Groundwater in Nigeria is widely used for domestic, agricultural, and industrial supplies. The Joint Monitoring Programme for Water Supply and Sanitation estimate that in 2018 60% of the total population were dependent on groundwater point sources for their main drinking water source: 73% in rural areas and 45% in urban areas. The cities of Calabar and Port Harcourt are totally dependent on groundwater for their water supply. In 2013, there were around 65,000 boreholes in Nigeria extracting an estimated 6,340,000 m3/day. The majority of these (almost 45,000) were equipped with hand pumps and used for water supply in rural areas and small towns. Estimates of total renewable groundwater resources in Nigeria are variable. The United Nations Food and Agriculture Organization (FAO) estimates that Nigeria has 87,000 Million m3/year of renewable groundwater resources. Japan International Cooperation Agency (JICA) estimate that total annual groundwater recharge is 155,800 Million m3/year. Recharge is variable across the country and largely controlled by climate: recharge is lower in the north of the country due to higher evapotranspiration and lower rainfall.
Groundwater Environments
Geology The geology of Nigeria includes large areas where Precambrian basement rocks are present at the ground surface, and other large areas where the basement rocks are overlain by younger sedimentary rocks. In the north west, these sedimentary rocks largely consist of Tertiary and Cretaceous rocks of the Sokoto Basin (the south eastern part of the Iullemmeden Basin), which are made up of varying amounts of sandstone and clay, with lesser amounts of limestone. In the north east, Tertiary and Quaternary rocks of the Chad Basin comprise sandstone, siltstone and shale. In the centre of Nigeria, along the course of the Benue River and Niger River, are Tertiary and Cretaceous sedimentary rocks of the Benue and Nupe Basins. The Benue Basin consists of continental sandstones overlain by marine and estuarine shales and limestones, while the Nupe Basin largely contains continental sandstones, siltstones, claystones and conglomerates. Along the coast, within the Niger Delta Basin, there are significant unconsolidated sediments of Tertiary to Quaternary age, comprising coarse to medium grained unconsolidated sands and gravels with thin peats, silts, clays and shales.
Basement Aquifers The basement rocks generally form low to moderate productivity aquifers where groundwater flow is concentrated in fractures, and often in a weathered mantle, which can develop in the upper few to tens of metres. Boreholes within basement aquifers are typically drilled to depths of 10–70 m, depending on local conditions. Water quality in these aquifers is generally good.
Sedimentary Aquifers Rocks in the lower, more southerly part, of the Benue Basin form moderately productive aquifers where groundwater flow is concentrated in fractures. Borehole yields typically vary from 2 to 8 litres per second (l/s), but can be much higher or lower than this depending on the degree of fracturing and weathering. Aquifers tend to be localised and unconfined, with boreholes ranging from 40 to 150 m deep. Groundwater from these aquifers can be highly mineralised. Rocks in the Upper Benue Basin typically form low to moderate productivity aquifers, with borehole yields varying between 1 and 5 L/s. Groundwater flow is largely intergranular and boreholes can vary in depth from 30 to 300 m. Groundwater quality is generally good. Rocks in the Nupe Basin form low to moderately productive aquifers. Groundwater flow predominantly occurs through pore spaces in the rocks, which are generally fine grained and slightly cemented, limiting groundwater potential. Where coarser sandstones dominate, yields of 2 to 4 L/s can be achieved; basal conglomerate beds may support higher yields. Borehole yields in rocks of the Sokoto Basin are highly variable, but can be moderate to highly productive where coarser sandstones dominate. Lower sandstones can be confined while upper sandstone layers are typically unconfined. The Chad Formation, found in the Chad Basin, forms a moderate to highly productive aquifer, with yields up to 30 L/s recorded. Groundwater flow is largely intergranular and aquifers can be unconfined or confined depending on local conditions. Deeper sandstone layers are often confined. The Gombe Formation, also in the Chad Basin, has much lower permeability providing yields of around 1 to 5 L/s. Natural water quality from both these formations is generally good.
Igneous Aquifers Volcanic rocks also occur in Nigeria, forming low to moderately productive aquifers. Borehole yields are typically less than 3 L/s and may be drilled to depths of around 15 to 50 m.
Unconsolidated Aquifers Unconsolidated rocks, which predominantly occur in the coastal Niger Delta Basin and along major river valleys, form high to very high productivity aquifers. Alluvial aquifers are largely unconfined with shallow water tables and are thickest (15 – 30 m) along the rivers Niger and Benue. In the Niger Delta Basin, the upper Deltaic Formation is unconsolidated and largely unconfined with a shallow water table (0–10 m below ground level). The older Benin Formation is partly consolidated. It is largely unconfined (locally confined by lower permeability beds) with a water table typically between 3 and 15 m below ground level, but can be as much as 55 m deep. Aquifers in the Niger Delta Basin can provide yields from 3 to 60 L/s with borehole depths ranging from 10 to 800 m. Recharge is mostly directly from rainfall. Water quality issues include salinity, due to intrusion of sea water, iron, and pollution from human activities, particularly in urban areas.
Groundwater Issues
… excerpt ends here. Continue reading the full article.
