Hangzhou Institute for Advanced Study, University of Chinese Academy of Sciences, Hangzhou 310024, China; State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
J Hazard Mater. 2023 Jun 15;452:131250. doi: 10.1016/j.jhazmat.2023.131250. Epub 2023 Mar 22.
Mercury (Hg) released by melting glaciers is likely to bind to suspended particles in meltwater runoff, posing potential risks to downstream ecosystems. The rapidly receding glaciers on the Tibetan Plateau promote the export of total suspended particles (TSP), increasing the uncertainty of Hg export released by glacier melting. To investigate the relationships between TSP and Hg, a multimedia sampling campaign was conducted in July 2020 in the Kuoqionggangri glacier region of the Lhasa River Valley No. 1 glacierized basin located in the inland Tibetan Plateau. Samples from glacier snow/ice, supraglacial rivers, subglacial rivers, proglacial lakes, and meltwater runoff were obtained, and the relationships between TSP and Hg and their transport in glacier meltwater runoff in the context of glacier retreat were explored. The average TSP concentration of different environmental samples ranged from 9.51 mg/L to 399. 27 mg/L, showing significant differences. The average total Hg (THg) concentrations ranged from 0.52 ng/L to 58.81 ng/L and decreased in the order of snow/ice >runoff> subglacial river > proglacial lake > supraglacial river. Both TSP mass concentration and number concentration have an impact on the diurnal variation in meltwater runoff Hg, and the influence of TSP number concentration is stronger than that of concentration. Sites with high TSP concentrations and quantities tended to have higher Hg concentrations, while TSP particle size had no significant effect on Hg concentration or spatial distribution. Our study further divided the glacier recharge basin into the glacier cover zone, the periglacial zone, and the downstream zone and discussed the potential impact of TSP on Hg transport in each zone. Our analysis highlights that the periglacial zone will expand and activate the resuspension process of river sediments in the warming future, which may increase the export of TSP and Hg downstream.
冰川融化释放的汞(Hg)很可能与融水中的悬浮颗粒结合,对下游生态系统构成潜在风险。青藏高原上快速退缩的冰川促进了总悬浮颗粒物(TSP)的输出,增加了冰川融化释放的 Hg 输出的不确定性。为了研究 TSP 与 Hg 之间的关系,我们于 2020 年 7 月在拉萨河流域 1 号冰川作用盆地的廓琼岗日冰川区开展了一项多介质采样活动。采集了冰川雪/冰、冰上河流、冰下河流、冰前湖泊和融水径流的样品,探讨了冰川退缩背景下冰川融水中 TSP 和 Hg 的关系及其输运。不同环境样品的 TSP 浓度平均值范围为 9.51mg/L 至 399.27mg/L,差异显著。总汞(THg)浓度平均值范围为 0.52ng/L 至 58.81ng/L,依次为雪/冰>径流>冰下河流>冰前湖泊>冰上河流。TSP 质量浓度和数量浓度均对融水径流 Hg 的日变化有影响,且 TSP 数量浓度的影响强于浓度。TSP 浓度和数量较高的站点往往具有较高的 Hg 浓度,而 TSP 粒径对 Hg 浓度或空间分布没有显著影响。我们的研究进一步将冰川补给流域划分为冰川覆盖区、冰缘区和下游区,并讨论了 TSP 对每个区 Hg 输运的潜在影响。我们的分析强调,在未来变暖的情况下,冰缘区将扩大并激活河流沉积物的再悬浮过程,这可能会增加下游 TSP 和 Hg 的输出。