S. Scaccia et al. / Thermochimica Acta 413 (2004) 81–86
85
samples derived from water-alcohol solutions at ambient
temperature. The XRD patterns of the amorphous precipi-
tates calcined at 750 ◦C/10 h in air showed that the samples
are crystalline. The major reflections are attributed to the
trigonal quartz-like structure FePO4 [8], whereas other ex-
traneous minor reflections around 16.2, 27.7, 29.3, and 30.4◦
are indicative of the formation of Fe4(P2O7)3 secondary
phase [9]. Exception is made for the calcined precipitate ob-
tained by precipitation from water solution for which all re-
flections are attributed to the anhydrous iron phosphate [7].
By way of example only XRD patterns of the as-precipitate
derived from water–ethanol solution and the same sample
calcined at 750 ◦C are displayed in Fig. 1.
The TG/DTG/DTA curves of the as-precipitate iron phos-
phate obtained from aqueous solution is shown in Fig. 2a.
The TG curve shows a well-defined weight loss between
50 and 500 ◦C (DTG peak at 120 ◦C), which is ascribed to
elimination of crystallisation water. The total mass loss is
22.0%, which based on the total moles of iron and phos-
phorus (0.550) in the precipitate, corresponds to 2 moles of
H2O. The corresponding DTA curve shows one endother-
weight loss of about 1.0% between 500 and 600 ◦C oc-
curs, which is immediately followed by another small weight
loss of about 2.0% as seen in the TG curve. These weight
ferric sulphate or ammonium iron alum. The exothermic
peak at 546 ◦C is displayed in the DTA curve. This event
was assigned to a transition phase from amorphous to crys-
talline as evidenced by XRD [10]. Finally, a width exother-
mic peak at 768 ◦C without appreciable weight loss was
observed.
tal mass loss is 28.0%, which is higher than the expected
value for two moles of crystallisation water. Physically ab-
sorbed iso-propanol on the surface of the as-precipitate pow-
der could take account for this. The corresponding DTA
curve shows one endothermic peak at 105 ◦C. At higher
500 and 600 ◦C was observed. A large exothermic peak at
560 ◦C was displayed on the DTA curve. Again this event
was assigned to a transition phase from amorphous to crys-
talline form. Further, a small exothermic effect at 669 ◦C
followed by a weak endothermic effect at 716 ◦C without
appreciable weight loss was observed in the DTA curve.
The latter effect may be ascribed to the ␣ →  transi-
tion as above-mentioned for the as precipitate derived from
water–ethanol solution.
The scanning electron micrographs of the as-precipitate
iron phosphate powders showed similar uniform morpho-
logical features. The powders consisted of round particles
near 80 nm in size along with a narrow size distribution.
By way of example only the SEM image of iron phosphate
derived from aqueous solution is depicted in Fig. 3a. Con-
observed for all the samples. The morphological image of
the 750 ◦C-calcined iron phosphate derived from aqueous
medium showed a slightly increase of grain size (crys-
the 750 ◦C-calcined FePO4 derived from alcoholic media
showed that crystallites larger than 10 m in size are yield,
indicating that a sintering process occurs at high tempera-
tures (Fig. 3c and d).
The TG/DTG/DTA curves of the as-precipitate iron phos-
phate obtained from water–ethanol solution is shown in
Fig. 2b. The TG curve shows that the elimination of crys-
tallisation water occurs between 50 and 500 ◦C in two over-
lapped steps with DTG peaks at 117 and 365 ◦C. The to-
tal mass loss is 20.0%, which based on the total moles of
iron and phosphorus (0.540) in the precipitate corresponds
to 2 mol of H2O. The corresponding DTA curve shows one
endothermic peak at 105 ◦C. At higher temperatures, a sud-
den small weight loss of 0.5% between 500 and 600 ◦C was
observed. A large exothermic peak at 559 ◦C was displayed
on DTA curve. Again, this event was assigned to a transi-
tion phase from amorphous to crystalline form. Further, a
small exothermic effect at 669 ◦C followed by a weak en-
dothermic effect at 716 ◦C without appreciable weight loss
was seen in the DTA curve. The latter effect may be ascribed
to the ␣ →  transition as reported for quartz-like materi-
als of type MXO4 (M = B, Al, Ga, Fe, Mn and X = P,
AS) [11].
4. Conclusions
Amorphous iron(III) phosphate has been synthe-
sised by homogeneous precipitation from equimolec-
ular Fe(NH4)2(SO4)2·6H2O and NH4H2PO4 aqueous,
water–ethanol and water–iso-propanol solutions at pH = 2.0
and ambient temperature using hydrogen peroxide as pre-
cipitating agent. The presence of ethanol and iso-propanol
in the precipitation medium suppressed the co-precipitation
of ferric sulphate/or ammonium iron alum as it does in
aqueous medium, but trace level of a new secondary phase,
Fe2(P2O7)3 is formed. Thermal treatment at 750 ◦C yields
a crystalline quartz-like structured FePO4 with markedly
different morphological features.
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The TG/DTG/DTA curves of the as-precipitate iron phos-
phate obtained from water–iso-propanol solution is shown
in Fig. 2c. The TG curve shows that the displacement of
crystallisation water occurs between 50 and 500 ◦C in two
overlapped steps with DTG peaks at 98 and 365 ◦C. The to-
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