SYNTHESES, CRYSTAL-STRUCTURES, AND CHARACTERIZATION OF BISMUTH PHOSPHATES

Citation
B. Romero et al., SYNTHESES, CRYSTAL-STRUCTURES, AND CHARACTERIZATION OF BISMUTH PHOSPHATES, Inorganic chemistry, 33(9), 1994, pp. 1869-1874
Citations number
19
Categorie Soggetti
Chemistry Inorganic & Nuclear
Journal title
ISSN journal
00201669
Volume
33
Issue
9
Year of publication
1994
Pages
1869 - 1874
Database
ISI
SICI code
0020-1669(1994)33:9<1869:SCACOB>2.0.ZU;2-E
Abstract
The syntheses of the three forms of bismuth phosphate have been optimi zed, and the resulting single phases have been characterized by therma l analysis, infrared spectroscopy, and powder X-ray diffraction. Two p hases may be obtained at room temperature, one trigonal (slightly hydr ated) and another monoclinic with a monazite-type structure. The cryst al structure of the trigonal phase, (stoichiometry BiPO4.0.67H2O, spac e group P3(1)21; a = 6.9885(2) angstrom, c = 6.4867(2) angstrom, Z = 3 ; R(WP) = 5.6%, R(F) = 3.6%) has been refined by the Rietveld method. The structure contains channels that run parallel to the c axis where the water molecules are located. This water is coordinated directly to the bismuth atoms and stabilizes this form respect to the monazite-ty pe BiPO4 under the synthetic conditions. But the trigonal phase is met astable (at room temperature it spontaneously loses all the crystalliz ation water in 2 months) and is transformed irreversibly to the monazi te-type structure. The crystal structure of this second form (stoichio metry BiPO4, space group P2(1)/n; a = 6.7626(1) angstrom, b = 6.9516(1 ) angstrom, c = 6.4822(1) angstrom, beta = 103.74(1)degrees) has been refined to R(WP) = 6.6% and R(F) = 3.7%. The monazite-type BiPO4 slowl y transforms into the high-temperature monoclinic form when it is heat ed above 600-degrees-C. The crystal structures of these three phases p resent some important similarities which are described in detail.