尼日利亚西南部基底复合区浅层地下水水文地球化学特征及脆弱性评价

Adeniyi JohnPaul Adewumi, A. Anifowose, F. O. Olabode, T. Laniyan
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引用次数: 19

摘要

摘要对乌沃地区35份地下水样品进行了理化参数分析。结果表明:pH平均值为6.32,TDS为208.92 mg/l,温度为28.77℃,EC为545.16 μs/cm;TH为111.09 mg/l, SO4为71.73 mg/l, Cl为0.07 mg/l, HCO3为14.09 mg/l, Na为25.06 mg/l, Ca为37.07 mg/l, K为24.36 mg/l, mg为4.41 mg/l。将结果与WHO和NDSQW标准进行比较。除OW6井的EC外,其余参数均在允许范围内,69%的样品中K高于规定标准。钾的高浓度与该地区用于农业用途的氮磷钾肥料有关。地下水分别属于Ca-Na-K-SO4和Na-Ca-SO4水型。地下水中的离子浓度是由构成含水层的岩石溶解造成的。斜长石和含硅酸盐的岩石是水中主要离子的来源。SAR、PI、RSBC和KR表明该地区地下水适合灌溉。DRASTIC模型进一步揭示了该地区地下水在当前环境条件下不容易受到污染。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeochemical Characterization and Vulnerability Assessment of Shallow Groundwater in Basement Complex Area, Southwest Nigeria
Abstract Thirty-five (35) groundwater samples from Owo area were analyzed for physicochemical parameters. Results show that the mean value of pH is 6.32, TDS is 208.92 mg/l, temperature is 28.77°C, EC is 545.16 μs/cm; TH is 111.09 mg/l, SO4 is 71.73 mg/l, Cl is 0.07 mg/l, HCO3 is 14.09 mg/l, Na is 25.06 mg/l, Ca is 37.07 mg/l, K is 24.36 mg/l and Mg is 4.41 mg/l. The results were compared to the WHO and NDSQW standards. All parameters were within the permissible limit except EC in well OW6 and K is above the stipulated standards in 69% of the total samples. The high concentration of K is linked to the use of NPK fertilizer in the area for agricultural purposes. The groundwater belongs to Ca-Na-K-SO4 and Na-Ca-SO4 water type respectively. The ionic concentration in the groundwater is due to the dissolution of the rock that makes up the aquifer. Plagioclase and silicate-bearing rocks are the sources of major ions in the water. SAR, PI, RSBC and KR reveals that groundwater in the area is good for irrigation purpose. DRASTIC model further revealed that groundwater in the area is less vulnerable to contamination under the current environmental conditions.
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