State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550081, China.
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China.
Environ Geochem Health. 2024 Aug 22;46(10):390. doi: 10.1007/s10653-024-02168-z.
In Chinese freshwater lakes, eutrophication often coincides with heavy metal/metalloids (HM/Ms) pollution, yet the coevolution of critical nutrients (P, S, Se) and HM/Ms (Cd, Hg, etc.) remains understudied. To address this gap, we conducted a sedimentary chemistry analysis on a 30 cm-deep core, dating back approximately 200 years, retrieved from Chaohu Lake, China. The age-depth model revealed a gradual increase in deposition rates over time. Notably, the concentrations and enrichment factors (EFs) of most target elements surged in the uppermost ~ 15 cm layer, covering the period from 1953 to 2013, while both the concentrations and EFs in deeper layers remained relatively stable, except for Hg. This trend indicates a significant co-enrichment and near-synchronous increase in the levels and EFs of both nutrients and HM/Ms in the upper sediment layers since the mid-twentieth century. Anthropogenic factors were identified as the primary drivers of the enrichment of P, Se, Cd, Hg, Zn, and Te in the upper core, with their contributions also showing a coupled evolutionary trend over time. Conversely, geological activities governed the enrichment of elements in the lower half of the core. The gradual accumulation of anthropogenic Hg between the - 30 to - 15 cm layers might be attributed to global Hg deposition resulting from the industrial revolution. The ecological risk index (RI) associated with HM/Ms loading has escalated rapidly over the past 50 years, with Cd and Hg posing the greatest threats. Furthermore, the PMF model was applied to specifically quantify source contributions of these elements in the core, with anthropogenic and geogenic factors accounting for ~ 60 and ~ 40%, respectively. A good correlation (r = 0.87, p < 0.01) between the PMF and Ti-normalized method was observed, indicating their feasibility and cross-validation in source apportionment. Finally, we highlighted environment impact and health implications of the co-enrichment of nutrients and HM/Ms. This knowledge is crucial for developing strategies to protect freshwater ecosystems from the combined impacts of eutrophication and HM/Ms pollution, thereby promoting water environment and human health.
在中国的淡水湖中,富营养化往往与重金属/类金属(HM/Ms)污染同时发生,但关键营养物质(P、S、Se)与 HM/Ms(Cd、Hg 等)的共同演变仍未得到充分研究。为了解决这一差距,我们对取自中国巢湖的一个 30 厘米深的沉积物岩芯进行了沉积化学分析,该岩芯的时间跨度约为 200 年。年龄-深度模型显示,沉积速率随时间逐渐增加。值得注意的是,大多数目标元素的浓度和富集因子(EF)在最上层约 15 厘米的层中急剧上升,该层覆盖了 1953 年至 2013 年的时间段,而较深的层中的浓度和 EF 则相对稳定,除了 Hg。这一趋势表明,自 20 世纪中叶以来,营养物质和 HM/Ms 的水平和 EF 在表层沉积物中发生了显著的共富集和近乎同步的增加。人为因素被确定为上覆岩芯中 P、Se、Cd、Hg、Zn 和 Te 富集的主要驱动因素,它们的贡献也随时间呈现出耦合的演变趋势。相反,地质活动控制了岩芯下半部分元素的富集。-30 至-15 厘米层之间 Hg 的逐渐积累可能归因于工业革命导致的全球 Hg 沉积。过去 50 年,与 HM/Ms 负荷相关的生态风险指数(RI)迅速上升,其中 Cd 和 Hg 构成最大威胁。此外,我们还应用 PMF 模型来定量确定这些元素在岩芯中的源贡献,人为因素和地质因素分别占60%和40%。PMF 与 Ti 归一化方法之间存在良好的相关性(r=0.87,p<0.01),表明它们在源分配方面具有可行性和相互验证。最后,我们强调了营养物质和 HM/Ms 的共富集对环境的影响和对健康的影响。这些知识对于制定策略来保护淡水生态系统免受富营养化和 HM/Ms 污染的综合影响至关重要,从而促进水环境保护和人类健康。