Spin-orbit coupling and zero-field splitting of the high-spin ferric enzyme-substrate complex: Protocatechuate 3,4-dioxygenase complexed with 3,4-dihydroxyphenylacetate
We used density functional calculations to investigate the electronic origins of the magnetic properties of the high-spin ferric en- zyme-substrate complex protocatechuate 3,4-dioxygenase (3,4-PCD). The calculated g-tensors show that ligand-to-metal charge transfer transitions are from the protocate...
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Published in | Chinese science bulletin Vol. 58; no. 6; pp. 627 - 633 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Heidelberg
Springer-Verlag
01.02.2013
SP Science China Press |
Subjects | |
Online Access | Get full text |
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Summary: | We used density functional calculations to investigate the electronic origins of the magnetic properties of the high-spin ferric en- zyme-substrate complex protocatechuate 3,4-dioxygenase (3,4-PCD). The calculated g-tensors show that ligand-to-metal charge transfer transitions are from the protocatechuate (PCA) and Tyr408 orbitals to the Fe dπ orbitals, which lead to x- and y-polarized transitions. These polarized transitions require a spin-orbit coupling (SOC) matrix element in the z-direction, Lz (z = z'), resulting in a gz' value of 2.0158, significantly deviating from 2.0023. A large zero-field splitting parameter value of +1.147 cm-1 is due to AS = -1 spin-orbit mixing with the quartet states for the sextet ground state, accounting for around 73% of the SOC contribution. The SOC matrix elements indicate that the high-spin d5 system Fe(III), 3,4-PCD-PCA is a weak spin-crossover compound with an SOC of 31.56 cm-1. |
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Bibliography: | 3,4-PCD-PCA, g-tensor, zero-field splitting, spin-orbit coupling 11-1785/N We used density functional calculations to investigate the electronic origins of the magnetic properties of the high-spin ferric en- zyme-substrate complex protocatechuate 3,4-dioxygenase (3,4-PCD). The calculated g-tensors show that ligand-to-metal charge transfer transitions are from the protocatechuate (PCA) and Tyr408 orbitals to the Fe dπ orbitals, which lead to x- and y-polarized transitions. These polarized transitions require a spin-orbit coupling (SOC) matrix element in the z-direction, Lz (z = z'), resulting in a gz' value of 2.0158, significantly deviating from 2.0023. A large zero-field splitting parameter value of +1.147 cm-1 is due to AS = -1 spin-orbit mixing with the quartet states for the sextet ground state, accounting for around 73% of the SOC contribution. The SOC matrix elements indicate that the high-spin d5 system Fe(III), 3,4-PCD-PCA is a weak spin-crossover compound with an SOC of 31.56 cm-1. http://dx.doi.org/10.1007/s11434-012-5316-7 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1001-6538 1861-9541 |
DOI: | 10.1007/s11434-012-5316-7 |