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首页> 外文期刊>Hydrology and Earth System Sciences >Hydrogeothermal modelling vs. inorganic chemical composition of thermal waters from the area of Carballi?o (NW Spain)
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Hydrogeothermal modelling vs. inorganic chemical composition of thermal waters from the area of Carballi?o (NW Spain)

机译:Carballi?o地区(西班牙西北部)的热水地热模拟与无机化学成分的关系

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摘要

Hydrothermic features in Galicia (northwest Spain) have been used since ancient times for therapeutic purposes. A characterization of these thermal waters was carried out in order to understand their behaviour based on inorganic pattern and water-rock interaction mechanisms. In this way 15 thermal water samples were collected in the same hydrographical system. The selected thermal water samples were classified using principal component analysis (PCA) and partial least squares (PLS) regression analysis in two groups according to their chemical composition: group I with the young water samples and group II with the samples with longest water-rock contact time. This classification agreed with the results obtained by the use of geothermometers and hydrogeochemical modelling, where the samples were classified into two categories according their residence time in the reservoir and their water-rock interaction.
机译:自古以来,加利西亚(西班牙西北部)就一直使用水热特征。对这些热水进行了表征,以便基于无机模式和水-岩相互作用机理来了解它们的行为。这样,在同一水文系统中收集了15个热水样品。使用主成分分析(PCA)和偏最小二乘(PLS)回归分析,根据化学成分将选定的热水样品分为两组:第一组为年轻水样品,第二组为最长水岩样品联系时间。这种分类与通过使用地热仪和水文地球化学模型获得的结果一致,其中根据样本在储层中的停留时间和水-岩相互作用将样本分为两类。

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