Investigation of the Hydrological Quality of Ethiope River Watershed, Southern Nigeria

The surface and groundwater resources of the Ethiope river watershed have been investigated for its hydrological and quality characteristics. The results indicate that Ethiope River is perennial and fed by groundwater seepages, precipitation and surface run-off from adjacent areas. The lowest discharge rate of the river is recorded in June and increases steadily reaching its peak in October. The physico-chemical parameters of both water sources include, pH (5.28-7.06), turbidity (1.16 \u2013 8.12 NTU), conductivity (65.00- 127.0 \u3bcs/cm), dissolved oxygen (4.40-7.60 mg/l) and total hardness (25.50 \u2013 45.0 mg/l). Others include, Na+ (3.91 \u2013 27.05 mg/l), K+ (3.91 \u2013 8.73 mg/l), Ca2+ (3.21 \u2013 9.60 mg/l), Mg2+ (1.46- 5.84 mg/l), HCO3- (31.50-80.00 mg/l), Cl- (17.55 \u201335.10 mg/l), SO42- (0.25-0.58 mg/l), NO32- (0.19-0.55 mg/l) and PO42- (0.20-19.00 mg/l). This physico-chemical quality is generally compatible with WHO guideline for domestic use. Nevertheless, the water samples consist of high microbial population including total coliform bacteria counts (39.00 \u2013 1100 MPN/100ml) and Escherichia coli (21.00 \u2013 305.00 MPN/100ml), which render both surface and groundwater unfit for domestic use without disinfection. An assessment of surface water-groundwater homogeneity using the parametric student\u2019s t and F tests on selected constituents (chloride, nitrate, sulphate, phosphate, sodium, potassium, calcium and magnesium), indicate non-significance in the variation within the tested parameters except for nitrate. This suggests some groundwater-surface water intermixing or communication, and the activity of denitrifying bacteria in surface water. A groundwater pollution vulnerability assessment using DRASTIC model indicates moderately high pollution risk level for the aquifer system

Investigation of the Hydrological Quality of Ethiope River Watershed, Southern Nigeria

The surface and groundwater resources of the Ethiope river watershed have been investigated for its hydrological and quality characteristics. The results indicate that Ethiope River is perennial and fed by groundwater seepages, precipitation and surface run-off from adjacent areas. The lowest discharge rate of the river is recorded in June and increases steadily reaching its peak in October. The physico-chemical parameters of both water sources include, pH (5.28-7.06), turbidity (1.16 – 8.12 NTU), conductivity (65.00- 127.0 μs/cm), dissolved oxygen (4.40-7.60 mg/l) and total hardness (25.50 – 45.0 mg/l). Others include, Na+ (3.91 – 27.05 mg/l), K+ (3.91 – 8.73 mg/l), Ca2+ (3.21 – 9.60 mg/l), Mg2+ (1.46- 5.84 mg/l), HCO3- (31.50-80.00 mg/l), Cl- (17.55 –35.10 mg/l), SO42- (0.25-0.58 mg/l), NO32- (0.19-0.55 mg/l) and PO42- (0.20-19.00 mg/l). This physico-chemical quality is generally compatible with WHO guideline for domestic use. Nevertheless, the water samples consist of high microbial population including total coliform bacteria counts (39.00 – 1100 MPN/100ml) and Escherichia coli (21.00 – 305.00 MPN/100ml), which render both surface and groundwater unfit for domestic use without disinfection. An assessment of surface water-groundwater homogeneity using the parametric student’s t and F tests on selected constituents (chloride, nitrate, sulphate, phosphate, sodium, potassium, calcium and magnesium), indicate non-significance in the variation within the tested parameters except for nitrate. This suggests some groundwater-surface water intermixing or communication, and the activity of denitrifying bacteria in surface water. A groundwater pollution vulnerability assessment using DRASTIC model indicates moderately high pollution risk level for the aquifer system

Investigation of the Hydrological Quality of Ethiope River Watershed, Southern Nigeria

The surface and groundwater resources of the Ethiope river watershed have been investigated for its hydrological and quality characteristics. The results indicate that Ethiope River is perennial and fed by groundwater seepages, precipitation and surface run-off from adjacent areas. The lowest discharge rate of the river is recorded in June and increases steadily reaching its peak in October. The physico-chemical parameters of both water sources include, pH (5.28-7.06), turbidity (1.16 – 8.12 NTU), conductivity (65.00- 127.0 μs/cm), dissolved oxygen (4.40-7.60 mg/l) and total hardness (25.50 – 45.0 mg/l). Others include, Na+ (3.91 – 27.05 mg/l), K+ (3.91 – 8.73 mg/l), Ca2+ (3.21 – 9.60 mg/l), Mg2+ (1.46- 5.84 mg/l), HCO3- (31.50-80.00 mg/l), Cl- (17.55 –35.10 mg/l), SO42- (0.25-0.58 mg/l), NO32- (0.19-0.55 mg/l) and PO42- (0.20-19.00 mg/l). This physico-chemical quality is generally compatible with WHO guideline for domestic use. Nevertheless, the water samples consist of high microbial population including total coliform bacteria counts (39.00 – 1100 MPN/100ml) and Escherichia coli (21.00 – 305.00 MPN/100ml), which render both surface and groundwater unfit for domestic use without disinfection. An assessment of surface water-groundwater homogeneity using the parametric student’s t and F tests on selected constituents (chloride, nitrate, sulphate, phosphate, sodium, potassium, calcium and magnesium), indicate non-significance in the variation within the tested parameters except for nitrate. This suggests some groundwater-surface water intermixing or communication, and the activity of denitrifying bacteria in surface water. A groundwater pollution vulnerability assessment using DRASTIC model indicates moderately high pollution risk level for the aquifer system

Major oxides and trace element distributions in coal and coaly shale seams in the Enugu escarpment of South-Eastern Nigeria.

Elemental distributions in nine (9) sub-bituminous coal and four coaly shale samples from the Anambra Basin, southeastern Nigeria were determined using FUS-ICP and TD-ICP spectrometry. Of the major oxides in these samples, SiO2 and Al2O3 indicate the prevalence of quartz and clay minerals. The strong statistical correlation between SiO2 and Al2O3 indicates a common source, likely detrital. The strong correlation between the other major oxides with both SiO2 and Al2O3 indicates that all of these elements have a common detrital source. However, epigenetic carbonates and syngenetic or epigenetic sulphides may also be present. The concentrations of most trace elements in these coals are unremarkably, falling well within the range for U.S. and World coals. These data do not indicate any potential for economic by-product, potential technological problems or environmental or health concerns.KEY WORDS: Nigerian sub-bituminous coal, coaly shale, trace elements, factor and, cluster analyses