Inorganic Chemistry Communications 7 (2004) 584–587 www.elsevier.com/locate/inoche Synthesis and characterization of a new iron(III) oxide cluster containing two different discrete [Fe3O] units: [Fe3O(O2CCH@CHACH3)6(H2O)3][Fe3O(O2CCH@CHAH3)7 (H2O)2](HO2CCH@CHACH3)4(OH)(H2O) q Kou-Lin Zhang a a,* , Yu-Jun Shi b, Song Gao c, Yao-Dong Dai d, Kai-Bei Yu e, Xiao-Zeng You d,* Chemistry and Chemical Engineering College, Yangzhou University, Ximen Street, Yangzhou, 225002, P.R. China b Department of Chemistry, Nantong Teachers University, Nantong, 226007, P.R. China c College of Chemistry and Molecular Engineering, Peking University, Peking, 100871, P.R. China d State Key Laboratory of Coordination Chemistry, Nanjing University, Nanjing, 210093, P.R. China e Chengdu Branch of Chinese Academy of Science, Analysis Center, Chengdu, 610041, P.R. China Received 3 February 2004; accepted 19 February 2004 Published online: 12 March 2004 Abstract A new complex containing two different discrete trinuclear oxo-centered [Fe3 O] units has been synthesized and characterized by single crystal X-ray diffraction analysis and M€ ossbauer spectra. The M€ ossbauer spectra of the complex are typical of high spin iron(III) complexes. Ó 2004 Elsevier B.V. All rights reserved. Keywords: Synthesis; New iron(III) oxide cluster; Crystal structure; M€ ossbauer spectra Researchers have made efforts to design and synthesize the new molecule-based magnets because they exhibit polyfunctional solid-state properties [1–8]. Among these, the polynuclear iron-oxo complexes are receiving much attention. One of the fascinating aspects of the investigation of large iron clusters is that of providing models for the biomineralization of iron, which leads to such diverse compounds as magnetite and ferritin [9–13]. The recent discovery that iron-oxo clusters offer the potential of acting as precursors to molecule-based magnetic materials and even of functioning as nanoscale magnetic particles that they may display novel properties intermediate between those of simple paraq Supplementary data associated with this article can be found, in the online version, at doi:10.1016/j.inoche.2004.02.024. * Corresponding authors. Tel.: +8605147869171; fax: +860514797 5520. E-mail address: [email protected] (K.-L. Zhang). 1387-7003/$ - see front matter Ó 2004 Elsevier B.V. All rights reserved. doi:10.1016/j.inoche.2004.02.024 magnets and bulk magnets has added more interest in this area [14–16]. Over the past few years, a great number of such clusters with aesthetically pleasing structures and interesting magnetic properties have been synthesized and studied. Among them, oxo-centered carboxylate-bridged trinuclear iron(III) complexes of general formula [Fe3 (l3 -O)(O2 CR)6 L3 ]z (z ¼ 0, +1) have been synthesized and structurally characterized for a long time [17,18]. Attention has been focused almost exclusively on various properties of these complexes in the solid state. The highly symmetrical structure and the relatively large metal–metal distances, which exclude the possibility of direct metal–metal bonding make these attractive systems with which to examine magnetic and electronic interactions [18]. The mono cationic complexes which contain three high-spin iron(III) centers were some of the first polynuclear systems to which ideas of magnetic exchange were applied [19]. As an extension to the above areas, we have been investigating K.-L. Zhang et al. / Inorganic Chemistry Communications 7 (2004) 584–587 new synthetic procedures capable of allowing access to new structural types. Our interests are mainly focused on the molecular-based magnets [20,21]. In this paper, we report the preparation, crystal structure and M€ ossbauer spectra of the title complex. As far as we know, this is the first case that contains two different discrete Fe3 O units in the same complex. The reaction [22] of excess trans-2-butenoic acid with FeSO4 7H2 O in the presence of NaOH gives the new complex [Fe3 O(O2 CCH@CHACH3 )6 (H2 O)3 ][Fe3 O(O2 CCH@CHACH3 )7 (H2 O)2 ](HO2 CCH@CHACH3 )4 (OH) (H2 O). The X-ray analysis reveals [23] that the complex contains two different discrete Fe3 O units, one OH anion, one water molecule and four free trans-2-butenoic acid molecules. The formulae of the two trinuclear oxocentered units are [Fe3 O(O2 CC@CHACH3 )6 (H2 O)3 ]þ (unit 1, Fig. 1) and [Fe3 O(O2 CC@CHACH3 )7 (H2 O)2 ] (unit 2, Fig. 2), respectively. The unit 1 is a Fe3 O description. It carries a positive charge. The Fe(4)–O(18) and Fe(6)–O(18) distances are almost the same, but the Fe(5)–O(18) distance is slightly Again comparing the Fe–O (H2 O) shorter [1.886(3) A]. distances, we can see that the bond lengths of Fe(4)– while O(27) and Fe(6)–O(33) are the same (2.053(4) A), the Fe(5)–O(32) distance of 2.093(4) A is obviously longer than the former two. The triangle composed of the Fe(4), Fe(5) and Fe(6) atoms is very close to an equilateral triangle, with Fe(4)–Fe(5), Fe(5)–Fe(6) and Fe(4)–Fe(6) distances of 3.29(6), 3.27(2) and 3.30(6) A, respectively. The Fe(5)–Fe(6)–Fe(4), Fe(4)–Fe(5)–Fe(6) and Fe(5)–Fe(4)–Fe(6) angles are 60.1°, 60.4° and 59.4°, respectively. The central oxygen atom O(18) lies slightly and angles Fig. 1. The structure of the unit 1. Chief bond lengths (A) (°): Fe(4)–O(18) 1.914(3), Fe(5)–O(18) 1.886(3), Fe(6)–O(18) 1.901(3); O(27)–Fe(4)–O(18) 178.68(17), O(25)–Fe(4)–O(21) 171.18(15), O(19)– Fe(4)–O(23) 170.02(17), O(18)–Fe(5)–O(32) 177.55(17), O(28)–Fe(5)– O(20) 169.11(16), O(30)–Fe(5)–O(22) 167.17(15), O(29)–Fe(6)–O(26) 168.16(16), O(24)–Fe(6)–O(31) 170.93(18), O(18)–Fe(6)–O(33) 175.69(16). 585 and angles Fig. 2. The structure of the unit 2. Chief bond lengths (A) (°): Fe(1)–O(1) 1.872(3), Fe(2)–O(1) 1.951(3), Fe(3)–O(1) 1.904(3); O(1)–Fe(1)–O(10) 178.30(15), O(2)–Fe(1)–O(6) 167.46(16), O(8)– Fe(1)–O(4) 166.03(16), O(1)–Fe(2)–O(15) 178.87(15), O(11)–Fe(2)– O(3) 172.44(16), O(13)–Fe(2)–O(5) 176.03(16), O(1)–Fe(3)–O(17) 178.09(17), O(12)–Fe(3)–O(9) 169.21(16), O(14)–Fe(3)–O(7) 170.02(16). The Fe(III) above the Fe(4)Fe(5)Fe(6) plane (0.0094 A). coordination geometry is slightly distorted octahedron with a terminal water oxygen atom, an oxygen atom in the center of the triangle and any other four oxygen atoms from the bridging carboxylate groups completing the coordination to each metal atom. In unit 2, the Fe(1)Fe(2)Fe(3) triangle is also very close to an equilateral triangle, with Fe(1)–Fe(3), Fe(2)– Fe(3) and Fe(1)–Fe(2) distances of 3.26(2), 3.33(8) and respectively. The Fe(1)–Fe(2)–Fe(3), Fe(2)– 3.31(9) A, Fe(1)–Fe(3) and Fe(1)–Fe(3)–Fe(2) angles are 58.7°, 61.0° and 60.4°, respectively. The central oxygen O(1) atom lies slightly below the Fe(1)Fe(2)Fe(3) plane The Fe(1) and Fe(3) coordination geometry 0.0087 A. can be described as slightly distorted octahedron with four oxygen atoms from the bridging carboxylate groups, one terminal water oxygen atom and an oxygen atom in the center of the triangle completing the coordination to each metal atom. The Fe(2) coordination geometry is also a slightly distorted octahedron with four oxygen atoms from the bridging carboxylate groups, one oxygen atom from the unidentate carboxylate group and an oxygen atom in the center of the triangle completing the coordination to the atom. The whole unit (2) carries no charge. To our knowledge, although there are many oxocentered carboxylate-bridged triiron complexes that have been prepared and structurally characterized [17,18], this is the first case that contains two different discrete Fe3 O units in the same compound. The distance between O(1) and O(18) is 8.48(8) A. The measurements of M€ ossbauer Spectra taken without an external magnetic field consist of two 586 K.-L. Zhang et al. / Inorganic Chemistry Communications 7 (2004) 584–587 Fig. 3. 57 Fe Mossbauer spectra for the complex at 298 K (a) and 77 K (b). Table 1 M€ ossbauer parameters for the complex Temperature (K) Subspectrum I.S. (mm/s) Q.S. (mm/s) Rel. Int.(%) 298 The first doublet The second doublet 0.25 0.23 0.70 0.46 49.2 50.8 77 The first doublet The second doublet 0.38 0.37 0.85 0.49 49.5 50.5 measurements at 77 and 298 K (Fig. 3) [24]. Presumably the rapid motion of the magnetic iron electronic moments causes the quenching of the magnetic hyperfine structure, and both the spectra are doublets. It shows that iron in this compound has two different chemical environments. The observed values (Table 1) for the isomer shift, I.S., range from 0.38 mm/s (a-Fe) at 77 K to 0.25 mm/s at 298 K. The quadrupole splitting decreases with increasing temperature from 0.85 mm/s at 77 K to 0.70 mm/s at 298 K, values which are characteristic of high-spin iron(III) ions [25]. Acknowledgements We gratefully acknowledge the National Natural Science Foundation of China and the Nature Science Foundation of Yangzhou University for the financial support. References [1] C. Cartier dit Moulin, F. Villain, A. Bleuzen, M.A. Arrio, P. Sainctowit, C. Lomenech, V. Escax, F. Baudelet, E. Dartyge, J.J. Gallet, M. Verdagur, J. Am. Chem. Soc. 122 (2000) 6653. [2] Z.J. Zhong, H. Seino, Y. Mizobe, M. Hidai, A. Fujishima, S. Ohkoshi, K. Hashimoto, J. Am. Chem. Soc. 122 (2000) 2952. [3] J. Larrionava, M. Gross, M. Pilkington, H. Andres, H. StoeckiEvans, H.V. G€ udel, S. Decurtins, Angew. Chem. Int. Ed. Engl. 39 (2000) 1605. [4] M. Marchivie, P. Guionneau, J.A.K. Howard, G. Chastanet, J.-F. Letard, A.E. Goeta, D. Chasseau, J. Am. Chem. Soc. 124 (2002) 194. [5] R. Podgajny, C. Desplanches, B. Sieklucka, R. Sessoli, V. Villar, C. Paulsen, W. Wernsdorfer, Y. Dromzee, M. Verdaguer, Inorg. Chem. 41 (2002) 1323. [6] J.J. Sokol, A.G. Hee, J.R. Long, J. Am. Chem. Soc. 124 (2002) 7656. [7] R. Sessoli, H.-L. Tsai, A.R. Schake, S. Wang, J.B. Vincent, K. Folting, D. Gatteschi, G. Christou, D.N. Hendrickson, J. Am. Chem. Soc. 115 (1993) 1804. [8] W. Chen, Q. Yue, C. Chen, H.M. Yuan, W. Xue, J.S. Chen, S.N. Wang, J.C.S. Dalton, Transactions 1 (2003) 28. [9] B. Xu, D.J. Chasteen, J. Biol. Chem. 266 (1991) 1965. [10] A. Caneschi, T. Ohem, C. Paulsen, D. Rovai, C. Sangregorio, R. Sessoli, J. Magn. Magn. Mater. 177–181 (1998) 1330. [11] A.-L. Barra, P. Debrunner, D. Gatleschi, C.E. Schulz, R. Sessoli, Europhs. Lett. 35 (1996) 133. [12] M.A.J. Homes, R.E. Stenkamp, J. Mol. Biol. 220 (1991) 723. [13] J.B. Vincent, G.-L. Olivier-Lilley, B.A. Averill, Chem. Rev. 90 (1990) 1447. [14] D. Gatteschi, L. Pardi, A.L. Barra, A. Muller, J. Doring, Nature 354 (1991) 463. [15] C. Delfs, D. Gatteschi, L. Pardi, Comments Inorg. Chem. 15 (1993) 27. [16] T. Schneppensieper, G. Liehr, R.V. Eldrik, J. Ensling, P. Gutlich, Inorg. Chem. 39 (2000) 5565. [17] A.K. Powell, S.L. Heath, D. Gatteschi, L. Pardi, R. Sessoli, G. Spina, F.D. Giallo, F. Pieralli, J. Am. Chem. Soc. 117 (1995) 2491. [18] A.M. Bond, R.J.H. Clark, D.G. Humphrey, P. Panayiotopouious, B.W. Skelton, A.H. White, J. Chem. Soc., Dalton Trans. (1998) 1845. [19] A.B. Blake, A. Yavari, W.E. Hatfield, C.N. Sethulekshmi, J. Chem. Soc., Dalton Trans. (1985) 2509. [20] K.-L. Zhang, Y. Xu, C.-G. Zheng, Y. Zhang, Z. Wang, X.Z. You, Inorg. Chim. Acta 318 (2001) 61. [21] Z. Shen, J.-L. Zuo, S. Gao, Y. Song, C.-M. Che, H.-K. Fun, X.Z. You, Angew. Chem. Int. Ed. Engl. 39 (2000) 3633. [22] To a solution of trans-2-butenoic acid (2.724 g, 31.6 mmol) in water (50 ml) was added a solution of NaOH (0.210 g, 5.2 mmol) in water (5 ml). Then FeSO4 7H2 O (0.733 g, 2.6 mmol) was added to the above solution and refluxed for 24 h. The brown crystals were formed after several days (yield: 0.545 g). Anal. Calc. for C68 H102 Fe6 O3 : C, 42.04; H, 5.29. Found: C, 42.42; H, 5.11. [23] A brown crystal having approximate dimensions 0.46 0.24 0.12 mm3 was used for data collection. Diffraction data were collected with a Siemens P4 diffractometer using graphite-monochromated (Mo KaÞ radiation (k ¼ 0:71073 A), 2h–h scan mode. The structure was solved by direct methods and refined by a full-matrix least-squares on F2 method using the SHELXL 97 program package. Complete listings of bond distances and angles, hydrogen atoms coordinates and isotropic displacement parameters, anisotropic displacement parameters and least-squares plans are available quoting the deposition number CCDC-203970 (12 Union Road, Cambridge, CB2 1EZ, UK; E-mail: [email protected]). Crystal data: C68 H102 Fe6 O43 , 1942.60 g mol1 , triclinic, P-1, a ¼ 14:724ð3Þ A, b ¼ 17:818ð3Þ A, c ¼ 18:764ð5Þ A, a ¼ 103:200ð10Þ°, 3 , Z ¼ 2, b ¼ 107:95ð2Þ°, c ¼ 92:010ð10Þ°, V ¼ 4529:8ð17Þ A Dcalc ¼ 1:424 g cm3 , l(Mo KaÞ ¼ 1.024 mm1 , F ð0 0 0Þ ¼ 2020. 15,457 independent reflections were measured (Rint ¼ 0:0393). The K.-L. Zhang et al. / Inorganic Chemistry Communications 7 (2004) 584–587 structure was refined to R1 ¼ 0:0516 (wR2 ¼ 0:1049) for the reflections with I > 2rðIÞ (all data) and largest difference peak and 3 . hole were 0.623 and )0.416 e A [24] The M€ ossbauer experiments were carried out in zero applied magnetic fields using a 57Co/Pd source and a constant acceleration spectrometer to collect the transmission spectra at 298 and 587 77 K (Fig. 3). The spectrometer was calibrated using a standard aFe foil. The isomer shifts are determined relative to the center of the a-Fe spectrum. The MOSWIN program was used to determine the M€ ossbauer parameters. [25] R.S. Drago (Ed.), Physical Methods in Chemistry, W.B. Saunders Company, 1977, p. 500.
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