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The Glaserite-like Structure of Double Sodium and Iron Phosphate Na3Fe(PO4)2

โœ Scribed by V.A. Morozov; B.I. Lazoryak; A.P. Malakho; K.V. Pokholok; S.N. Polyakov; T.P. Terekhina


Publisher
Elsevier Science
Year
2001
Tongue
English
Weight
424 KB
Volume
160
Category
Article
ISSN
0022-4596

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โœฆ Synopsis


The double sodium and iron phosphate Na 3 Fe(PO 4 ) 2 was synthesized and studied by the XRD method, the second harmonic generation technique, and MoK ssbauer and IR spectroscopy. The compound crystallizes into a monoclinic system (space group C2/c) with unit cell parameters a โ€ซุโ€ฌ 9.0736(2) A > , b โ€ซุโ€ฌ 5.0344(1) A > , c โ€ซุโ€ฌ 13.8732(3) A > , โ€ซุโ€ฌ 91.435(2)3 and is found to be related to the K 3 Na(SO 4 ) 2 structure type. The crystal structure was determined by Rietveld analysis (R wp โ€ซุโ€ฌ 5.86, R I โ€ซุโ€ฌ 2.03). Iron cations occupy the M (Na) position while sodium cations occupy the X (K) and Y (K) positions of the glaserite-like structure. MoK ssbauer spectroscopy shows the presence of highspin Fe 3ุ‰ in octahedral coordination.


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Single crystals of sodium iron hydrogen phosphate, NaFe(HPO 4 )(H 2 PO 4 ) 2 ยดH2 O, were prepared hydrothermally by heating a mixture of Fe 2 O 3 , H 3 PO 4 and Na 2 CO 3 with a small amount of water. It crystallizes orthorhombic (Pbcn (Nยฐ60), Z = 8, a = 872.91( 7), b = 1249.54(8), c = 1894.4(1) pm)