Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing 100101, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China.
Sci Total Environ. 2018 Aug 1;631-632:270-278. doi: 10.1016/j.scitotenv.2018.03.012. Epub 2018 Mar 16.
Glacierized mountain environments can preserve and release mercury (Hg) and play an important role in regional Hg biogeochemical cycling. However, the behavior of Hg in glacierized mountain environments and its environmental risks remain poorly constrained. In this research, glacier meltwater, runoff and wetland water were sampled in Zhadang-Qugaqie basin (ZQB), a typical glacierized mountain environment in the inland Tibetan Plateau, to investigate Hg distribution and its relevance to environmental risks. The total mercury (THg) concentrations ranged from 0.82 to 6.98ng·L, and non-parametric pairwise multiple comparisons of the THg concentrations among the three different water samples showed that the THg concentrations were comparable. The total methylmercury (TMeHg) concentrations ranged from 0.041 to 0.115ng·L, and non-parametric pairwise multiple comparisons of the TMeHg concentrations showed a significant difference. Both the THg and MeHg concentrations of water samples from the ZQB were comparable to those of other remote areas, indicating that Hg concentrations in the ZQB watershed are equivalent to the global background level. Particulate Hg was the predominant form of Hg in all runoff samples, and was significantly correlated with the total suspended particle (TSP) and not correlated with the dissolved organic carbon (DOC) concentration. The distribution of mercury in the wetland water differed from that of the other water samples. THg exhibited a significant correlation with DOC as well as TMeHg, whereas neither THg nor TMeHg was associated with TSP. Based on the above findings and the results from previous work, we propose a conceptual model illustrating the four Hg distribution zones in glacierized environments. We highlight that wetlands may enhance the potential hazards of Hg released from melting glaciers, making them a vital zone for investigating the environmental effects of Hg in glacierized environments and beyond.
冰川化的山地环境可以保存和释放汞(Hg),并在区域汞生物地球化学循环中发挥重要作用。然而,汞在冰川化山地环境中的行为及其环境风险仍然难以确定。在这项研究中,我们在扎当-曲嘎盆地(ZQB)采集了冰川融水、径流和湿地水,以研究 Hg 的分布及其与环境风险的关系。ZQB 是青藏高原内陆地区的一个典型冰川化山地环境。总汞(THg)浓度范围为 0.82 至 6.98ng·L,三种不同水样之间的非参数两两多重比较表明,THg 浓度相当。总甲基汞(TMeHg)浓度范围为 0.041 至 0.115ng·L,TMeHg 浓度的非参数两两多重比较表明存在显著差异。ZQB 流域水样的 THg 和 MeHg 浓度与其他偏远地区的水样相当,表明 ZQB 流域的 Hg 浓度与全球背景水平相当。所有径流样品中均以颗粒态汞(Hgp)为主,与总悬浮颗粒物(TSP)显著相关,而与溶解有机碳(DOC)浓度无关。湿地水的汞分布与其他水样不同。THg 与 DOC 以及 TMeHg 呈显著相关,而 THg 和 TMeHg 均与 TSP 无关。基于以上发现和以往工作的结果,我们提出了一个概念模型,说明了冰川化环境中 Hg 的四个分布区。我们强调,湿地可能会增加融化冰川释放的 Hg 的潜在危害,使其成为研究冰川化环境及其他环境中 Hg 环境效应的重要区域。