在埃特纳火山 (西西里) 火山含水层中探索稀土元素的行为
Salvatore Dominech1, Cinzia Federico2, Lorenzo Brusca1
1Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, Via La Malfa 153, 90146, Palermo, Italy.
Environmental geochemistry and health
|June 7, 2024
概括
这项研究揭示了埃特纳山的稀土元素 (REY) 模式.
科学领域:
- 地质化学 地质化学
- 水文地质学 水文地质学
- 环境科学 环境科学
背景情况:
- 埃特纳山的含水层系统受到火山过程的影响.
- 了解稀土元素 (REY) 的行为对于评估水岩相互作用至关重要.
研究的目的:
- 介绍关于埃特纳山含水层REY分布的第一个数据.
- 为了研究控制 REY 行为的水地化学过程.
主要方法:
- 分析地下水中的REY度.
- 对 REY 模式的规范化,以使其适用于地铁.
- 与水地化学代理的相关性分析.
主要成果:
- 强烈的水岩相互作用,由REY模式表示.
- 火山CO2溶解中的酸性pH值促进了REY的移动性.
- 有矿物质溶解 (铁矿物质) 和二次阶段形成 (铁/氧化物) 的证据.
- 阴性Ce和阳性Y异常表明有氧化条件.
- 由二碳酸盐复合影响的Y/Ho分化.
结论:
- REY模式为火山含水层中的地化学过程提供了宝贵的见解.
- 地下水REY度低于饮用水的安全限值.
- 这项研究强调了岩石气体,水岩相互作用和氧化还原条件的相互作用.
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