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利用多元统计方法评估尼日利亚南部的水化学相和地表水水质动态

Evaluation of hydro-chemical facies and surface water quality dynamics using multivariate statistical approaches in Southern Nigeria.

作者信息

Ubuoh E A, Nwogu F U, Ossai-Abeh E Q, Ikwuemesi J C, Oke A O, Umoh J D

机构信息

Department of Environmental Management and Toxicology, Michael Okpara University of Agriculture, Umudike, Nigeria.

Department of Fisheries and Aquatic Management, Michael Okpara University of Agriculture, Umudike, Nigeria.

出版信息

Sci Rep. 2024 Dec 30;14(1):31600. doi: 10.1038/s41598-024-77534-z.

DOI:10.1038/s41598-024-77534-z
PMID:39738172
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11685720/
Abstract

The geochemical and chemical constituents of river water quality could be influenced by human activities and organic processes like water interacting with the lithogenic structure that the river flows through. Evaluating evidence based primary root of the predominant pollutant ions, their interactions as well as the factors controlling their dominance is crucial in studies regarding water environment and hydrology especially as most studies focus on theoretical methods. In order to understand the water cycle, safeguard surface water resources, and preserve the human environment, this study evaluated surface water hydro-chemical facies, quality dynamics, and portability in southern Nigeria using multivariate statistical approaches by analyzing selected hydro-chemical characteristics as indicators of pollution along the river during wet and dry seasons. Twenty water samples were taken, analyzed, and subjected to mathematical statistics: Gibbs plot, trilinear piper analysis, stiff pattern analysis, ionic scatter analysis, correlation, and principal component analysis. Result of surface water recorded mean pH ranges from 4.8 for wet season and 5.3 for dry season, above the WHO, and during dry season TDS, Mg Pb, and Cd were above the WHO limits, respectively. Abundance of cation and anion in surface water was in a decreasing trend of: HCO > Ca > Mg > Cl > Na > SO > K + > NO. Trilinear plot, stiff pattern, and Gibbs ratio indicated hydrochemical facie of water dominated by calcium bicarbonate (Ca-HCO) water type. From plots and ionic ratio, the major hydrochemical process of water chemistry during wet and dry seasons was rock-water interaction arising majorly from weathering processes. Ionic ratios of Ca and Mg, Ca and HCO [1:2], Ca + Mg and HCO + SO4 [1:1], revealed dissolution of dolomite as their common origin, with total cations in wet and dry seasons ranging between 43 and 57% and total anions: 37.3-62.7, with dry season dominance. The overall WQI of the river seemed good quality due to rapid flow and self-purification of the river but may be harmful in the future. It was recommended that constant surveillance and monitoring of human activities along waterways be enforced in order to ensure that undesirable pollution levels don't occur in the river.

摘要

河水水质的地球化学和化学成分可能会受到人类活动以及诸如水与河流流经的岩石成因结构相互作用等有机过程的影响。在水环境和水文学研究中,评估主要污染离子的基于证据的主要根源、它们的相互作用以及控制其优势地位的因素至关重要,尤其是因为大多数研究侧重于理论方法。为了理解水循环、保护地表水资源并维护人类环境,本研究采用多变量统计方法,通过分析选定的水化学特征作为河流在湿季和干季污染指标,评估了尼日利亚南部地表水的水化学相、水质动态和便携性。采集了20个水样进行分析,并进行了数学统计:吉布斯图、三线派珀分析、刚性模式分析、离子散射分析、相关性分析和主成分分析。地表水结果显示,湿季平均pH值范围为4.8,干季为5.3,高于世界卫生组织标准,且在干季,总溶解固体、镁、铅和镉分别高于世界卫生组织限值。地表水中阳离子和阴离子的丰度呈以下递减趋势:碳酸氢根>钙>镁>氯>钠>硫酸根>钾>硝酸根。三线图、刚性模式和吉布斯比率表明,水的水化学相以碳酸氢钙(Ca-HCO)水型为主。从图表和离子比率来看,湿季和干季水化学的主要水化学过程是岩石-水相互作用,主要源于风化过程。钙与镁、钙与碳酸氢根[1:2]、钙+镁与碳酸氢根+硫酸根[1:1]的离子比率表明,白云石的溶解是它们的共同来源,湿季和干季的总阳离子含量在43%至57%之间,总阴离子含量在37.3%至62.7%之间,干季占主导。由于河流流速快和自净能力,河流的总体水质指数似乎良好,但未来可能会有害。建议对沿水道的人类活动进行持续监测,以确保河流中不会出现不良污染水平。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/907a/11685720/14ebeaab2cd8/41598_2024_77534_Fig12_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/907a/11685720/0b12ce744c9e/41598_2024_77534_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/907a/11685720/89aab6710347/41598_2024_77534_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/907a/11685720/672f3a7e4a07/41598_2024_77534_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/907a/11685720/fa8e3ae9f30b/41598_2024_77534_Fig11_HTML.jpg
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