参数化,可转移的古典密度功能理论,用于烯/烯分离在阴离子热质石
Tiong Wei Teh1, André Kowoll1, Gernot Bauer1
1Institute of Thermodynamics and Thermal Process Engineering, University of Stuttgart, Pfaffenwaldring 9, D-70569 Stuttgart, Germany.
The journal of physical chemistry. B
|November 22, 2025
概括
我们开发了一种增强的经典密度函数理论 (DFT),以准确预测热石中的气体吸附. 这种方法为设计新材料的分子模拟提供了一个计算效率高的替代方案.
科学领域:
- 材料科学 材料科学 材料科学
- 物理化学 物理化学
- 计算化学计算化学
背景情况:
- 预测热石中的气体吸附对于分离和储存技术至关重要.
- 在多孔材料中精确建模气体-固体相互作用仍然是一个挑战.
研究的目的:
- 开发一种准确和高效的计算方法,用于预测阴离子交换热石中的气体吸附.
- 在经典的DFT中引入和验证可转移的二进制固体-流体相互作用参数 (k_si).
主要方法:
- 经典密度函数理论 (DFT) 增强了二进制固体-流体相互作用参数 (k_si).
- 使用大法典蒙特卡洛 (GCMC) 模拟,对特定的化/系统进行k_si的参数化.
- 对各种热带石结构,条件和混合物的GCMC模拟进行验证.
主要成果:
- 增强的DFT方法准确预测/混合物在交换热石 (FAU和LTA) 中的吸附等温度.
- 该k_si参数证明了在不同的热带石结构和条件中具有可转移性.
- 鉴于离子流动效应,鉴于交换的热石的局限性.
结论:
- 具有可转移k_si参数的经典DFT为实证模型和分子模拟提供了强大的,计算效率高的替代方案.
- 该方法使得高通量选和准确预测吸附在单价化化中.
- 这种方法有可能扩展到其他多孔材料和吸附剂系统.
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