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向最大的北极高湖输入有机磷酸酯类阻燃剂的冰川融化物。

Glacial Melt Inputs of Organophosphate Ester Flame Retardants to the Largest High Arctic Lake.

机构信息

CAS Key Laboratory of Tropical Marine Bio-resources and Ecology; Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, P. R. China.

Aquatic Contaminants Research Division, Environment and Climate Change Canada, Burlington, Ontario L7S 1A1, Canada.

出版信息

Environ Sci Technol. 2020 Mar 3;54(5):2734-2743. doi: 10.1021/acs.est.9b06333. Epub 2020 Feb 20.

Abstract

Organophosphate esters (OPEs) have been detected in the Arctic environment, but the influence of glacial melt on the environmental behavior of OPEs in recipient Arctic aquatic ecosystems is still unknown. In this study, water samples were collected from Lake Hazen (LH) and its tributaries to investigate the distribution of 14 OPEs in LH and to explore the input of OPEs from glacial rivers to LH and the output of OPEs from LH in 2015 and 2018. ΣOPE concentrations in water of LH were lower than glacial rivers and its outflow, the Ruggles River. In 2015, a high melt year, we estimated that glacial rivers contributed 7.0 ± 3.2 kg OPEs to LH, compared to a 16.5 ± 0.3 kg OPEs output by the Ruggles River, suggesting that residence time and/or additional inputs via direct wet and dry deposition and permafrost melt likely result in OPE retention in the LH watershed. In 2018, a lower melt year, ΣOPE concentrations in glacial rivers were much lower, indicating that the rate of glacier melt may govern, in part, the concentrations of OPEs in the tributaries of LH. This study highlights long-range transport of OPEs, their deposition in Arctic glaciers, landscapes, and lakes.

摘要

有机磷酸酯 (OPEs) 已在北极环境中被检测到,但冰川融化对接收北极水生生态系统中 OPEs 环境行为的影响仍不清楚。本研究采集了哈森湖 (LH) 及其支流的水样,以调查 LH 中 14 种 OPEs 的分布,并探讨 OPEs 从冰川河流输入 LH 以及 OPEs 从 LH 输出的情况。2015 年和 2018 年,LH 水中ΣOPE 浓度低于冰川河流及其流出的拉格尔斯河。在高融雪年份 2015 年,我们估计冰川河流向 LH 输送了 7.0 ± 3.2 千克 OPEs,而拉格尔斯河的输送量为 16.5 ± 0.3 千克 OPEs,这表明停留时间和/或通过直接干湿沉积和永冻层融化的额外输入可能导致 OPEs 在 LH 流域中被截留。在低融雪年份 2018 年,冰川河流中的ΣOPE 浓度要低得多,这表明冰川融化的速度可能部分决定了 LH 支流中 OPEs 的浓度。本研究强调了 OPEs 的长距离传输、它们在北极冰川、景观和湖泊中的沉积。

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