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The influence of hydrogeological and anthropogenic variables on phthalate contamination in eogenetic karst groundwater systems

机译:水文地质和人为因素对新生岩溶地下水系统邻苯二甲酸盐污染的影响

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摘要

This study investigates the occurrence of six phthalates and distribution of the three most-detected phthalates in the karst region of northern Puerto Rico (KRNPR) using data from historical records and current field measurements. Statistical data analyses, including ANOVA, Chi-Square, and logistic regression models are used to examine the major factors affecting the presence and concentrations of phthalates in the KRNPR. The most detected phthalates include DEHP, DBP, and DEP. At least one phthalate specie is detected above DL in 7% of the samples and 24% of the sampling sites. Concentrations of total phthalates average 5.08 ± 1.37 µg L−1, and range from 0.093 to 58.4 µg L−1. The analysis shows extensive spatial and temporal presence of phthalates resulting from dispersed phthalate sources throughout the karst aquifers. Hydrogeological factors are significantly more important in predicting the presence and concentrations of phthalates in eogenetic karst aquifers than anthropogenic factors. Among the hydrogeological factors, time of detection and hydraulic conductivities larger than 300 m d−1 are the most influential factors. Persistent presence through time reflects continuous sources of phthalates entering the aquifers and a high capacity of the karst aquifers to store and slowly release contaminants for long periods of time. The influence of hydraulic conductivity reveals the importance of contaminant fate and transport mechanisms from contamination sources. This study improves the understanding of factors affecting the spatial variability and fate of phthalates in karst aquifers, and allows us to better predict their occurrence based on these factors.
机译:这项研究使用历史记录和当前田间测量的数据,调查了波多黎各北部喀斯特地区(KRNPR)中六种邻苯二甲酸盐的发生以及三种检测最多的邻苯二甲酸盐的分布。统计数据分析(包括方差分析,卡方和对数回归模型)用于检查影响KRNPR中邻苯二甲酸酯存在和浓度的主要因素。检出最多的邻苯二甲酸盐包括DEHP,DBP和DEP。在7%的样品和24%的采样点中,在DL以上检测到至少一种邻苯二甲酸盐。总邻苯二甲酸酯的平均浓度为5.08±1.37 µg L -1 ,范围为0.093至58.4 µg L -1 。分析表明,由于整个岩溶含水层中分散的邻苯二甲酸盐来源而产生的邻苯二甲酸盐的时空分布广泛。与人为因素相比,水文地质因素在预测新生岩溶含水层中邻苯二甲酸盐的存在和浓度方面更为重要。在水文地质因素中,影响探测时间和水力传导率大于300 m d -1 的因素最为明显。持续存在的时间反映了邻苯二甲酸盐源源不断地进入含水层,并且岩溶含水层具有很高的容量,可以长时间存储和缓慢释放污染物。水力传导率的影响揭示了污染物命运和来自污染源的运输机制的重要性。这项研究增进了对影响岩溶含水层中邻苯二甲酸盐空间变异性和命运的因素的理解,并使我们能够基于这些因素更好地预测它们的发生。

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