在玄武岩-水-CO2相互作用期间的元素流动性:在自然系统中的观察与实验室实验,以及对碳储存的影响
Pierangelo Romano1, Lorenzo Brusca2, Marcello Liotta2
1Istituto Nazionale di Geofisica e Vulcanologia Sezione di Palermo, Via Ugo la Malfa 143, Palermo, 90100, Italy. pierangelo.romano@ingv.it.
Geochemical transactions
|May 16, 2024
概括
富含二氧化碳的水域的玄武岩化有效地去除大气中的二氧化碳. 这个过程从岩石中释放元素,其移动性取决于水的pH值,影响潜在的碳捕集策略.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 矿物学是什么?矿物学是什么?
背景情况:
- 消除二氧化碳对于减缓气候变化至关重要.
- 在全球范围内丰富的玄武岩石含有与碳酸反应的金属.
- 了解玄武岩-水-二氧化碳相互作用是碳捕获的关键.
研究的目的:
- 为了汇总世界各地的玄武岩含水层的水化学数据.
- 在二氧化碳充电水实验中调查玄武岩气候变化和元素释放.
- 评估地质化学过程和二氧化碳储存在地形岩石中的环境影响.
主要方法:
- 汇编了全球基岩含水层水组成数据.
- 实验室实验涉及玄武岩粉和二氧化碳和水.
- 在水与岩石相互作用期间分析元素度和pH值变化.
主要成果:
- 在高二氧化碳条件下,玄武岩气候变化加速,形成金属碳酸盐.
- 元素的释放 (Ca,Mg,Fe) 是依赖于pH的,受CO2度的影响.
- 诸如Fe,Al和稀土元素等元素的移动性随着pH值而变化.
结论:
- 玄武岩气候变化是去除二氧化碳的可行途径.
- 玄武岩含水层中的地质化学过程对于二氧化碳的储存至关重要.
- 元素的移动性和潜在的毒性需要仔细考虑环境安全.
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