Institute of Hydrogeology, RWTH Aachen University, Lochnerstraße 4-20, 52064 Aachen, Germany.
Institute of Hydrogeology, RWTH Aachen University, Lochnerstraße 4-20, 52064 Aachen, Germany.
J Contam Hydrol. 2020 Nov;235:103710. doi: 10.1016/j.jconhyd.2020.103710. Epub 2020 Sep 1.
The rare earth element (REE) group is widely used for geochemical prospection and the hydrochemical differentiation of waters. Most of the currently applied methods use normalized REE patterns to determine enrichments or depletions of certain REE in comparison to standard materials, which are caused by specific environmental conditions. Contrast agents containing Gadolinium (Gd), which are used for magnetic resonance imaging (MRI), have been emitted into surface waters since the 1980s. Patients excrete these contrast agents shortly after ambulant medication in hospitals or at home. Sewage treatment is currently unable to hold back Gd from this anthropogenic source. Therefore, the Gd concentration in the receiving channel increases significantly and creates a Gd peak in the REE pattern. This anthropogenic peak propagates into adjacent groundwater bodies. In a karst aquifer showing a connection between a river/ponor (input) and three springs (output), such an anthropogenic Gd anomaly has been traced, the local Gd background quantified, and surface water groundwater interaction evaluated. In two sampling campaigns, water samples were taken every day at the input and output side during one week in February and three weeks in May. Sampling of springs and brooks in the vicinity of the karst aquifer proved excessive Gd from anthropogenic sources. The evaluation of concentration, mass flow and total mass of Gd show that Gd can be an environmental tracer to monitor surface water-groundwater interaction as well as the anthropogenic influence on water bodies. Further anthropogenic pollutants - diclofenac, carbamazepine, galaxolide, caffeine, and acesulfame-K - representing different classes of common organic substances were tested as co-indicators to Gd. However, out of these only acesulfame-K was detected and is related with the Gd-anomaly. Our results indicate that Gd is a more powerful indicator of surface water- groundwater interaction than most organic pollutants.
稀土元素(REE)广泛应用于地球化学勘探和水的地球化学分异。目前应用的大多数方法都使用标准化 REE 模式来确定特定环境条件下某些 REE 的富集或贫化。自 20 世纪 80 年代以来,用于磁共振成像(MRI)的含钆(Gd)造影剂已被排放到地表水中。患者在医院或家中进行门诊治疗后不久就会排泄这些造影剂。目前,污水处理厂无法阻止这种人为来源的 Gd 排放。因此,接收渠道中的 Gd 浓度显著增加,并在 REE 模式中形成 Gd 峰。这种人为峰传播到相邻的地下水体中。在一个显示河流/泉眼(输入)与三个泉眼(输出)之间存在联系的喀斯特含水层中,已经追踪到了这种人为的 Gd 异常,量化了当地的 Gd 背景,并评估了地表水与地下水的相互作用。在两次采样活动中,在 2 月和 5 月的一周和三周内,每天在输入和输出端采集水样。对喀斯特含水层附近的泉眼和溪流进行采样,证明了人为来源的 Gd 含量过高。对 Gd 的浓度、质量流和总质量的评估表明,Gd 可以作为一种环境示踪剂,用于监测地表水-地下水相互作用以及水体受到的人为影响。进一步的人为污染物——双氯芬酸、卡马西平、加乐麝香、咖啡因和乙酰磺胺酸钾——代表不同类别的常见有机物质,被用作 Gd 的共同指示物进行测试。然而,在这些物质中,只有乙酰磺胺酸钾被检测到,并且与 Gd 异常有关。我们的结果表明,Gd 是地表水-地下水相互作用的比大多数有机污染物更强大的指示物。