JOURNAL ARTICLE

The Synthesis of Mg3(PO4)2·8H2O and Its New Polymorphism

Takafumi KanazawaTakao UmegakiMasao Shimizu

Year: 1979 Journal:   Bulletin of the Chemical Society of Japan Vol: 52 (12)Pages: 3713-3717   Publisher: Oxford University Press

Abstract

Abstract Bobierrite, Mg3(PO4)2·8H2O, could be synthesized from mixed solutions of Na2HPO4 and MgSO4 at an initial pH of 6.4–7.0 with the addition of Ca(NO3)2, CuSO4, NiSO4, gelatin, or agar, by heating at 80–90 °C for 2–48 h. X-Ray studies indicated the coexistence of two kinds of lattice in each synthetic Mg3(PO4)2·8H2O crystal. One phase (Phase 1) is monoclinic, space group P21/m or P21 with a=10.08(2), b=27.86(3), c=4.656(7) Å, and β=105.0(2)°. The other phase (Phase 2) is monoclinic, space group C2/m, C2, or Cm, with a=10.07(2), b=13.38(2), c=4.656(7) Å, and β=105.0(2)°. If a centrosymmetric space group C2/m is assumed for the latter, Phase 2 may be considered to be a new polymorph of Mg3(PO4)2·8H2O, one belonging to the vivianite series. Newberyite, MgHPO4·3H2O, was also formed in the above synthetic procedure. This phosphate was precipitated under slightly more acidic conditions than those where Mg3(PO4)2·8H2O was obtained.

Keywords:
Monoclinic crystal system Chemistry Crystallography Crystal structure Polymorphism (computer science) Group (periodic table) Phase (matter) Stereochemistry Organic chemistry

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Citation History

Topics

Chemical Synthesis and Characterization
Physical Sciences →  Environmental Science →  Industrial and Manufacturing Engineering
Crystal Structures and Properties
Physical Sciences →  Materials Science →  Electronic, Optical and Magnetic Materials
Layered Double Hydroxides Synthesis and Applications
Physical Sciences →  Materials Science →  Materials Chemistry

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