Geology
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Item Assessment of Groundwater Quality for Irrigation Purposes in parts of Minna Sheet 164, North-Central Nigeria(Nigerian Association of Hydrogeologists (NAH) Book of Abstract, 2022-11) Ameh, I. M.; Ibrahim, H. A.; Amadi, A. N.; Dan-Hassan, M. A.; Omanayin, Y. A.; Abubakar, A. E.Assessing groundwater quality for sustainable agricultural through irrigation farming cannot be over-emphasized. Groundwater quality assessment for irrigation purposes was carried out in part of Minna Sheet 164, North-central Nigeria. Borehole samples were collected from boreholes and sent to the laboratory for the following analysis; pH, total dissolved solid and electrical conductance, calcium, magnesium, sodium and potassium, carbonate, sulphate, chlorine and bicarbonate. The pH ranged from 6.5 to 7.4, total dissolved solids varied from 20.4 mg/L to 124.5 mg/L while the electrical conductivity varies from 32.5 µs/cm to 250.0 µs/cm. the concentrations of these physical parameters are important criteria for suitability of water for agricultural purposes as water with low pH, high values of electrical conductivity and total dissolved solids is not good for irrigation. Also, the results of the major cations and anions were converted to meq/l from mg/l and used to determine the following index properties for irrigation water; Sodium Adsorption Ration, Soluble Sodium Percentage, Magnesium Adsorption Ratio, Plasticity Index, Residual Sodium Bicarbonate and Kelly’s Ratio. The values of the computed irrigation quality parameters are within their respective allowable limit for good to excellent water for irrigation use. The study has established that groundwater resources within the study area are suitable for irrigation. It is therefore recommended farmers in these localities should be sensitized to explore groundwater resources in their domain through hand-dug wells or boreholes to supplement the short-lived rain-farming. This will ensure an all year-round farming and availability of farm products and guaranty food security in the state.Item GEOLOGY AND GEOCHEMISTRY OF PEGMATITES OF OGODO – ODOBOLA, NORTH CENTRAL NIGERIA: A STATUS REVIEW(FUDMA Journal of Sciences (FJS), 2022-12) Omanayin, Y. A.; Waziri, N. M.; Onoduku, U. S.; Alabi, A. A.; Amadi, A. N.Pegmatites are an extremely, coarse-grained igneous rocks of granitic composition, constituting of mainly large crystals of quartz, feldspar and mica. Their occurrence cut across various formations, but mostly around granitoids. They are known to host industrial, rare metals, exotic minerals and gemstones of economic value. Due to the continuous demands and recently discovered uses of some of these minerals, its continuous exploration can never be over-emphasized. Pegmatites occurrence in Nigeria were formerly confined to certain quadrants but resent research has proved they also exist in other zones too. Its occurrence in Ogodo-Odobola area is a recent discovery with scantily available literature. The Few available research work conducted on pegmatite of the Ogodo-Odobola area in Kogi State, North central Nigeria has been reviewed. The works focused on its feldspar content for economic value and the latter attempted the mineralization potential of the pegmatites. The area is revealed to be underlain by schistose and granitic lithologies and intruded by the pegmatite dykes of various dimensions. However, recent studies on granitic pegmatites have evolved just as the pegmatites, not only concentrating on their industrial potentials but also on rare metal mineralization potentials which presently are a key to unlocking the future technologically. A few of those relevant and recent studies in the field were also reviewed to bring forth new ways of dealing with this present world cake to geoscientists. White micas are a useful mineral for determining the degree of evolution in pegmatites. This was achieved in the research work using K/Rb ratios paired with incompatible elements such as Cs. Decreasing K/Rb and increasing Cs is a signs of increasing evolution. The modeling of fractional crystallization of white micas in pegmatites using these trace elements determined that the pegmatites are a result of 99% to 99.99% crystallization of a granitic melt. Keywords: Pegmatites, Ogodo-Odobola, White Mica, Kogi State, North Central, Nigeria