Hydrochemical interfaces and spatial assessment of Usuma River water quality in North-Central Nigeria

Ogwueleka, Toochukwu Chibueze; Igibah, Ehizemhen Christopher

doi:10.1016/j.sciaf.2020.e00371

Cited by 17 publications

(11 citation statements)

References 21 publications

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“…Similarly, Cadmium occur in the river water owing to corrosion of galvanized plumbing in consort with industrial waste and certain fertilizers contagions. Naturally cadmium ensues in lead, copper ores, zinc, coal, fossil fuels, shales and discharge in the course of volcanic deed [3,5]. Sulphate denotes the physicochemical, leaking of agrarian wastes into the river, excretion, wastewaters from household activities.…”

Section: Impacts Of Principal Component Scrutiny On River Ikpobamentioning

confidence: 99%

“…It means reliant of the chemical nature of the river and the solubility of the aquifer substances via which the river water is flows. Ogwueleka and Igibah (2020) [5] professed that excessive TDS occur via sediment suspension, ion exchange, evaporation, and rainwater. Unmistakably, PC2 connotes the impact of contagion from chemical stimulants /fertilizers or mineral dissolution.…”

Section: Impacts Of Principal Component Scrutiny On River Ikpobamentioning

confidence: 99%

“…They frequently found in river systems as a result of anthropogenic origins, human and volcanic deeds, geological sediments, erosion of both rocks as well as soils. pH a substantial water attribute parameter, serves as controlling factor that defines the types of ion available in water and also displays the potency of the river water to react with either alkaline or acidic substances [5,9,14].…”

Section: Impacts Of Principal Component Scrutiny On River Ikpobamentioning

confidence: 99%

“…With the initiation of more flooding or overflowing and famines, warmer air is produced and excessive water content is held, which in turn makes precipitation styles extreme [3,4]. Streams, rivers, and lakes, which are fundamental resources for farming or agribusiness, industry, and companies and also a source of drinking and household water for people and animals, have been disparagingly influenced by climatic-changeability dynamics [5,6]. Freshwater ecosystems around the globe are already down due to disproportionate pressure from drainage, abstraction, dredging, blockading, contamination, silting, and bellicose species [8,9].…”

Section: Introductionmentioning

confidence: 99%

See 3 more Smart Citations

Modeling the Semivariogram of Climatic Scenario around Rivers by Using Stream Network Mapping and Hydrological Indicator

Agashua

Oluyemi-Ayibiowu

Ihimekpen³

et al. 2022

J. Hum. Earth Future

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Precipitation erosivity propels detrimental hydrological happenings with substantial eco-friendly and socio-economic influences. The conception of the precipitation-vegetation interface is very vital for implementing acclimatization and mitigation techniques for terrestrial bionetworks. Numerous investigations have reconnoitered the spatial correlation of precipitation-vegetation context along the season-precipitation quantity gradient. Here, comprehensive scrutiny of spatio-temporal patterns of climatology-vegetation response to seasonal variability incongruities in River Ikpoba, southern Nigeria, using principal component scrutiny (PCS), semivariogram, cross-validation statistics, spatial distribution mapping, and hydrological indicators for multi-source climatic datasets for pre-impact flow (1913–1966) and post-impact flow (1967–2022). PCS outcomes reveal seven PCs whose eigenvalues were greater than one were hauled out of the twenty-five variables. The River Ikpoba water quality variables displayed a moderately strong rate of spatial reliance, which made it possible to create the spatial distribution map for the carefully chosen water quality variables. Results from further scrutiny of the river Ikpoba flow duration curve show the highest flow rate value between 900–1000cms for the month of October. The post-impact flow's highest value was 65cms in 2008, whereas the pre-impact flow was 64cms. Likewise, 90 days’ minimum highest flow rate was 250cms, 30 days was 1180cms, 7 days was 105cms, and 1 day was 105cms. Whereas the maximum for 1 day was 7200cms, 3 days’ value was 6400cms and 7 days' was 4500cms. This indicates that as the day progressed, the flow rate was increasing for a consecutive 30 days at a low flow rate, but at 90 days it declined. As the day progresses, the values for the maximum value decrease. Doi: 10.28991/HEF-2022-03-01-02 Full Text: PDF

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Section: Impacts Of Principal Component Scrutiny On River Ikpobamentioning

confidence: 99%

Section: Impacts Of Principal Component Scrutiny On River Ikpobamentioning

confidence: 99%

Section: Impacts Of Principal Component Scrutiny On River Ikpobamentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 2 more Smart Citations

Modeling the Semivariogram of Climatic Scenario around Rivers by Using Stream Network Mapping and Hydrological Indicator

Agashua

Oluyemi-Ayibiowu

Ihimekpen³

et al. 2022

J. Hum. Earth Future

View full text Add to dashboard Cite

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“…The studies on water chemistry emphasizing on ions has been conducted globally for determining water quality and its controlling factors by (Sahoo et al 2019;Ayogu et al 2020;Liu et al 2020;Ogwueleka & Christopher 2020). Similarly in India, physicochemical studies of rivers have been conducted by several researchers (Sharma & Subramanian 2008;Gupta et al 2011;Ghosh et al 2019;Patel et al 2020).…”

Section: Introductionmentioning

confidence: 99%

Mechanisms controlling major ion chemistry and its suitability for irrigation of Narmada River, India

et al. 2021

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Surface water chemistry of the upper Narmada River was investigated at 13 different locations for 4 consecutive years (2017 to 2020) during pre- and post-monsoon seasons. The main objective of the study was to identify the processes governing the water chemistry of Narmada River and evaluate its suitability for irrigation. The physical parameters estimated were; pH (7.9 ± 0.4 for pre- and 8 ± 0.4 for post-monsoon seasons), EC (322.8±93.3 μS/cm for pre- and 312.1±80.2 μS/cm for post-monsoon) and TDS (203.4±41.5 mg/L for pre-and 213.4±48 mg/L for post-monsoon). The obtained concentration of cations and anions were in the order of Ca++ > Na+ > Mg++> K+ and HCO3−> Cl−>SO4−> NO3−> PO4− respectively. Thus, the water of Narmada was found to be alkaline in nature. Piper diagram inferred that the water was dominated by Ca-Mg-HCO3− type of hydrochemical faces. Gibb's plot clarified that rock-water interaction regulates the ion chemistry of the Narmada. Various indices like sodium percentage (Na%), sodium absorption ration (SAR), Kelly index (Ki), permeability index (PI), magnesium hazard (MH) was calculated which showed that the surface water was suitable for irrigation. Lastly, one-way ANOVA (p < 0.05) confirmed no significant differences in water quality except for temperature, EC and SO4−, for pre- and post-monsoon season.

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Comparison of Water Quality Parameters in Two Regions (Northern Cameroon, Central Africa) Based on Statistical Tools

Djimi,

Belibi Belibi,

Soh

et al. 2023

Advances in Science, Technology &Amp; Innovation

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Hydrochemical interfaces and spatial assessment of Usuma River water quality in North-Central Nigeria

Cited by 17 publications

References 21 publications

Modeling the Semivariogram of Climatic Scenario around Rivers by Using Stream Network Mapping and Hydrological Indicator

Modeling the Semivariogram of Climatic Scenario around Rivers by Using Stream Network Mapping and Hydrological Indicator

Mechanisms controlling major ion chemistry and its suitability for irrigation of Narmada River, India

Comparison of Water Quality Parameters in Two Regions (Northern Cameroon, Central Africa) Based on Statistical Tools

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