稀土和重金属元素在一个代表性的岩沉积系统中的变化
Mengyuan Xu1, Cheng Wang2, Yang Pu1
1School of Geographic Sciences, Nanjing University of Information Science and Technology, Nanjing, 210044, China.
Environmental science and pollution research international
|December 11, 2023
概括
长江洪水平原沉积物中的重金属和稀土元素显示出明显的垂直分布. 自然沉会稀释一些污染物,而燃烧煤炭会显著影响含量.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 沉积物学的沉积物学
背景情况:
- 洪水平原沉积物充当环境变化的档案.
- 了解重金属和稀土元素的分布对于评估污染至关重要.
- 长江下游是一个充满活力的系统,受到自然过程和人类活动的影响.
研究的目的:
- 研究洪水平原沉积物中重金属 (Ni,Cr,W,Cd,Pb) 和稀土元素 (REE) 的垂直分布.
- 要区分自然沉积过程和人为污染.
- 确定这些元素的来源和运输机制.
主要方法:
- 战略图分析包括磁性易感性和颗粒大小分布.
- 对重金属和稀土元素度的分析.
- 澳大利亚石页岩 (PAAS) 对于REE模式的正常化.
- 元素度,磁性易感性和历史数据之间的相关性分析.
主要成果:
- 沉积物流入较高的层显示了Cr,Ni,W和Cd的低度,这表明石质起源.
- REE模式表明沉积物来源主要是混合物,而不是人为.
- 最上层的沉积物层呈现出Y/Ho比率和重金属度的急剧增加,这与污染的水运输有关.
- 高度与高磁性易感性和热电站活动相关,表明燃煤作为来源.
结论:
- 垂直沉积物形状反映了自然沉积和人为投入的组合.
- 虽然自然过程可以稀释一些污染物,但等特定污染物显示出明显的人为特征.
- 燃烧煤炭是研究区域洪水平原沉积物中污染的重要来源.
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