Crystal chemical characterization and computational modeling of a μ-oxo Fe(III) complex with 1,10-phenanthroline clarify its interaction and reactivity with montmorillonite

被引:10
作者
Brigatti, Maria Franca [1 ]
Sainz Diaz, Claro Ignacio [2 ]
Borsari, Marco [1 ]
Bernini, Fabrizio [1 ]
Castellini, Elena [1 ]
Malferrari, Daniele [1 ]
机构
[1] Univ Modena & Reggio Emilia, Dept Chem & Geol Sci, Via Campi 103, I-41125 Modena, Italy
[2] Univ Granada, IACT, CSIC, Av Palmeras 4, Granada 18100, Spain
关键词
Ab initio calculations; Iron phenanthroline; Montmorillonite; Thermal analysis; X-ray diffraction;
D O I
10.1007/s12210-017-0615-1
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
This work provides a systematic study of the mu-oxo-di-fac-[triaqua-(1,10-phenanthroline-kappa(2) N,N')-iron(III)]bis(sulfate), [(OH2)(3)(phen)FeOFe(phen)(OH2)(3)] (SO4)(2) (phen = phenanthroline). Crystal structure is determined by single-crystal X-ray diffraction data and refined to R = 0.039. The crystal structure is monoclinic (Z = 2), space group P2(1) with unit cell dimensions a = 8.5157(3), b = 17.6434(5), c = 9.9678(3) angstrom, beta = 90.133(2)degrees, V = 1497.62(8) angstrom(3). The triaqua(1,10-phenanthroline)iron(III) parts are linked through one oxo-bridge. Both Fe(III) cations show a distorted octahedral coordination. The single-crystal data are complemented by computational chemistry modeling at quantum mechanical level, X-ray powder diffraction at room and high temperature conditions and by thermal analysis. Molecular modeling suggests that the role of the crystallization water molecules is critical to establish the intermolecular interactions for the stability of the crystal structure.
引用
收藏
页码:605 / 614
页数:10
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