Faculty of Geology and Geoenvironment, University of Athens, Athens 15784, Greece.
Sci Total Environ. 2014 Apr 1;476-477:577-90. doi: 10.1016/j.scitotenv.2014.01.042. Epub 2014 Feb 1.
The present study involves an integration of the hydrogeological, hydrochemical and isotopic (both stable and radiogenic) data of the groundwater samples taken from aquifers occurring in the region of northeastern Peloponnesus. Special emphasis has been given to health-related ions and isotopes in relation to the WHO and USEPA guidelines, to highlight the concentrations of compounds (e.g., As and Ba) exceeding the drinking water thresholds. Multivariate statistical analyses, i.e. two principal component analyses (PCA) and one discriminant analysis (DA), combined with conventional hydrochemical methodologies, were applied, with the aim to interpret the spatial variations in the groundwater quality and to identify the main hydrogeochemical factors and human activities responsible for the high ion concentrations and isotopic content in the groundwater analysed. The first PCA resulted in a three component model, which explained approximately 82% of the total variance of the data sets and enabled the identification of the hydrogeological processes responsible for the isotopic content i.e., δ(18)Ο, tritium and (222)Rn. The second PCA, involving the trace element presence in the water samples, revealed a four component model, which explained approximately 89% of the total variance of the data sets, giving more insight into the geochemical and anthropogenic controls on the groundwater composition (e.g., water-rock interaction, hydrothermal activity and agricultural activities). Using discriminant analysis, a four parameter (δ(18)O, (Ca+Mg)/(HCO3+SO4), EC and Cl) discriminant function concerning the (222)Rn content was derived, which favoured a classification of the samples according to the concentration of (222)Rn as (222)Rn-safe (<11 Bq·L(-1)) and (222)Rn-contaminated (>11 Bq·L(-1)). The selection of radon builds on the fact that this radiogenic isotope has been generally related to increased health risk when consumed.
本研究整合了来自伯罗奔尼撒半岛东北部地区含水层的地下水样本的水文地质、水文化学和同位素(稳定和放射性)数据。特别关注与世界卫生组织和美国环保署指南有关的与健康有关的离子和同位素,以突出超过饮用水阈值的化合物(如 As 和 Ba)的浓度。应用了多元统计分析,即两个主成分分析(PCA)和一个判别分析(DA),结合常规水文化学方法,旨在解释地下水质量的空间变化,并确定导致地下水高离子浓度和同位素含量的主要水文地球化学因素和人为活动。第一个 PCA 得出了一个三成分模型,该模型解释了数据集总方差的约 82%,并确定了导致同位素含量(即 δ(18)O、氚和 (222)Rn)的水文地质过程。第二个 PCA 涉及水样中痕量元素的存在,揭示了一个四成分模型,该模型解释了数据集总方差的约 89%,更深入地了解了地下水成分的地球化学和人为控制(例如,水-岩相互作用、热液活动和农业活动)。使用判别分析,得出了一个涉及(δ(18)O、(Ca+Mg)/(HCO3+SO4)、EC 和 Cl)的四个参数的(222)Rn 含量判别函数,该函数有利于根据(222)Rn 的浓度对样本进行分类,即(222)Rn-安全(<11 Bq·L(-1))和(222)Rn-污染(>11 Bq·L(-1))。选择氡的原因是,这种放射性同位素通常与摄入后健康风险增加有关。