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INDUCED PARAMAGNETISM AND HYPERFINE INTERACTIONS IN THE ([FE4S4]-FE) ACTIVE SITE OF ESCHERICHIA COLI SULFITE REDUCTASE

机译:大肠埃希氏菌亚硫酸盐还原酶([FE4S4] -FE)活性位点中引起的超磁性和超精细相互作用

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摘要

The spin-coupling model of the {[Fe4S4]-siroheme} center of the active site of sulfite reductase is developed. The tetramer-siroheme coupling 2J(th)s(1) . s(h) results in the induced paramagnetism of individual ions of the Fe/S tetramer which provides non-zero effective hyperfine constants A(1,2) = - A(3,4) = - 33/8(J(th)/J)a(i), where J is the parameter of the Heisenberg pair-pair interaction in the Fe/S tetramer and a(i) is the local hyperfine constant. The siroheme g-factor contributes dominantly to the molecular g-factor, the tetramer contribution is small (approximate to(J(th)/J)(2), J(th)/J 1). The model explains the observed paramagnetism of the Fe/S component of the active site in Mossbauer, ENDOR and H-1 NMR experiments and concurrently the diamagnetism of this moiety in magnetic and EPR measurements. [References: 55]
机译:建立了亚硫酸还原酶活性位点的{[Fe4S4] -siroheme}中心的自旋耦合模型。四聚体-siroheme偶联2J(th)s(1)。 s(h)导致Fe / S四聚体的各个离子的感应顺磁性,从而提供非零的有效超精细常数A(1,2)=-A(3,4)=-33/8(J(th) / J)a(i),其中J是Fe / S四聚体中海森堡对-对相互作用的参数,而a(i)是局部超精细常数。西罗血红素g因子主要作用于分子g因子,四聚体作用较小(近似于(J(th)/ J)(2),J(th)/ J 1)。该模型解释了在Mossbauer,ENDOR和H-1 NMR实验中观察到的活性位的Fe / S成分的顺磁性,同时解释了在磁性和EPR测量中该部分的反磁性。 [参考:55]

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