对微量元素释放的实验室研究以及来自页岩与裂变流体相互作用的环境风险
Alison R Keimowitz1, George L Diehl2, Ryan N Farley3
1Chemistry Department, Vassar College, 124 Raymond Avenue, Poughkeepsie, NY 12601, United States.
Journal of hazardous materials
|September 17, 2025
概括
液压压裂液改变了页岩的地化学,调动了危险的微量元素. 这些元素可以进入水源,随着开采现场的老化,构成环境风险.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 地球科学 地球科学 地球科学
背景情况:
- 水力压裂 (fracking) 是一个关键的天然气提取方法.
- 黑色页岩,像马塞卢斯,是开采的目标.
- 压裂液与页岩相互作用,改变矿物学和调动微量元素.
研究的目的:
- 调查压裂过程中微量元素的释放和再分配.
- 分析压裂液和页岩之间的地化学反应.
- 评估动员元素的长期环境流动性.
主要方法:
- 实验室实验模拟压裂阶段 (关闭,回流,生产,关闭).
- 在页岩中分析地质化学反应和矿物学变化.
- 监测微量元素的调动和再分配.
主要成果:
- 关闭过程中的酸添加溶解碳酸盐和硫化物,导致硫化物氧化和矿物转化.
- 微量元素在初始生产过程中通过酸性溶解释放出来.
- 一些元素 (兰化物, Zn, Sr) 从固态阶段消失.
- 诸如As,Mo和U这样的元素被转化为更具流动性的矿物质形式.
结论:
- 压裂过程显著改变了页岩地质化学.
- 移动的微量元素,特别是As,Mo和U,对长期的环境流动性构成风险.
- 随着井网的老化,饮用水污染的可能性会增加.
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