确定水性在生态系统中的同位素组成,使用薄膜中的扩散梯度
Hongqian Yin1,2, Heng Yao1, Wei Yuan1
1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.
Analytical chemistry
|August 22, 2023
概括
使用功能化纳米颗粒的新DGT (薄膜扩散梯度) 方法有效测量水中的同位素. 这种被动采样技术有助于了解.
科学领域:
- 环境化学环境化学
- 分析化学 分析化学
- 地质化学 地质化学
背景情况:
- 测量超微量水性 (Hg) 同位素是困难的,因为度低 (ng L-1),需要大量的水量 (>10 L),并带来污染的风险与传统的采集采样.
- 精确的Hg同位素分析需要至少5 ng的Hg质量,这对于自然水样来说是一个重大挑战.
- 传统方法是劳动密集型,耗时,在样品处理和预缩过程中容易受到污染.
研究的目的:
- 开发和验证一种新的薄膜扩散梯度 (DGT) 方法,用于确定水性的度和同位素组成.
- 评估DGT方法在Hg吸附过程中诱导的质量依赖分化 (MDF) 和质量独立分化 (MIF).
- 评估DGT方法在污染水环境中的Hg生物地球化学循环的表征方面的有效性.
主要方法:
- 使用aminopropyl和mercaptopropyl双功能SBA-15纳米颗粒用于Hg吸附的DGT设备的开发.
- 通过DGT对Hg吸附的实验室分析,量化诱导的MDF和MIF.
- 现场部署DGT方法与传统的采集采样一起用于对Hg同位素特征进行比较分析.
主要成果:
- 实验室测试表明,Hg的DGT吸附会诱导大约-0.2‰的MDF和最小的MIF,MDF受扩散层厚度的影响.
- 现场结果表明,DGT方法和采样采样之间的一致的MIF签名 (Δ199Hg).
- DGT方法在描述水性Hg MIF方面被证明是有效的,这对于理解Hg生物地球化学循环至关重要.
结论:
- 开发的DGT方法提供了一种被动且有效的方法来分析水中的度和同位素组成.
- 由于潜在的环境过程影响,建议在解释DGT的Hg-MDF数据时谨慎使用.
- DGT方法成功地描述了Hg MIF,提供了有关Hg在受污染地点的生态化学循环的宝贵见解.
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