低温碳化和CO2矿物捕获在改变的富含酸盐的超级岩石中
Mahmoud Leila1, Randy Hazlett2, Paul-Mathews George2
1School of Mining and Geosciences, Nazarbayev University, Astana, 010000, Kazakhstan. Mahmoud.Leila@nu.edu.kz.
Scientific reports
|August 24, 2025
概括
超岩在低温下通过矿化有效地封存二氧化碳 (CO2). 层状双氧化物 (LDH) 是地质碳捕获 (GCS) 中二氧化碳矿物捕获的关键反应阶段.
科学领域:
- 地质化学
- 环境科学
- 矿物学
背景情况:
- 全球变暖需要减少二氧化碳 (CO2) 排放并加强碳封存.
- 地质碳捕获 (GCS) 使用宿主岩石的二氧化碳矿化.
- 超岩提供了二氧化碳封存的潜力,但它们的反应性比岩更少研究.
研究的目的:
- 在低温GCS条件下研究蛇形化哈兹堡石的碳化.
- 评估特定矿物阶段,包括层状双化物 (LDH) 在二氧化碳封存中的作用.
- 评估超级岩石对工程二氧化碳矿物捕获的效率.
主要方法:
- 实验研究水性二氧化碳与粉碎的蛇形化哈兹堡石的相互作用.
- 在14天内控制低温 (40°C) 和低压 (60bar).
- 分析固态转换,点火损失和SiO2含量.
主要成果:
- 显著的内斯基霍尼特形成 (约. 70%) 和LDH的完全碳化.
- 蛇形素和橄素含量大幅降低 (75%).
- 增加的LOI和减少的SiO2表明有效的CO2被纳入新的碳酸盐矿物质中.
结论:
- 超岩在低温和低压下有效地进行二氧化碳矿化.
- 在提高二氧化碳矿物捕获能力方面,LDH阶段起着至关重要的作用.
- 这些发现支持了在地表超级岩层中人工捕获二氧化碳的可能性.
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