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Assessment of background levels and pollution sources for arsenic and fluoride in the phreatic and confined groundwater of Xi'an city, Shaanxi, China

机译:中国陕西西安市潜伏型和氟化砷和氟化物的背景水平和污染源评估

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The presence of arsenic and fluoride in groundwater and their impacts on human health have been reported in many countries worldwide, but little information is available on As or F- contamination in Xi'an city. This study highlights the distribution and sources of As and F- anomalies in different aquifers of Xi'an city, based on the assessment of natural background levels (NBLs) and threshold values (TVs). Groundwater samples collected from phreatic and confined aquifers were analyzed to evaluate NBLs and TVs, using median + 2MAD, Tukey inner fence (TIF), and percentile-based methods. Results showed that NBLs and TVs of As and F- in the phreatic aquifer were lower than those in the confined aquifer, indicating importance of the geological effects on the enrichment of arsenic and fluoride in the confined aquifer. Combined with hydrogeochemical methods, the distributions of As and F- anomalies show that high concentrations of As in both aquifers and F- in the confined aquifer can be attributed to the upward flow of geothermal water through faults and ground fissures, while high concentrations of F- in the phreatic aquifer may be greatly influenced by contaminated rivers. Although geological structures such as faults and ground fissures contribute to the high concentrations of potentially toxic elements, anthropogenic activities cannot be ignored because over exploitation of groundwater accelerates the development of ground fissures and results in the upward flow and mixing of geothermal water with groundwater in the upper aquifers.
机译:在全球许多国家报告了地下水中砷和氟化物的存在及其对人体健康的影响,但在西安市的污染或F-污染的信息很少。本研究突出了西安市不同含水层的分布和来源,基于自然背景水平(NBL)和阈值(TVS)的评估。分析了从潜水和局限性含水层收集的地下水样本来评估NBL和TVS,使用中位+ 2MAD,Tukey内围栏(TIF)和基于百分位的方法。结果表明,潜水患者的NBL和F-电视低于受限含水层中的NBL和电视,表明地质影响对狭窄含水层中砷和氟化物的富集的重要性。结合水力地球化学方法,AS和F-异常的分布表明,在密闭的含水层中,在含水层和F-中的高浓度可以归因于通过故障和地面裂隙的地热水向上流动,而高浓度的F - 在潜水层中可能受到污染河流的影响。虽然诸如故障和地裂隙的地质结构有助于潜在有毒元素的高浓度,但由于对地下水的开采加速了地面裂隙的发展,并且导致地热水与地下水的向上流动和混合导致地下水的发展,因此不忽视人类学活动。上含水层。

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