阿尔及利亚Oued-Fodda大坝水化学季节变化的评估

IF 0.9 Q4 ENVIRONMENTAL STUDIES Environmental & Socio-Economic Studies Pub Date : 2021-09-01 DOI:10.2478/environ-2021-0019
A. Bouderbala
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引用次数: 0

摘要

摘要本研究对阿尔及利亚西部Oued Fodda大坝的地表水进行了研究,旨在评估化学特征的季节变化,以确定控制该大坝地表水矿化的过程。结果显示,在2009年至2013年的研究期间,大多数参数发生了显著变化,表明水呈微碱性,属于SO4-Cl-Ca-Mg水类型。主成分分析(PCA)和聚类分析(CA)用于解释所分析的参数与地表水污染的可能来源之间的相关性。水饱和指数(SI)的计算表明,水相对于岩盐(NaCl)不饱和,相对于其他矿物平衡。尽管EC、TDS、SO42-、Cl-、Ca2+、Mg2+等物理化学参数的时间变化表明,该大坝的物理化学参数和水量(WV)之间存在反向调整,这可以通过硅酸盐和碳酸盐矿物的风化来解释,但通过使用离子比、图表和散点图以及多元统计技术,这些都是合理的。相反,对该大坝有机水污染水平的评估显示,水质从中度污染到重度污染。
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Assessment of the seasonal variations in hydrochemistry of Oued Fodda dam, Algeria
Abstract This study was carried out on the surface water of Oued Fodda dam in western Algeria, and aimed to evaluate the seasonal variations of chemical characteristics with the aim to define the processes controlling the mineralization of surface water in this dam. The results showed significant variations in the majority of parameters during the study period from 2009 to 2013, indicating slightly alkaline water, and a SO4-Cl-Ca-Mg water type. Principal component analysis (PCA) and cluster analysis (CA) were used to explain the correlations between the parameters analysed, and the probable sources of surface water contamination. The calculation of saturation indices (SI) of water indicated undersaturated water with respect to halite (NaCl), and equilibrium with respect to the other minerals. While, the temporal variation of physico-chemical parameters such as EC, TDS, SO42-, Cl-, Ca2+, Mg2+ indicated a reverse adjustment between physico-chemical parameters and water volumes (WV) in this dam, which can be explained by the weathering of silicate and carbonate minerals, these were justified by the use of ionic ratios, diagrams and scatter plots and multivariate statistical techniques. Conversely, evaluation of the organic water pollution level in this dam showed a water quality from moderately to severely polluted.
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来源期刊
CiteScore
2.20
自引率
0.00%
发文量
18
审稿时长
12 weeks
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