gneisses was sustainable, but the discharge of regolith aquifers mainly associated with migmatite and granite terrains declined at late pumping stage. The transmissivities of the dual and leaky aquifers were between 2.02 and 11.65 m2/day, while those of regolith aquifers were mostly less than 1.00 m2/day. The average aquifer transmissivities in m2/day by bedrocks were: 6.85, 2.57, 0.76 and 1.72, correspondingly. The inter-relationships between transmissivities and groundwater discharge showed diverse aquifer representations, from sustainable high-yielding to unsustainable low-yielding types. Conscientious effort is, therefore, required for well construction in the area.https://doi.org/10.2478/rmzmag-2019-0016groundwaterwell-inventorytime-drawdownaquifer-typesyield
collection DOAJ
language English
format Article
sources DOAJ
author Akanbi Olanrewaju Akinfemiwa
Tijani Moshood ‘Niyi
spellingShingle Akanbi Olanrewaju Akinfemiwa
Tijani Moshood ‘Niyi
Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers
Materials and Geoenvironment
groundwater
well-inventory
time-drawdown
aquifer-types
yield
author_facet Akanbi Olanrewaju Akinfemiwa
Tijani Moshood ‘Niyi
author_sort Akanbi Olanrewaju Akinfemiwa
title Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers
title_short Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers
title_full Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers
title_fullStr Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers
title_full_unstemmed Sustainability and Conceptual Groundwater Hydraulic Models of Basement Aquifers
title_sort sustainability and conceptual groundwater hydraulic models of basement aquifers
publisher Sciendo
series Materials and Geoenvironment
issn 1854-7400
publishDate 2019-06-01
description Groundwater flow of the basement terrains of the Ibarapa region was studied by carrying out pumping test and measurement of borehole inventory. The view was to identify the associated aquifer systems from the time-drawdown curves, quantify the estimable hydraulic properties and develop hypothetical models for the understanding of the groundwater flow in the area underlain by diverse crystalline bedrocks. Three aquifer types were identified namely, dual, leaky and regolith. The yield of groundwater in dual and leaky aquifers that dominated terrains underlain by amphibolite and gneisses was sustainable, but the discharge of regolith aquifers mainly associated with migmatite and granite terrains declined at late pumping stage. The transmissivities of the dual and leaky aquifers were between 2.02 and 11.65 m2/day, while those of regolith aquifers were mostly less than 1.00 m2/day. The average aquifer transmissivities in m2/day by bedrocks were: 6.85, 2.57, 0.76 and 1.72, correspondingly. The inter-relationships between transmissivities and groundwater discharge showed diverse aquifer representations, from sustainable high-yielding to unsustainable low-yielding types. Conscientious effort is, therefore, required for well construction in the area.
topic groundwater
well-inventory
time-drawdown
aquifer-types
yield
url https://doi.org/10.2478/rmzmag-2019-0016
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