MODIFIED PECHINI SYNTHESIS OF Na3Ce(PO4)2
been observed. No secondary phases were detected in
orthophosphates synthesis was observed and ex-
plained in [16–18]. In acidic solutions, the HPO24– for
PO34– substitution is possible. By further heating of
the prepared material at temperatures higher than
500°C, the P2O74– anions are formed from HPO24– ac-
cording to the reaction: 2HPO24– ®P2O74– +H2O.
The XRD results confirm that the pyrophosphate
is present in sample B as the Na4P2O7 phase. Nature of
P2O47– anion in sample D is non-crystalline and it
could be not detected by XRD analysis.
Karpowich et al. [18] reported that pyrophosphates
could occur as a phosphate-rich amorphous phase at
grain boundaries, even after heating up to 800°C,
which could be also a good explanation of the amor-
phous state of P2O47– in sample D.
samples heated for 1 h at 1100°C
Ceria was formed in gels containing high con-
centration of citric acid and ethylene glycol. The oxi-
dation of Ce3+ to Ce4+ in the samples was possible un-
der strongly oxidizing conditions of the self-combus-
tion process, which was observed by heat treatment of
gels. Lowering of the organic precursors content in
the prepared sols has to prevent the Ce(III) oxidation,
as was in sample C. Further calcining the samples up
to 1100°C lowered the cerium dioxide and Na3PO4
content in samples, what indicated that samples cal-
cined at 780°C were not finally reacted.
The phase composition of powders calcined at
780°C was checked also by FTIR spectra (Fig. 2). The
main absorption bands were observed at 412–465,
547–601, 960 and 986–1118 cm–1. The bands at
986–1118 cm–1 were due to the asymmetric stretching
and the band at 960 cm–1 to the symmetric stretching
of PO4 group. The asymmetric and symmetric defor-
mation modes of the PO4 group can be observed at
547–601 and 412–465 cm–1, respectively. The above
mentioned absorption bands are in agreement with the
literature data for IR spectra of Na3Ce(PO4)2 com-
pound [1]. In sample C additional peaks at 860, 1367
and 1470 cm–1 were attributed to Na3PO4 phase [14],
which presence was first recognized by XRD. The
strong absorption at 734 cm–1 in sample B was proba-
bly due to symmetric stretching the POP group ob-
served for pyrophosphates [15]. Absorption at the
same position, but much less intensive, was recog-
nized for sample D, indicating the existence of
pyrophosphate in the obtained powder. The XRD and
FTIR results show that the pyrophosphates are built,
when nitric acid is used (samples B and D). The phe-
nomena of pyrophosphate formation on rare-earth
The average crystallite size of Na3Ce(PO4)2
phase calculated from the reflection broadening tech-
nique is found to be 47–53 nm (Table 1) for
samples B–D. The estimated dimensions are very nar-
row, almost independent on the concentration of citric
acid and ethylene glycol used in initial solutions. The
smallest crystallites of 38 nm dimension in sample A
were found, where EDTA without nitric acid addition
was used during synthesis of this material. This could
be explained by the fact, that stronger formation of
cerium chelates could be achieved in sample A than in
acidic conditions, as in sample B [19]. More efficient
complexing in solution prevented faster crystal-
lization of compounds.
The thermochemistry of phase transition of the
Na3Ce(PO4)2 compound was determined by the
TG/DSC analysis. Szczygiel et al. [6] reported, that
the polymorphic transition of the compound occurs at
constant temperature (i.e. 1060°C) during cooling of
molten samples and on heating of powders synthe-
sized in temperatures up to 1150°C. Two effects
(weak at 920 and strong at 1060°C) were observed
otherwise. Unfortunately the temperature of the first
one coincides with the point of b/d’-transition of
Na3PO4 (914°C). Since sodium orthophosphate could
be present in the binary compound as a secondary
phase or formed on its melting, we investigated firstly
the thermal behavior of a sample containing 60 mol%
of CePO4 and 40 mol% of Na3PO4. The sample exhib-
ited during cooling two exothermic effects in temper-
ature range 920–1060°C. Since in this temperature in-
terval monazite does not show any polymorphic tran-
sitions [17], then both effects are connected to
a/b-phase transition of Na3Ce(PO4)2.
The total enthalpy change of Na3Ce(PO4)2 phase
transition was determined on heating and cooling of
sample containing 50 mol% of monazite and 50 mol%
of sodium phosphate. One strong endothermic peak at
1060°C
with
the
enthalpy
change
of
14.1±0.5 kJ mol–1 was observed (Fig. 3). During cool-
Fig. 2 FTIR spectra of samples A–D calcined at 780°C
J. Therm. Anal. Cal., 93, 2008
691