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铁氧卟啉的密度泛函理论(DFT)和从头算研究:它们是否存在低能态的铁(V)-氧异构体?

DFT and Ab Initio Study of Iron-Oxo Porphyrins: May They Have a Low-Lying Iron(V)-Oxo Electromer?

作者信息

Radoń Mariusz, Broclawik Ewa, Pierloot Kristine

机构信息

Faculty of Chemistry, Jagiellonian University , ul. Ingardena 3, 30-060 Kraków, Poland.

Institute of Catalysis and Surface Chemistry, Polish Academy of Sciences , ul. Niezapominajek 8, 30-239 Kraków, Poland.

出版信息

J Chem Theory Comput. 2011 Apr 12;7(4):898-908. doi: 10.1021/ct1006168. Epub 2011 Mar 23.

Abstract

The energetics of various electromeric states for two heme complexes with an iron-oxo (FeO(3+)) group, FeO(P)(+) and FeO(P)Cl (P = porphin), have been investigated, employing DFT and correlated ab initio methods (CASPT2, RASPT2). Our interest focused in particular on tri- and pentaradicaloid iron(IV)-oxo porphyrin radical states as well as iron(V)-oxo states. Surprisingly, the iron(V)-oxo ground state is predicted for both models in vacuo. However, the presence of a polarizable medium, such as a solvent or a protein environment, favors the iron(IV)-oxo porphyrin radical cation, which is predicted to be the actual ground state of FeO(P)Cl under such conditions. Nonetheless, the iron(V)-oxo electromer is still expected to lie only a few kcal/mol above the ground state-a conclusion coming from both CASPT2 and RASPT2 calculations with a very large active space and further supported by a calibration with respect to coupled cluster CCSD(T) calculations for a simplified small model. The DFT results turn out to be strongly functional-dependent and thereby inconclusive. The widely used B3LYP functional-although correctly predicting the iron(IV)-oxo porphyrin radical ground state for FeO(P)Cl-seems to place the iron(V)-oxo states much too high in energy, as compared to the present CASPT2, RASPT2, and CCSD(T) results.

摘要

利用密度泛函理论(DFT)和相关的从头算方法(CASPT2、RASPT2),研究了两种含有铁氧(FeO(3+))基团的血红素配合物FeO(P)(+)和FeO(P)Cl(P = 卟啉)的各种电子异构态的能量学。我们特别关注三自由基和五自由基类铁(IV)-氧卟啉自由基态以及铁(V)-氧态。令人惊讶的是,在真空中两种模型都预测出铁(V)-氧基态。然而,存在可极化介质,如溶剂或蛋白质环境时,有利于铁(IV)-氧卟啉自由基阳离子,预计在此类条件下它是FeO(P)Cl的实际基态。尽管如此,铁(V)-氧电子异构体预计仅比基态高出几千卡/摩尔——这一结论来自于使用非常大的活性空间的CASPT2和RASPT2计算,并通过针对简化小模型的耦合簇CCSD(T)计算进行校准得到进一步支持。DFT结果强烈依赖于泛函,因此没有定论。广泛使用的B3LYP泛函——尽管正确预测了FeO(P)Cl的铁(IV)-氧卟啉自由基基态——但与目前的CASPT2、RASPT2和CCSD(T)结果相比,似乎将铁(V)-氧态的能量定得过高。

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