화학공학소재연구정보센터
Journal of the American Chemical Society, Vol.118, No.32, 7542-7550, 1996
Mossbauer-Spectroscopy of Spin-Coupled Iron-Chromium Complexes - Mu-Hydroxo-bis(Mu-Acetato)-Bridged Iron(2+)-Chromium(3+) and Mu-Oxo-bis(Mu-Acetato)-Bridged Iron(3+)-Chromium(3+)
We have analyzed Mossbauer spectra of a model complex of known structure with an Fe2+(S-1=2)-mu OH-Cr3+(S-2=3/2) center (A) and of its Fe3+(S-1=5/2)-mu O-Cr3+(S-2=3/2) analog (B). These mu-hydroxo and mu-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 = JS(1) . S-2 is weaker for the mu-hydroxo (J approximate to 21 cm(-1)) than for the mu-oxo (J approximate to 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 = beta S-eff.(g) over tilde(eff). H + S-eff.(A) over tilde(1)(eff). I-1 + I-1 .(P) over tilde(1) . I-1 - beta(n)g(n)H . I-1. For complex B, the zero-field splitting S-eff. D-eff. S-eff is also included in R(eff).In applied fields, the 4.2 K spectra of Fe2+ in A showed hyperfine splittings which allowed the determination of the following S-eff = 1/2 Hamiltonian parameters: 1/3 Tr (g) over tilde(eff) approximate to 2.00, (A) over tilde(1)(eff)/g(n) beta(n) = -(18.3,5.6,25.0) T, Delta E(Q) = +2.87 mm/s, eta = 0.93, and delta(Fe) = 1.22 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 Fe2+ by diagonalizing the (2S(1) + 1 = 5) x (2S(2) + 1 = 4) matrix of the Hamiltonian H = JS(1) . S-2 + Sigma(i=1)(2){S-i .(D) over tilde(i) . S-i + beta S-i .(g) over tilde(i) . H} + S-1 .(a) over tilde(1) . I-1 +I-1 + I-1 .(P) over tilde(1) . I-1 - beta(n)g(n)H . I-1. We determined the following parameters for Fe2+: D-1 = +4.0 cm(-1), E(1) = +0.4 cm(-1), 1/3 Tr (g) over tilde(1) greater than or similar to 2.07, <(alpha)over tilde>(1)/g(n) beta(n) = -(10.2,3.5,15.6) T. For complex B, we found that Fe3+ has a large quadrupole splitting (Delta E(Q) = -2.00 mm/s, eta = 0.22) presumably as a result of anisotropic covalency due to the close proximity of the bridging O2-. This large Delta 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 (g) over tilde(eff) = 2.01, (A) over tilde(1)(eff)/g(n) beta(n) = -(33.8,30.9,35.8) T, delta(Fe) = 0.52 mm/s.