Oxide Analysis of River Bed Sediments from Lower Reaches of River Forcados along Patani and Environ
DOI: 10.23977/geors.2024.070109 | Downloads: 6 | Views: 207
Author(s)
Edirin Akpofure 1, Ufuoma E. Odeji 1
Affiliation(s)
1 Department of Geology, Niger Delta University, Wilberforce Island, Bayelsa State, Nigeria
Corresponding Author
Edirin AkpofureABSTRACT
The river bed sediments of River Forcados along Patani and environs were sampled and taken to the laboratory for bulk analysis using XRD. It was observed that the sediments were silty clay to coarse sand. The sediment colour range from brown to grey. SiO2 was observed to be the most abundant oxide with a concentration ranging from 58.660% to 84.258% with an average of 72.955%. The sediments are enriched in the following oxides: Sio2, Al2O3, Fe2O3, K2O, MgO, CaO and TiO2. Whereas, the sands are depleted in the following oxides: V2O5, Cr2O3, MnO. Co3O4, NiO. CuO, Nb2O3, MoO3, WO3, P2O5, SO3, BaO, Ta2O5, ZnO, Ag2O, Cl, ZrO2, SnO2. Sodium in oxide form (NaO) or elemental form (Na) is not observed because its concentration is below detection limit of 0.01%. The SiO2/Al2O3 ratio and the K2O,/NaO ratios show that the sediments are mineralogically mature and have an acidic igneous rock source.
KEYWORDS
Oxide Analysis, River Bed, Weathering, Source Rock, Sediment Maturity, RiversCITE THIS PAPER
Edirin Akpofure, Ufuoma E. Odeji, Oxide Analysis of River Bed Sediments from Lower Reaches of River Forcados along Patani and Environ. Geoscience and Remote Sensing (2024) Vol. 7: 75-81. DOI: http://dx.doi.org/10.23977/geors.2024.070109.
REFERENCES
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