吸附动力学和粘土扩散:对的地质储存和天然勘探的影响
Qian Zhang1, Jiguang Wang1, Lunxiang Zhang2
1Key Laboratory of Ocean Energy Utilization and Energy Conservation of the Ministry of Education, Dalian University of Technology, Dalian 116024, China.
粘土矿物质对于地下 (H2) 储存至关重要. 石的H2吸附和扩散率高于蒙莫里隆石,表明其在地质H2应用中的潜力.
科学领域:
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
- 能源科学 能源科学
背景情况:
- (H2) 储存对于能源转型和缓解气候变化至关重要.
- 了解H2的地下行为对于地下储存和勘探等应用至关重要.
- 储水池和岩中的粘土矿物质显著影响H2吸附和扩散.
研究的目的:
- 为了研究粘土矿物质 (蒙莫里隆石和石) 中的吸附和扩散.
- 在不同温度和压力下建模H2吸附平衡和动力学.
- 评估不同吸附和动力学模型对H2粘土相互作用的适用性.
主要方法:
- 在蒙特莫里隆石和石上进行了H2异热吸附和动力实验.
- 测试条件: 30°C,40°C,50°C和0-9.8 MPa压力范围.
- 应用了Langmuir,Freundlich,BET,DA,伪第一阶,伪第二阶,Bangham,以及拉伸指数模型.
主要成果:
- 布鲁纳uer-Emmett-Teller (BET) 模型最适合于H2吸附等热体.
- 班哈姆运动模型准确地预测了压力阶段的实验动力学.
- 在 sepiolite 中,H2 的吸附能力和扩散率比在 montmorillonite 中更高.
- 温度和压力的增加降低了班哈姆吸附率常数.
- 粘土矿物中的H2扩散系数随着压力增加而下降.
结论:
- 与蒙特莫里隆石相比,石具有更高的H2吸附能力和扩散特性.
- BET和Bangham模型有效地描述了粘土矿物中的H2吸附和动力学.
- 这些发现凸显了 sepiolite 在地质构成中增强 H2 运输和运输的潜力.
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