Journal of the American Chemical Society · 1996 · 22 citations · 32 references
Natural SciencesBiochemistryChemistryInorganic ChemistrySpectroscopyStructural BiologyAntiferromagnetismMagnetic Properties Of SolidsMagnetism In SolidsMagnetism Of Inorganic CompoundsMössbauer SpectroscopyAntiferromagnetic ExchangeAntiferromagnetic OrderCoordination Compound MagnetismGround StatesMagnetic PropertiesMagnetic Properties Of Transition Metal ComplexesMagnetism Of Transition Metal ComplexesMössbauer Effect
We have analyzed Mössbauer spectra of a model complex of known structure with an Fe 2+ ( S 1 =2)−μOH−Cr 3+ ( S 2 = 3 / 2 ) center ( A ) and of its Fe 3+ ( S 1 = 5 / 2 )−μO−Cr 3+ ( S 2 = 3 / 2 ) analog ( B ). These μ-hydroxo and μ-oxo bridged binuclear metal centers display unusual magnetic properties as found in several diiron−oxo proteins. Our results confirm antiferromagnetic spin coupling between Fe and Cr ions which results in S eff = 1 / 2 and S eff = 1 ground states for A and B, respectively. The isotropic exchange ℋ ex = J S 1 · S 2 is weaker for the μ-hydroxo ( J ≈ 21 cm -1 ) than for the μ-oxo ( J ≈ 275 cm -1 ) complex. Spectra recorded at 4.2 K, in fields of 0.22−4.7 T, have been analyzed with the effective spin Hamiltonian for the ground state ℋ eff = β S eff · g̃ eff · H + + I 1 · P̃ 1 · I 1 − β n g n H · I 1 . For complex B, the zero-field splitting S eff · D̃ eff · S eff is also included in ℋ eff . In applied fields, the 4.2 K spectra of Fe 2+ in A showed hyperfine splittings which allowed the determination of the following S eff = 1 / 2 Hamiltonian parameters: 1 / 3 Tr g̃ eff ≈ 2.00, = −(18.3,5.6,25.0) T, Δ E Q = +2.87 mm/s, η = 0.93, and δ Fe = 1.21 mm/s. The weak coupling of A allows the zero-field splitting to mix higher spin manifolds with the ground state doublet, and, to obtain intrinsic parameters, we also calculated the spectra of Fe 2+ by diagonalizing the (2 S 1 + 1 = 5) × (2 S 2 + 1 = 4) matrix of the Hamiltonian ℋ = J S 1 · S 2 + + β S i · g̃ i · H } + S 1 · ã 1 · I 1 + I 1 · P̃ 1 · I 1 − β n g n H · I 1 . We determined the following parameters for Fe 2+: D 1 = +4.0 cm -1, E 1 = +0.4 cm -1, 1 / 3 Tr g̃ 1 ≳ 2.07, ã 1 / g n β n = −(10.2,3.5,15.6) T. For complex B, we found that Fe 3+ has a large quadrupole splitting (Δ E Q = −2.00 mm/s, η = 0.22) presumably as a result of anisotropic covalency due to the close proximity of the bridging O 2- . This large Δ E Q is comparable to values found in diiron−oxo proteins. Spectra of B in applied fields also displayed hyperfine splittings, and the following S eff = 1 Hamiltonian parameters could be deduced: D eff = +3.9 cm -1, E eff = +1.7 cm -1, 1 / 3 Tr g̃ eff = 2.01, = −(33.8,30.9,35.8) T, δ Fe = 0.52 mm/s.
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EPR of exchange-coupled systems
W. Weltner · Journal of Magnetic Resonance (1969) · 1990 · 700 citations
Origin of Effective Fields in Magnetic Materials
R. E. Watson, A. J. Freeman · Physical Review · 1961 · 617 citations
Crystal Structure of a Purple Acid Phosphatase Containing a Dinuclear Fe(III)-Zn(II) Active Site
Norbert Sträter, Thomas Klabunde, Paul A. Tucker et al. · Science · 1995 · 433 citations
Life Sciences, Biochemistry, Biology +17