Iron
porphyrins exhibit unrivalled catalytic activity for electrochemical
CO2-to-CO conversion. Despite intensive experimental and
computational studies in the last 4 decades, the exact nature of the
prototypical square-planar [FeII(TPP)] complex (1; TPP2– = tetraphenylporphyrinate dianion) remained
highly debated. Specifically, its intermediate-spin (S = 1) ground state was contradictorily assigned to either a nondegenerate 3A2g state with a (d
xy
)2(d
z
2
)2(d
xz,yz
)2 configuration or a degenerate 3Eg
θ state with a (d
xy
)2(d
xz,yz
)3(d
z
2
)1/(d
z
2
)2(d
xy
)1(d
xz,yz
)3 configuration.
To address this question, we present herein a comprehensive, spectroscopy-based
theoretical and experimental electronic-structure investigation on
complex 1. Highly correlated wave-function-based computations
predicted that 3A2g and 3Eg
θ are well-isolated
from other triplet states by ca. 4000 cm–1, whereas
their splitting ΔA–E is on par with the effective
spin–orbit coupling (SOC) constant of iron(II) (≈400
cm–1). Therfore, we invoked an effective Hamiltonian
(EH) operating on the nine magnetic sublevels arising from SOC between
the 3A2g and 3Eg
θ states. This approach enabled
us to successfully simulate all spectroscopic data of 1 obtained by variable-temperature and variable-field magnetization,
applied-field 57Fe Mössbauer, and terahertz electron
paramagnetic resonance measurements. Remarkably, the EH contains only
three adjustable parameters, namely, the energy gap without SOC, ΔA–E, an angle θ that describes the mixing of (d
xy
)2(d
xz,yz
)3(d
z
2
)1 and (d
z
2
)2(d
xy
)1(d
xz,yz
)3 configurations,
and the ⟨r
d
–3⟩ expectation value of the iron d orbitals that is necessary
to estimate the 57Fe magnetic hyperfine coupling tensor.
The EH simulations revealed that the triplet ground state of 1 is genuinely multiconfigurational with substantial parentages
of both 3A2g (<88%) and 3Eg (>12%), owing to their accidental near-triple degeneracy
with ΔA–E = +950 cm–1. As
a consequence of this peculiar electronic structure, 1 exhibits a huge effective magnetic moment (4.2 μB at 300 K),
large temperature-independent paramagnetism, a large and positive
axial zero-field splitting, strong easy-plane magnetization (g
⊥ ≈ 3 and g
∥ ≈ 1.7) and a large and positive internal field
at the 57Fe nucleus
aligned in the xy plane. Further in-depth analyses
suggested that g
⊥ ≫ g
∥ is a general spectroscopic signature
of near-triple orbital degeneracy with more than half-filled pseudodegenerate
orbital sets. Implications of the unusual electronic structure of 1 for CO2 reduction are discussed.