HYDROGEOCHEMICAL ASSESSMENT OF CHEMICAL COMPOSITION OF GROUNDWATER; A CASE STUDY OF THE APTIAN-ALBIAN AQUIFER WITHIN SEDIMENTARY BASIN (NIGERIA)

Q2 Engineering
M. Eyankware
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引用次数: 12

Abstract

: The research was carried out to evaluate major source influencing chemical quality of groundwater within suburban area of Abakaliki. It lies between latitudes 6°15' and 6°35'N and longitudes 7°40' and 8°15'E. A total of twenty one (21) groundwater samples were collected and analyzed. Parameter analyzed were; EC, pH, TDS, Cl¯, Na , Mg , NO ¯, SO ¯, Ca , HCO ¯, K , CO ¯ these parameterwere analyzed using American Public + 3 Health Association standard method. Various hydrogeochemical approach and model were used to assess chemical quality of groundwater within the study area. These include; Gibbs, Mg /Ca . End-member, Diamond 2+ 2+ field of Piper and Parson plots were used to indentify major source influencing groundwater chemistry within the study. Finding, from Gibbs plot and Mg /Ca against Mg /Na revealed that rock dominance is the major 2+ 2+ 2+ + process that control groundwater chemistry, while End-member plot showed that silicate and carbonate weathering are the two weathering process that influence groundwater chemistry within the study area. Diamond field of Piper by Lawrence and Bal-Subramanian modified, revealed that groundwater fell within High Ca + Mg & SO + Cl. Parson plot revealed that 65 % of groundwater fell within Ca - Mg – Cl water type, while 4 35 % fells within Ca - Mg - SO . Relationship between TDS vs TH plots showed that groundwater samples fell 4 within soft - fresh water category. The results of the geochemical survey reveal major ionic components trend in other of Mg>Ca>Na>HCO3>SO4>Cl, result reveal that there is no particular trend of ions movement in groundwater.
地下水化学成分的水文地球化学评价;沉积盆地内的阿替安-阿尔比亚含水层实例研究(尼日利亚)
:本研究旨在评估影响阿巴卡利基郊区地下水化学质量的主要来源。它位于北纬6°15'和6°35'之间,经度7°40'和8°15'之间。共采集并分析了二十一(21)个地下水样本。分析的参数包括:;EC、pH、TDS、Cl、Na、Mg、NO、SO、Ca、HCO、K、CO这些参数使用美国公共+3健康协会标准方法进行分析。使用各种水文地球化学方法和模型来评估研究区域内地下水的化学质量。其中包括:;吉布斯,Mg/Ca。Piper和Parson图的端元、Diamond 2+2+域用于确定研究中影响地下水化学的主要来源。根据Gibbs图和Mg/Ca对Mg/Na的发现,岩石优势是控制地下水化学的主要2+2+++过程,而端元图显示硅酸盐和碳酸盐风化是影响研究区内地下水化学的两个风化过程。Lawrence和Bal Subramanian对Piper的Diamond field进行了修改,揭示了地下水属于高Ca+Mg和SO+Cl。Parson图揭示了65%的地下水属于Ca-Mg–Cl水类型,而4 35%的地下水属于Ca-Mg–SO水类型。TDS与TH图之间的关系表明,地下水样品在软淡水类别中下降了4个。地球化学调查结果表明,地下水中主要离子成分的变化趋势为Mg>Ca>Na>HCO3>SO4>Cl,表明地下水中离子的运动没有特别的趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Water Conservation and Management
Water Conservation and Management Engineering-Ocean Engineering
CiteScore
2.90
自引率
0.00%
发文量
0
审稿时长
12 weeks
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