Dinuclear and Hexanuclear Iron(III) Oxide Complexes with a Bis(bipyridine) Ligand: A New [Fe(6)(&mgr;(3)-O)(4)](10+) Core. 1998

Craig M. Grant, and Michael J. Knapp, and William E. Streib, and John C. Huffman, and David N. Hendrickson, and George Christou
Department of Chemistry and Molecular Structure Center, Indiana University, Bloomington, Indiana 47405-4001, and Department of Chemistry, University of California at San Diego, La Jolla, California 92093-0358.

The use of the bis(bipyridine) ligand L (1,2-bis(2,2'-bipyridyl-6-yl)ethane) has yielded new dinuclear and hexanuclear complexes. The FeCl(3)/NaO(2)CPh/L (4:4:1) reaction system in MeCN gives red-brown [Fe(6)O(4)Cl(4)(O(2)CPh)(4)L(2)][FeCl(4)](2) (1). The same reaction system in a 3:3:1 ratio in MeOH gives orange [Fe(2)(OMe)(2)Cl(2)(O(2)CPh)L][FeCl(4)] (2). Complex 1.2MeCN: monoclinic, P2(1)/a, a = 15.317(2) Å, b = 18.303(3) Å, c = 16.168(3) Å, beta = 108.91(1) degrees, and Z = 2. Complex 2: triclinic, P&onemacr;, a = 14.099(6) Å, b = 18.510(7) Å, c = 7.108(3) Å, alpha = 96.77(2) degrees, beta = 99.45(2) degrees, gamma = 81.16(2) degrees, and Z = 2. The cation of 1 consists of a near-planar [Fe(6)(&mgr;(3)-O)(4)](10+) core that can be described as three edge-fused [Fe(2)O(2)] rhombs to which are attached two additional Fe atoms. The cation of 2 contains a [Fe(2)(&mgr;-OMe)(2)(&mgr;-O(2)CPh)](3+) core. In both cations, the L group acts as a bridging ligand across an Fe(2) unit, with the bpy rings essentially parallel. Variable-temperature solid-state magnetic-susceptibility studies of 1 and 2 in the 2.00-300 K range reveal that for both complexes the data are consistent with an S = 0 cation and S = (5)/(2) [FeCl(4)](-) anions. These conclusions were confirmed by magnetization vs field studies in the 2.00-4.00 K and 10.0-50.0 kG ranges. Fitting of the data for 2 to the appropriate theoretical equation for an equimolar composition of Fe(2) cations and [FeCl(4)](-) anions allowed the exchange interaction in the cation to be determined as J = -10.5 cm(-)(1) (H = -2JS(1)S(2)) with g held at 2.00. The obtained J value is consistent with that predicted by a previously published magnetostructural relationship.

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