Estimating the groundwater storage for future irrigation schemes

Presented in this paper is a feasibility study of groundwater for agricultural use (irrigation) in Northern Ghana. The study was conducted using geo-electrical data, boreholes drill logs, results of water quality, and results of the pumping test. The geo-electrical results were to unearth the lithol...

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Autores principales: Shaibu Abdul-Ganiyu, Kpiebaya Prosper
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Lenguaje:EN
Publicado: IWA Publishing 2021
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Acceso en línea:https://doaj.org/article/a2a200131f104f50a294eaf4e565de52
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spelling oai:doaj.org-article:a2a200131f104f50a294eaf4e565de522021-11-06T07:18:45ZEstimating the groundwater storage for future irrigation schemes1606-97491607-079810.2166/ws.2021.041https://doaj.org/article/a2a200131f104f50a294eaf4e565de522021-08-01T00:00:00Zhttp://ws.iwaponline.com/content/21/5/2202https://doaj.org/toc/1606-9749https://doaj.org/toc/1607-0798Presented in this paper is a feasibility study of groundwater for agricultural use (irrigation) in Northern Ghana. The study was conducted using geo-electrical data, boreholes drill logs, results of water quality, and results of the pumping test. The geo-electrical results were to unearth the lithology of the study area; it was found to be underlain with varying geology of both Precambrian and Paleozoic sedimentary formation. These formations consist of phyllite, schist, granite, meta-sediments, and meta-volcanics making up the Precambrian and sandstone, shale, siltstone, mudstones, granitiods also, of the Paleozoic sedimentary. Areas of low resistivity were targeted for drilling per the geophysical results of the profile, values between 24 and 100 ohm.m were zones of probable groundwater occurrence in the study. The groundwater storage capacity and the extractable storage capacity were estimated to be approximately 710,000 km3 and 290,000 km3. The pumping test results acquired from 81 boreholes from the study were used to analyze the sustainability. However, groundwater depth was studied using the Static water level (SWL), areas of SWL around 22 m and 25 m are likely to have a shallow depth whereas areas of 17 m would have deeper groundwater depth. HIGHLIGHTS Groundwater resistivity was determined from the VES values.; The groundwater storage and extractable storage were computed from borehole data.; Overburden thickness suggest thick weathering.; Pumping test reveals the quantity of groundwater discharged.; Groundwater irrigation might be possible per this study.;Shaibu Abdul-GaniyuKpiebaya ProsperIWA Publishingarticlegeo-electricalgroundwaterpaleozoicprecambrianpumpingsedimentaryWater supply for domestic and industrial purposesTD201-500River, lake, and water-supply engineering (General)TC401-506ENWater Supply, Vol 21, Iss 5, Pp 2202-2216 (2021)
institution DOAJ
collection DOAJ
language EN
topic geo-electrical
groundwater
paleozoic
precambrian
pumping
sedimentary
Water supply for domestic and industrial purposes
TD201-500
River, lake, and water-supply engineering (General)
TC401-506
spellingShingle geo-electrical
groundwater
paleozoic
precambrian
pumping
sedimentary
Water supply for domestic and industrial purposes
TD201-500
River, lake, and water-supply engineering (General)
TC401-506
Shaibu Abdul-Ganiyu
Kpiebaya Prosper
Estimating the groundwater storage for future irrigation schemes
description Presented in this paper is a feasibility study of groundwater for agricultural use (irrigation) in Northern Ghana. The study was conducted using geo-electrical data, boreholes drill logs, results of water quality, and results of the pumping test. The geo-electrical results were to unearth the lithology of the study area; it was found to be underlain with varying geology of both Precambrian and Paleozoic sedimentary formation. These formations consist of phyllite, schist, granite, meta-sediments, and meta-volcanics making up the Precambrian and sandstone, shale, siltstone, mudstones, granitiods also, of the Paleozoic sedimentary. Areas of low resistivity were targeted for drilling per the geophysical results of the profile, values between 24 and 100 ohm.m were zones of probable groundwater occurrence in the study. The groundwater storage capacity and the extractable storage capacity were estimated to be approximately 710,000 km3 and 290,000 km3. The pumping test results acquired from 81 boreholes from the study were used to analyze the sustainability. However, groundwater depth was studied using the Static water level (SWL), areas of SWL around 22 m and 25 m are likely to have a shallow depth whereas areas of 17 m would have deeper groundwater depth. HIGHLIGHTS Groundwater resistivity was determined from the VES values.; The groundwater storage and extractable storage were computed from borehole data.; Overburden thickness suggest thick weathering.; Pumping test reveals the quantity of groundwater discharged.; Groundwater irrigation might be possible per this study.;
format article
author Shaibu Abdul-Ganiyu
Kpiebaya Prosper
author_facet Shaibu Abdul-Ganiyu
Kpiebaya Prosper
author_sort Shaibu Abdul-Ganiyu
title Estimating the groundwater storage for future irrigation schemes
title_short Estimating the groundwater storage for future irrigation schemes
title_full Estimating the groundwater storage for future irrigation schemes
title_fullStr Estimating the groundwater storage for future irrigation schemes
title_full_unstemmed Estimating the groundwater storage for future irrigation schemes
title_sort estimating the groundwater storage for future irrigation schemes
publisher IWA Publishing
publishDate 2021
url https://doaj.org/article/a2a200131f104f50a294eaf4e565de52
work_keys_str_mv AT shaibuabdulganiyu estimatingthegroundwaterstorageforfutureirrigationschemes
AT kpiebayaprosper estimatingthegroundwaterstorageforfutureirrigationschemes
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