分子密度波动控制受限水性的可溶性和扩散
Khang Quang Bui1, Tran Thi Bao Le1, Gabriel D Barbosa1
1School of Sustainable Chemical, Biological, and Materials Engineering, The University of Oklahoma, Norman, Oklahoma 73019, United States.
分子模拟显示,地下储存场所内封闭水中的溶性可能比散装水高25倍. 这种增强的溶解性和扩散性对于设计有效的地下储存 (UHS) 系统至关重要.
科学领域:
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
- 储能 储能 储能 储能 储能 储能
背景情况:
- 地下储存 (UHS) 对可持续能源转型至关重要,需要精确建模地下环境中的行为.
- 了解在地质构成中的热力学和运输特性对于设计高效和安全的UHS站点至关重要.
研究的目的:
- 用原子分子动力学 (MD) 模拟来量化卡奥利尼特裂孔内的水性 (H2) 的热力学和运输特性.
- 研究孔径几何和矿物表面相互作用对溶性和扩散的影响.
主要方法:
- 采用原子分子动力学 (MD) 模拟,在10和20 Å宽的形高利尼特孔内建模水性H2.
- 分析的重点是水化层的形成,H2的分布,可溶性和扩散系数.
主要成果:
- 由于水密度的波动,被封闭的水形成了独特的水合层,显著增加了在锡洛表面附近的H2溶解度 (多达约25倍).
- 吉布石表面的一层密集的水化层在很大程度上排除了H2.
- 尽管水的流动性降低,但随着孔径的宽度的减少,H2扩散增加,这与水密度的波动有关.
结论:
- 与散装条件相比,高矿孔中的封闭效应大大改变了的溶解性和运输特性.
- 这些发现为地下储设施的设计和优化提供了有关H2透性的关键见解.
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