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首页> 外文期刊>Ingenieria y Ciencia >Análisis de las características fisicoquímicas del agua subterránea de la cuenca del río Chicú, Colombia, usando indicadores hidroquímicos y estadística multivariante
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Análisis de las características fisicoquímicas del agua subterránea de la cuenca del río Chicú, Colombia, usando indicadores hidroquímicos y estadística multivariante

机译:使用水化学指标和多元统计数据分析哥伦比亚奇库伊河流域地下水的理化特性

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摘要

The hydrochemical characteristics of an intramontane basin, located in the Bogotá Savannah, were evaluated using indicators and statistical methods, based on 10 monitoring wells physicochemical data, obtained during two sampling campaigns conducted in 2014, to establish the hydrochemical characteristics that are generated by the groundwater and sedimentary matrix interaction of the aquifer and determine the extracted groundwater quality conditions’ in the studied aquifer. To analyze the data, (1) hydrochemical indicators were applied to evaluate the groundwater and the sedimentary matrix interaction processes’ in the studied aquifer, which was corroborated by (2) principal components analysis, which allowed to disclose strong associations between the variables?(Na+, Mg2+, Ca2+, SO42-?y HCO3-),?and T, pH y TDS variables influence on the hydrochemical process that govern the analyzed aquifer, in addition (3) physicochemical parameters were compared with the Colombian environmental regulations, referring to human consumption and irrigation use.?As results, in water-sediment matrix was determined reverse cation exchange and minerals meteorization processes, present in the formations that conform the analyzed aquifer, likewise, the water samples obtained do not present quality characteristics that allow its use for irrigation or human consumption.
机译:根据2014年两次采样活动中获得的10口监测井的理化数据,使用指标和统计方法对位于波哥大萨凡纳的山内盆地的水化学特征进行了评估,以建立地下水产生的水化学特征与含水层的沉积基质相互作用,并确定所研究含水层中提取的地下水水质条件。为了分析数据,(1)用水化学指标评估研究含水层中的地下水和沉积基质相互作用过程,(2)主成分分析证实了这一点,从而揭示了变量之间的强关联? Na +,Mg2 +,Ca2 +,SO42-γyHCO3-)和T,pH y TDS变量对控制所分析含水层的水化学过程的影响,此外(3)将理化参数与哥伦比亚的环境法规进行了比较,结果,在水-沉积物基质中确定了与被分析含水层相符的地层中存在的反向阳离子交换和矿物质气象化过程,同样,所获得的水样也没有允许使用的质量特征。用于灌溉或人类消费。

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