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琥珀酸锰配合物的合成、结构与磁相变,MN(C4H4O4)。

Synthesis, structure and magnetic phase transitions of the manganese succinate hybrid framework, MN(C4H4O4).

机构信息

Department of Materials Science and Metallurgy, The University of Cambridge, Cambridge CB2 3QZ, UK.

出版信息

Chemistry. 2010 Jul 5;16(25):7579-85. doi: 10.1002/chem.201000390.

Abstract

An anhydrous manganese succinate, Mn(C(4)H(4)O(4)), has been synthesised hydrothermally and studied by single-crystal X-ray diffraction. It adopts a succinate pillared structure in which layers of corner-sharing MnO(6) octahedra alternate with sheets that contain chains of edge-sharing octahedra. This unique 3D framework structure contains highly distorted MnO(6) octahedra, which are made possible by the lack of ligand field stabilisation energy for the high-spin Mn(2+) ion. Attempts to dope the structure with other divalent transition-metal ions were accordingly unsuccessful. Magnetic susceptibility and heat capacity measurements indicate that Mn(C(4)H(4)O(4)) undergoes antiferromagnetic ordering below 12 K, with a second antiferromagnetic transition at approximately 6 K. These two antiferromagnetic phases undergo further transitions in applied fields, underlining the subtle magnetic behaviour that is possible in inorganic-organic frameworks of this structural complexity.

摘要

一水合琥珀酸锰,Mn(C(4)H(4)O(4)),通过水热法合成,并通过单晶 X 射线衍射进行了研究。它采用琥珀酸柱撑结构,其中角共享 MnO(6)八面体层与包含边缘共享八面体链的薄片交替排列。这种独特的 3D 骨架结构包含高度扭曲的 MnO(6)八面体,这是由于高自旋 Mn(2+)离子缺乏配体场稳定能所致。因此,尝试用其他二价过渡金属离子掺杂该结构的尝试均未成功。磁化率和热容测量表明,Mn(C(4)H(4)O(4))在 12 K 以下经历反铁磁有序,在大约 6 K 时经历第二次反铁磁转变。这两个反铁磁相在施加的磁场下进一步转变,强调了在这种结构复杂性的无机-有机骨架中可能存在的微妙磁行为。

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