Department of Chemical and Biomolecular Engineering, University of California, Los Angeles, Los Angeles, California 90095, United States.
Princeton Plasma Physics Laboratory, Princeton, New Jersey 08540-6655, United States.
J Am Chem Soc. 2023 Jun 14;145(23):12561-12575. doi: 10.1021/jacs.3c01283. Epub 2023 Jun 5.
Simulations of carbon dioxide (CO) in water may aid in understanding the impact of its accumulation in aquatic environments and help advance technologies for carbon capture and utilization (via, e.g., mineralization). Quantum mechanical (QM) simulations based on static molecular models with polarizable continuum solvation poorly reproduce the energetics of CO hydration to form carbonic acid in water, independent of the level of QM theory employed. Only with density-functional-theory-based molecular dynamics and rare-event sampling, followed by energy corrections based on embedded correlated wavefunction theory (in conjunction with density functional embedding theory), can a close agreement between theory and experiment be achieved. Such multilevel simulations can serve as benchmarks for simpler, less costly models, giving insight into potential errors of the latter. The strong influence of sampling/averaging over dynamical solvent configurations on the energetics stems from the difference in polarity of both the transition state and product (both polar) versus the reactant (nonpolar). When a solute undergoes a change in polarity during reaction, affecting its interaction with the solvent, careful assessment of the energetic contribution of the solvent response to this change is critical. We show that static models (without structural sampling) that incorporate three explicit water molecules can yield far superior results than models with more explicit water molecules because fewer water molecules yield less configurational artifacts. Static models intelligently incorporating both explicit (molecules directly participating in the reaction) and implicit solvation, along with a proper QM theory, e.g., CCSD(T) for closed-shell systems, can close the accuracy gap between static and dynamic models.
二氧化碳(CO)在水中的模拟可能有助于了解其在水生环境中积累的影响,并有助于推进碳捕集和利用技术(例如,通过矿化作用)。基于具有可极化连续体溶剂化的静态分子模型的量子力学(QM)模拟,无论所采用的 QM 理论水平如何,都无法很好地再现 CO 水合形成碳酸的能量学。只有通过基于密度泛函理论的分子动力学和稀有事件采样,以及基于嵌入相关波函数理论(与密度泛函嵌入理论相结合)的能量校正,才能在理论和实验之间实现紧密一致。这种多层次模拟可以作为更简单、成本更低的模型的基准,深入了解后者的潜在误差。采样/平均对动态溶剂构型对能量的强烈影响源于过渡态和产物(均为极性)与反应物(非极性)的极性差异。当溶质在反应过程中经历极性变化,从而影响其与溶剂的相互作用时,必须仔细评估溶剂对这种变化的响应的能量贡献。我们表明,静态模型(不进行结构采样),其中包含三个显式水分子,可以产生远优于具有更多显式水分子的模型的结果,因为更少的水分子会产生更少的构型伪影。静态模型可以巧妙地结合显式(直接参与反应的分子)和隐式溶剂化,以及适当的 QM 理论,例如,对于闭壳系统的 CCSD(T),可以缩小静态和动态模型之间的准确性差距。