Gorantla Koteswara Rao, Mallik Bhabani S
Department of Chemistry, Indian Institute of Technology Hyderabad, Sangareddy 502285 Telangana, India.
J Phys Chem A. 2021 Jan 14;125(1):279-290. doi: 10.1021/acs.jpca.0c09943. Epub 2020 Dec 28.
This work elucidates the reactivity of water molecules toward the tridentate nitrogen-containing iron complex in the water oxidation process. Here, we consider the Fe-bisoxo complex {[Fe(Metacn)(OH)(═O)]} to be responsible for the oxygen-oxygen bond formation. This O-O bond formation happens through the addition of water as a nucleophile. The transition state was determined by the synchronous transit-guided quasi-Newton method using reactants and products and verified by intrinsic reaction coordinates (IRCs). From the IRC calculations, we observe that the Fe═O moiety is attacked by water and assisted by the H-bonded interaction with the oxygen atom of the bisoxo complex. The hydrogen atom is transferred to the oxygen atom of the bisoxo complex through the transition state, and subsequently, the hydroxide is transferred to another oxygen of the bisoxo complex, resulting in the formation of the oxygen-oxygen bond. This work also explains the effect of explicit water molecules on the oxygen-oxygen bond formation. Our results also show how the formation of superoxide plays an essential role in O evolution. We used the potential energy scan method to compute the transition state in the oxygen evolution step. In the present work, we study the effect of chlorine on the formation of the oxygen-oxygen bond formation. In this study, the changes in the oxidation state, spin density, and spin multiplicity of the complexes are investigated for each successive step. Apart from these static theoretical calculations, we also studied the oxygen-oxygen bond formation through first-principles molecular dynamics with the aid of the well-tempered metadynamics sampling technique. From the observation of the free energy surfaces from metadynamics simulations, it is evident that the hydroxide transfer has a lesser free energetic reaction as compared to the proton transfer. This complete mechanistic study may give an idea to design a suitable water oxidation catalyst.
这项工作阐明了水分子在水氧化过程中对含三齿氮的铁配合物的反应活性。在此,我们认为铁-双氧基配合物{[Fe(Metacn)(OH)(═O)]}负责氧-氧键的形成。这种O-O键的形成是通过亲核试剂水的加成发生的。过渡态通过使用反应物和产物的同步过渡引导准牛顿法确定,并通过内禀反应坐标(IRC)进行验证。从IRC计算中,我们观察到Fe═O部分受到水的攻击,并通过与双氧基配合物的氧原子的氢键相互作用得到辅助。氢原子通过过渡态转移到双氧基配合物的氧原子上,随后,氢氧根转移到双氧基配合物的另一个氧原子上,导致氧-氧键的形成。这项工作还解释了明确的水分子对氧-氧键形成的影响。我们的结果还表明超氧化物的形成如何在氧气析出中起重要作用。我们使用势能扫描方法来计算析氧步骤中的过渡态。在本工作中,我们研究了氯对氧-氧键形成的影响。在这项研究中,研究了配合物在每个连续步骤中的氧化态、自旋密度和自旋多重性的变化。除了这些静态理论计算外,我们还借助良好温度的元动力学采样技术通过第一性原理分子动力学研究了氧-氧键的形成。从元动力学模拟的自由能表面观察中可以明显看出,与质子转移相比,氢氧根转移的自由能反应较小。这项完整的机理研究可能为设计合适的水氧化催化剂提供思路。