Zhang Yingchun, Liu Xiandong, van Duin Adri C T, Lu Xiancai, Meijer Evert Jan
State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 210023, People's Republic of China.
Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing, Jiangsu 210023, People's Republic of China.
J Chem Phys. 2024 Mar 7;160(9). doi: 10.1063/5.0194486.
ReaxFF reactive force field bridges the gap between nonreactive molecular simulations and quantum mechanical calculations and has been widely applied during the past two decades. However, its application to earth materials, especially those under high T-P conditions relevant to Earth's interior, is still limited due to the lack of available parameters. Here, we present the development and validation of a ReaxFF force field containing several of the most common elements in Earth's crust, i.e., Si/Al/O/H/Na/K. The force field was trained against a large data set obtained from density functional theory (DFT) calculations, including charges, bond/angle distortion curves, equation of states, ion migration energy profiles, and condensation reaction energies. Different coordination environments were considered in the training set. The fitting results showed that the current force field can well reproduce the DFT data (the Pearson correlation coefficient, Rp, is 0.95). We validated the force field on mineral-water interfaces, hydrous melts/supercritical geofluids, and bulk crystals. It was found that the current force field performed excellently in predicting the structural, thermodynamic, and transport properties of various systems (Rp = 0.95). Moreover, possible applications and future development have been discussed. The results obtained in this study suggest that the current force field holds good promise to model a wide range of processes and thus open opportunities to advance the application of ReaxFF in earth material modeling.
ReaxFF反应力场填补了非反应性分子模拟与量子力学计算之间的空白,并在过去二十年中得到了广泛应用。然而,由于缺乏可用参数,其在地球材料中的应用,尤其是在与地球内部相关的高温高压条件下的应用仍然有限。在此,我们展示了一种包含地壳中几种最常见元素(即硅/铝/氧/氢/钠/钾)的ReaxFF力场的开发与验证。该力场是根据从密度泛函理论(DFT)计算中获得的大量数据集进行训练的,这些数据集包括电荷、键/角畸变曲线、状态方程、离子迁移能分布以及缩合反应能量。训练集中考虑了不同的配位环境。拟合结果表明,当前力场能够很好地再现DFT数据(皮尔逊相关系数Rp为0.95)。我们在矿物 - 水界面、含水熔体/超临界地质流体以及块状晶体上对该力场进行了验证。结果发现,当前力场在预测各种系统的结构、热力学和输运性质方面表现出色(Rp = 0.95)。此外,还讨论了可能的应用和未来发展。本研究获得的结果表明,当前力场在模拟广泛的过程方面具有良好前景,从而为推进ReaxFF在地球材料建模中的应用提供了机会。