在模拟的蒙莫里隆石-流体系统中丰富和金属生成的机制
Song Yan1, Tao Sun1, Yuanfeng Cai1
1State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China.
Langmuir : the ACS journal of surfaces and colloids
|August 21, 2023
概括
蒙莫里隆石 (Mt) 矿床中的缩在富含和富含的系统之间存在差异,影响了勘探. 在Mt内部易于交换的是沉积等级的关键.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 材料科学 材料科学 材料科学
背景情况:
- 对的工业需求推动了对含蒙莫里隆石 (Li-Mt) 矿床的勘探.
- 了解Li-Mt中的缩机制对于高效的勘探至关重要.
研究的目的:
- 研究富含F和富含Cl系统中的丰富机制.
- 为了阐明影响吸附在蒙莫里隆石 (Mt) 中的水岩反应.
主要方法:
- 在不同度,温度,持续时间和pH下进行吸附实验.
- 矿物学分析包括核磁共振 (NMR) 和CaCl2出.
主要成果:
- 水岩反应不同:在LiCl-Mt系统中脱化和在LiF-Mt系统中脱化.
- LiF-Mt 的吸附能力是 LiCl-Mt 的 2.8 倍.
- 在Mt腔内形成内部球体复合物;>50%的是可交换的.
结论:
- 可交换含量决定了离子吸附型沉积物的等级.
- 丰富机制依赖于素,影响金属生成.
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