Geophysical survey and radiometric assessment of aquifer strata and vulnerable groundwater quality of Ukwuani Ommunities in Delta State

E.O. Esi, O. Akpoyibo
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Abstract

The study assessed the aquifer strata and groundwater quality of Obeti, Umuaja, and Ebedei communities of Ukwuani, Delta State, Nigeria using electrical resistivity technique and sodium iodide [Na(TI)] detector. The electrical resistivity technique revealed that lithology has five to six geoelectric strata, which ranged from topsoil to clay formations with thickness of 0.6 to 6.0 m sits and aquifer resistivity range of 182.1– 6032.0 Ωm with depth of 29–70 m. These ranges indicate significant changes in the aquifer level and sufficient reservoirs for groundwater. To assess the activity concentrations of 238U, 232Th and 40K at the aquifer depth of 29–70 m groundwater, a total of fifteen groundwater samples were collect for analysis and the mean results are 9.00±1.24Bql−1, 4.82±2.95Bql−1 and 57.93±4.20Bql−1 respectively. These results are all above world threshold limits. However, the computed mean radiological health risk values for radium equivalent (Raeq), representative index (Iy), external hazard index (Hin), internal hazard index (Hex), absorbed dose rate (D), annual effective dose equivalent (AEDE), outdoor and indoor, and excess lifetime cancer risk (ELCR) outdoor and indoor are 20.35±5.78 Bql−1, 0.15mSvy−1, 0.056mSvy−1, 0.08mSvy−1, 9.55μGyh−1, 11.71mSvy−1, 46.84mSvy−1and 0.04×10−3, 0.16×10−3 and 0.20×10−3 for the addition of (ELCR) outdoor and indoor respectively. The computed mean radiological values are below world threshold limits. Hence, the studied communities’ drinking groundwater is safe radiologically. It is advised that government, oil and gas operators and individuals should drill above 30 m depth for quality groundwater and should be treated before usage. These values will serve as baseline data.  
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三角洲州 Ukwuani 社区含水层地层和脆弱地下水质量的地球物理勘测和辐射测量评估
这项研究使用电阻率技术和碘化钠[Na(TI)]检测器评估了尼日利亚三角洲州 Ukwuani 的 Obeti、Umuaja 和 Ebedei 社区的含水层地层和地下水质量。电阻率技术显示,岩性有五到六个地电层,从表土层到粘土层,厚度从 0.6 米到 6.0 米不等,含水层电阻率范围为 182.1- 6032.0 Ωm,深度为 29-70 米。为评估含水层 29-70 米地下水中 238U、232Th 和 40K 的放射性浓度,共采集了 15 个地下水样本进行分析,平均结果分别为 9.00±1.24Bql-1、4.82±2.95Bql-1 和 57.93±4.20Bql-1。这些结果均高于世界阈值限值。然而,镭当量(Raeq)、代表性指数(Iy)、外部危害指数(Hin)、内部危害指数(Hex)、吸收剂量率(D)、室外和室内年有效剂量当量(AEDE)以及室外和室内超终生癌症风险(ELCR)的计算平均辐射健康风险值为 20.35±5.78Bql-1、0.15mSvy-1、0.056mSvy-1、0.08mSvy-1、9.55μGyh-1、11.71mSvy-1、46.84mSvy-1 以及室外和室内(ELCR)分别为 0.04×10-3、0.16×10-3 和 0.20×10-3。计算得出的平均辐射值低于世界阈值限值。因此,研究社区的饮用地下水在辐射方面是安全的。建议政府、石油和天然气运营商和个人应在 30 米以上的深度钻探优质地下水,并在使用前进行处理。这些数值将作为基准数据。
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