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aDepartment of Materials Science and Engineering, College of Materials, Xiamen University, Xiamen 361005, Fujian Province, People's Republic of China
Correspondence e-mail: yaxihuang@xmu.edu.cn
Diammonium diaquabis(phosphato)triferrate(II), (NH4)2[Fe3(P2O7)2(H2O)2], was synthesized under solvothermal conditions at 463 K. The crystal structure, isotypic to its Mn and Ni analogues, is built from iron pyrophosphate layers parallel to (100), which are linked by ammonium ions sitting in the interlayer space via O-H
O and N-H
O hydrogen bonds. There are two crystallographic Fe sites in the crystal structure, one at a special position (2a, -1), the other at a general position (4e, 1). The former Fe atom on the inversion centre is coordinated by six O atoms, forming an FeO6 octahedron, while the latter is coordinated by five phosphate O atoms and one water molecule, forming an FeO5(H2O) octahedron. Each FeO6 octahedron shares trans edges with two FeO5(H2O) octahedra, forming a linear trimeric unit. These trimers share the lateral edges of FeO5(H2O) with other trimers, forming a zigzag chain running along [010]. The zigzag chains are further linked by P2O7 groups into a layered structure parallel to (100).
For background to this compound, see: Moore & Shen (1983
); Lii et al. (1998
); Alfonso et al. (2010
); Mi et al. (2010
). For background to the bond-valence method, see: Brown & Altermatt (1985
). For related structures, see: Chippindale et al. (2003
) for (NH4)2[Mn3(P2O7)2(H2O)2]; Lightfoot et al. (1990
) for K2Co3(P2O7)2·2H2O; Liu et al. (2004
) for Na(NH4)[Ni3(P2O7)2(H2O)2]; Wei et al. (2010
) for (NH4)2[Ni3(P2O7)2(H2O)2].
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Data collection: SMART (Bruker, 2001
); cell refinement: SAINT (Bruker, 2001
); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008
); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008
); molecular graphics: DIAMOND (Brandenburg, 2005
) and ATOMS (Dowty, 2004
); software used to prepare material for publication: SHELXL97 and WinGX (Farrugia, 1999
).
Supplementary data and figures for this paper are available from the IUCr electronic archives (Reference: FI2119 ).
This work was supported by the National Natural Science Foundation of China (No. 40972035), the Natural Science Foundation of Fujian Province of China (No. 2010 J01308) and the Scientific and Technical Project of Fujian Province of China (No. 2009 J1009).
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