尼日利亚Song及其周边地区地下水潜力地电测量

A. Yakubu, A. Nur
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摘要

摘要在尼日利亚阿达马瓦州的Song及周边地区进行了17次垂直电测深(VES)研究,采用斯伦贝谢配置,电流电极间距为AB/2 = 80m。16台VES显示三层地球模型;而剩下的是四层地球模型。第一层平均厚度2m,平均电阻率75.14Ωm;代表表层土壤和粘土材料。第二层平均厚度为12.09m,平均电阻率为50.0Ωm。该层为疏松、风化/断裂基底。第三层平均电阻率值为5150Ωm,代表新鲜基底。水样采集自7口钻孔(BH)和4口手挖井(HDW)。综合评价该地区的采样水,平均pH值为5.8,平均温度为28.96℃,平均浊度值为0.453NTU,平均电导率值为159.39µs/cm。水大多是酸性的,温度适中,浑浊。总硬度平均值为98.78mg/l,为中等软质水质。研究区所有手挖井硝酸盐和总大肠菌群浓度均较高,分别为50.93 ~ 67.17mg/l和12cfu ~ 27cfu/ml。高价值可归因于人为活动,如施用化肥和在该地区任意倾倒家庭固体废物以及动物和人类粪便。BH4由于深度较浅,总大肠菌群数量也较高。除了HDW和BH4的深度较浅外,地下水总体上对人类以及工农业用途都是有益的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geoelectrical Survey for Groundwater Potential in Song and Environs NE, Nigeria 
Abstract: Seventeen Vertical Electrical soundings (VES) using the Schlumberger configuration with current electrode spacing of AB/2 = 80m were carried out in Song and environs of Adamawa State of Nigeria to study the groundwater potential. Sixteen VES showed a three-layer earth model; while the remaining one has four-layer earth model. The average thickness of the first layer is 2m with a mean resistivity of 75.14Ωm; representing the top soil and clay material. The second layer has an average thickness of 12.09m with a mean resistivity of 50.0Ωm. This layer is unconsolidated and highly weathered/fractured basement. The average resistivity value of the third layer is 5150Ωm and represents the fresh basement. Water samples were collected from Seven Boreholes (BH) and four Hand-Dug wells (HDW). The overall assessment of the sampled water in the area indicates an average pH value of 5.8, mean temperature of 28.96°C, an average turbidity value of 0.453NTU, and with a mean conductivity value of 159.39µs/cm. The water is mostly acidic with a moderate temperature, and turbidity. Total hardness has an average value of 98.78mg/l indicating a moderately soft water quality. All the Hand-Dug wells in the study area have high concentration of Nitrate and total Coliform count of 50.93mg/l to 67.17mg/l and 12cfu/ml to 27cfu/ml respectively. The high value can be attributed to anthropogenic activities such as chemical fertilizer application and indiscriminate dumping of house hold solid waste in the area as well as animals and human faeces. The high concentration of total coliform count was also observed in BH4 because of the shallow depth. Apart from the HDW and BH4 that are of shallow depth, the groundwater is generally good for human as well as industrial and agricultural uses.
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