利用建模方法对压裂页岩含水层进行灌溉评价;尼日利亚下贝努埃海槽Oju的个案研究

M. Eyankware, C. Ogwah
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引用次数: 4

摘要

摘要:在尼日利亚贝努埃州Oju地区的选定部分,对地下水样本进行了灌溉评估。研究区域位于尼日利亚南部下贝努埃海槽的阿苏河群内。理化参数采用APHA,2012方法进行分析。研究结果表明,研究区域内的pH值在微碱性至酸性范围内,Ec值在127至760μS/cm之间,SSP在1.53至43.78之间,钠百分比在1.55至77.8%之间,凯利比在0.01至0.77之间,镁吸收比在0.00至61.98之间,总硬度在72.00至425.5之间。除LBT/04的MAR、LBT/09、13和14的Na%、01和04的SAR以及LBT/04时的TH略高于各种允许标准值外,上述参数均低于各种灌溉的允许标准值。从吉布斯图中可以观察到,岩石优势是影响地下水的主要因素,除了少数采样点外,还观察到降水优势对研究区域内的地下水有影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Use of Modelling Approach in evaluation of Fractured Shale Aquifers for irrigation purpose; a case study of Oju, Lower Benue Trough Nigeria
Abstract Groundwater samples were evaluated for irrigation purpose, within selected part of Oju area of Benue State, Nigeria. The study area lies within Asu River Group of the Lower Benue Trough, southern part of Nigeria. Physicochemical parameters were analyzed using APHA, 2012 method. Results from the study showed that pH falls within slightly basic to acidic, with Ec value ranging from 127 to 760 μS/cm, SSP ranges from 1.53 to 43.78, Sodium Percentage ranges from 1.55 to 77.8 %, Kelly Ratio ranges from 0.01 to 0.77, Magnesium Absorption Ratio ranges from 0.00 to 61.98 and total hardness Total Hardness ranges from 72.00 to 425.5 within the study area. The above listed parameters were below various permissible standard value for irrigation except for MAR at LBT/04, Na % at LBT/09, 13 and 14, SAR at 01 and 04 and TH at LBT/04 that were slightly above various permissible standard values. From Gibbs plot it was observed that rock dominance is the major factor that influences groundwater except for few sampling point were precipitation dominance was observed to have influence on groundwater within the study area.
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