尼日利亚卡杜纳州Kaura地区含水层保护能力、土壤腐蚀性和Dar-Zarrouk参数估算

I. Olaniyan
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引用次数: 1

摘要

本文对尼日利亚北部卡杜纳州Kaura地区的含水层保护能力、土壤腐蚀性和Dar-Zarrouk参数进行了估算。本研究获取了LGA内20个位置的电阻率测深数据和井泵试验数据。地电资料曲线类型一般为H型、HA型、KH型或K-A-H型,据此圈定了整个研究区的5层岩性。井的产量为16 ~ 400升/分钟,泵送速率为16 ~ 140升/分钟,井降为1 ~ 22m,而比容为1 ~ 95升/分钟。根据覆盖层纵向单位电导值表征含水层的保护能力,35%的位置具有良好的保护能力,其余65%的位置具有中等保护能力。从土壤腐蚀性评价来看,上层土壤有1处为中度腐蚀性,4处为轻度腐蚀性,其余为基本无腐蚀性。根据覆盖层的厚度和电阻率,确定了Dar-Zarrouk参数。反射系数范围为0.29 ~ 0.92,电阻率对比范围为0.35 ~ 25.38,各向异性系数范围为0.70 ~ 3.84,平均值为1.57。高于1.0的值通常被认为是高的,它们更多地出现在该地区的西部,而不是中部和东部。生成了该区域的纵向单位电导图和各向异性系数图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of Aquifer Protective Capacity, Soil Corrosivity and Dar-Zarrouk Parameters in Kaura Area of Kaduna State, Nigeria
This study presents an estimation of aquifer protective capacity, soil corrosivity and Dar-Zarrouk parameters for Kaura area of Kaduna State in northern Nigeria. Electrical resistivity sounding data and borehole pumping test data obtained from 20 locations within the LGA were obtained and used for this study. The geoelectric data exhibited curve types generally consisting of H, HA, KH or K-A-H types from which five-layer lithology were delineated across the entire study area. Well yield varies from 16 – 400 litres/min, pumping rate ranges from 16 to 140 l/min, drawdown varies from 1 – 22m, while specific capacity ranged from 1 – 95 litres/min. The aquifer protective capacity characterization was based on values of longitudinal unit conductance of the overburden, and 35% of the locations showed good protective capacity, while the remaining 65% exhibited moderate protective capacity. From the soil corrosivity evaluation, the upper soil layers were classified as moderately corrosive at one location, four locations were marked as slightly corrosive, while the remaining locations were found to be practically non-corrosive. Based on thicknesses and resistivities of the overburden layers, Dar-Zarrouk parameters were determined. The reflection coefficient ranged from 0.29 to 0.92, resistivity contrast occurred between 0.35 to 25.38, while the coefficient of anisotropy ranged from 0.70 to 3.84 with mean value of 1.57. Values above 1.0 are generally considered high and they occurred more toward the western part of the area than the middle and eastern parts. Both the longitudinal unit conductance map and coefficient of anisotropy map were generated for the area.
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