Assessment of groundwater quality for irrigation purposes in ilesha West local government, Osun State, Nigeria

IF 8.7 Q1 Environmental Science Water Cycle Pub Date : 2022-01-01 DOI:10.1016/j.watcyc.2022.10.001
Olusola O. Fadipe , Abiola U. Adebanjo , Mubarak O. Thanni , Oluwole A. Olawuyi
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引用次数: 1

Abstract

This study assessed the suitability of different groundwater resources in a basement complex of Ilesha West Local Govt. Area (LGA) for irrigation purposes. A total of 207 water samples were collected from hand-dug wells, boreholes and springs during the peak periods of wet and dry seasons. The physicochemical characteristics (pH, total dissolved solids (TDS), electrical conductivity (EC), Alkalinity, Hardness), basic cations, anions (Ca2+, Mg2+, Na+, K+, HCO3, SO42−, Cl, NO3) and heavy metals (Pb2+, Cr2+, Fe2+ and As5+) present were determined. The results were subjected to irrigation quality models such as sodium adsorption ratio (SAR), Kelly ratio (KR), sodium hazard (SH), permeability index (PI) and magnesium hazard (MH). To reveal the hydro-geochemical facies of the groundwater, Piper and Durov diagrams were plotted using the geochemist workbench sheet (GWB) software. A maximum SAR value of 6.0197 was recorded in the hand-dug wells during the dry season and the mean concentration of Cr2+ was observed to be higher than the recommended limits for irrigation. The percentage suitability of the water sources for irrigation purposes are 76%, 94%, 46% and 96% for SH, PS, KR, and MH models, respectively. Piper and Durov's diagrams revealed Na++ K+ (80%), Ca+ (90%) and HCO3 ​+ ​CO3, Cl. as the dominant cations, and anions respectively. Additional Hydro-geochemical plots revealed intermixing of the cations and anions, suggesting the dissolution of carbonate and silicate minerals from the parent soil or rock. Generally, the groundwater in the study area is suitable for irrigation, but the sustainability based on quantity should be investigated.

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尼日利亚奥孙州伊莱沙西部地方政府灌溉用地下水水质评估
本研究评估了伊勒沙西部地方政府辖区地下综合设施不同地下水资源的灌溉适宜性。在干湿季节的高峰期,从手挖井、钻孔和泉水共采集了207个水样。测定了其理化性质(pH、总溶解固形物(TDS)、电导率(EC)、碱度、硬度)、碱性阳离子、阴离子(Ca2+、Mg2+、Na+、K+、HCO3−、SO42−、Cl−、NO3−)和重金属(Pb2+、Cr2+、Fe2+、As5+)。采用钠吸附比(SAR)、凯利比(KR)、钠危害(SH)、渗透指数(PI)和镁危害(MH)等灌溉质量模型对结果进行了分析。为了揭示地下水的水文地球化学相,使用地球化学工作台表(GWB)软件绘制了Piper和Durov图。旱季手挖井的SAR最大值为6.0197,Cr2+的平均浓度高于灌溉建议限值。SH、PS、KR和MH模式的水源灌溉适宜度分别为76%、94%、46%和96%。Piper和Durov的图显示Na++ K+ (80%), Ca+(90%)和HCO3−+ CO3−,Cl−。分别为优势阳离子和阴离子。另外的水文地球化学图显示了阳离子和阴离子的混合,表明碳酸盐和硅酸盐矿物从母质土壤或岩石中溶解。研究区地下水总体上适合灌溉,但需对其水量可持续性进行研究。
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来源期刊
Water Cycle
Water Cycle Engineering-Engineering (miscellaneous)
CiteScore
9.20
自引率
0.00%
发文量
20
审稿时长
45 days
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