在韩国的瓶装水中稳定的H-O和放射性Sr同位素比率
Hyo Min Lee1, Hui Je Jo1, Hanna Choi2
1Geology & Space Division, Korea Institute of Geoscience and Mineral Resources, Daejeon, Republic of Korea.
Isotopes in environmental and health studies
|January 20, 2025
概括
韩国瓶装水中稳定的氧和同位素显示出不同的起源和水岩相互作用. 这项研究追踪水源并使用同位素签名验证瓶装水的来源.
科学领域:
- 地质化学 地质化学
- 同位素水文学 同位素水文学
背景情况:
- 瓶装水的质量依赖于来源认证.
- 了解水岩相互作用对于水地质学至关重要.
研究的目的:
- 为了追溯南韩瓶装水的起源.
- 用同位素分析阐明水地化学水岩相互作用.
主要方法:
- 对稳定的氧同位素 (δD和δ18O) 的分析.
- 测量放射性同位素 (87Sr/86Sr比率) 和含量.
- 来自韩国的81个瓶装水样本的采集和同位素分析.
主要成果:
- 与淡化深海水相比,地下水来源的瓶装水显示出明显的同位素范围.
- 稳定同位素 (δ18O) 与度负相关,表明地理变化.
- 同位素比率 (87Sr/86Sr) 与含水层地质相关,反映了水岩相互作用.
结论:
- 同位素组成有效地区分瓶装水源.
- 结合稳定和放射性同位素分析可以提高对水岩相互作用的理解.
- 这种方法可以准确地验证瓶装水的来源.
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