Mn(HPO3):: A new manganese (II) phosphite with a condensed structure

被引:43
作者
Chung, UC
Mesa, JL
Pizarro, JL
Jubera, V
Lezama, L
Arriortua, MI
Rojo, T
机构
[1] Univ Basque Country, Fac Ciencias & Tecnol, Dept Quim Inorgan, E-48080 Bilbao, Spain
[2] Univ Basque Country, Fac Ciencias & Tecnol, Dept Mineral & Petrol, E-48080 Bilbao, Spain
[3] Univ Bordeaux 1, CNRS, ICMCB, UPR 9048, F-33608 Pessac, France
关键词
hydrothermal synthesis; X-ray diffraction; UV/v is and luminescent spectroscopies; magnetic behavior;
D O I
10.1016/j.jssc.2005.06.038
中图分类号
O61 [无机化学];
学科分类号
070301 [无机化学]; 081704 [应用化学];
摘要
A new manganese (II) phosphite with the formula Mn(HPO3) has been synthesised under mild hydrothermal conditions and autogenous pressure. Large pink coloured single crystals were obtained, allowing the resolution of the structure by x-ray diffraction. Mn(HPO3) crystallises in the P2(t)/c monoclinic space group with a = 8.036(3) angstrom, b = 8.240(3) angstrom, c = 10.410(3)angstrom, beta = 124.73(3)degrees and Z = 8. The structure consists of a three-dimensional, compact framework of edge sharing MnO6 octahedra linked to phosphite groups via oxygens. The presence of the phosphite anion has been confirmed by IR spectroscopy. Mn(HPO3) presents a high thermal stability limit of 580 degrees C, before rapid transformation to Mn2P2O7 occurs. Photoluminescence and diffuse reflectance spectroscopy studies show the presence of high spin Mn(II) in significantly distorted octahedral coordination with Dq and Racah parameters of Dq = 820, B = 910 and C = 3135 cm(-1). The ESR spectra, performed at different temperatures, are isotropic with a g-value of 2.00(l). Magnetic measurements indicate global antifierrornagnetic interactions with a ferromagnetic transition at 15 K, attributed to a canting of the antiferrornagneticaly aligned spins. (c) 2005 Elsevier Inc. All rights reserved.
引用
收藏
页码:2913 / 2921
页数:9
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