PHASE TRANSFORMATIONS DURING THE SYNTHESIS AND SINTERING
391
used a 2.5 M solution of ammonium bicarbonate, transmitted (transparent specimens) or reflected (polꢀ
NH4HCO3. The resultant precipitate was held in the ished surfaces) light.
precipitation medium for 24–63 h at room temperaꢀ
ture with constant stirring by a magnetic stirrer, then
filtered off, and dried in air at room temperature.
RESULTS AND DISCUSSION
During heating of (Y,Yb)2(CO3)3
cubic yttria particles nucleate and grow starting at
450–500 (Figs. 1a, 1b). The thermal decomposition
of the precursor involves the formation of monoclinic
yttria, ꢀY2O3, as an intermediate, metastable phase,
which is supported by the fact that the XRD patterns
of the samples calcined between 300 and 400 show
a halo in the range 28 –33 , which contains the
⋅
2Н2О in air,
To study the mechanisms of (Y,Yb)2(CO3)3 2Н2О
⋅
decomposition, phase transformations, and structural
changes during heating, the precursors were heatꢀ
treated in air at 110, 300, 400, 450, 500, 600, 800, 900,
°
С
β
1000, and 1100 С for 60 min at each temperature.
°
The sintering process was studied using nanopowꢀ
ders with a hypothetical composition of Y1.84Yb0.16O3
(3.2 at % Yb) after heat treatment of the precursors at
°С
2θ
°
°
strongest diffraction lines 111, 401, 402, 310, and 112
of monoclinic yttria (JCPDS PDF, card 47ꢀ1274)
(Figs. 1a, 1c). The asymmetric shape of the halo in the
900 С. Samples in the form of disks 10 mm in diameꢀ
°
ter and 2.5 mm in thickness were prepared by pressing
dry powder at 100 MPa with no plasticizers. The green
compacts were sintered in a vacuum electric furnace at
XRD pattern of the sample calcined at 450 С seems to
°
be due to the onset of cubic Y2O3 crystallization and
the presence of two yttria polymorphs: monoclinic
and cubic (Fig. 1b). Raising the synthesis temperature
1700 and 1950°С with a 1ꢀh hold at the final firing
temperature, followed by air annealing at 1450
°С.
Next, we determined the density and volume shrinkꢀ
age of the ceramics and examined their microstrucꢀ
ture.
to 500 С gives rise to the main diffraction lines of cubic
°
Y2O3 (JCPDS PDF, card 41ꢀ1105) and leads to the
formation of a single, yttriaꢀbased crystalline phase
(Fig. 1a).
Xꢀray diffraction (XRD) patterns were collected on
a Shimadzu XRDꢀ6000 diffractometer (Cu
K radiaꢀ
α
According to the differential thermal analysis
tion). The phases present were identified using JCPDS
PDF data and the software supplied with the diffractoꢀ
meter. The crystallite size was evaluated by the Scherꢀ
(DTA) data in Fig. 2, (Y,Yb)2(CO3)3
involves several steps. The large endotherm in the temꢀ
perature range 68 to 157 , with a maximum peak
temperature of 104 , corresponds to the release of
adsorbed water vapor. The weight loss in the temperaꢀ
ture range from 220 to 340 is due to the sequential
⋅
2Н2О pyrolysis
°С
rer formula: Dhkl
size, is the Cu
half maximum of the peak (rad), and
=
K
λ
/
β
cos
θ
, where Dhkl is the crystallite
is the full width at
is the angular
°С
λ
wavelength,
β
α
θ
°С
position of the peak (deg). We analyzed the 622, 400,
and 222 reflections from cubic yttria. The particle size
of nanopowders was estimated from their crystallite
size. When the precursor was heated from 600 to
detachment of two molecules of water of crystallizaꢀ
tion and carbonate groups. The exothermic event cenꢀ
tered at 340
crystallization of monoclinic yttria. The exotherm
between 477 and 607 , with a maximum peak temꢀ
perature of 540 , is due to the monoclinicꢀtoꢀcubic
phase transition of yttria. The exothermic peak cenꢀ
tered at 646 seems to result from structural ordering
°С is the decomposition of the salt and
1100 С, the average particle size of Yb:Y2O3 increased
°
°С
from 18 to 47 nm.
°С
The crystallite size extracted from XRD data was in
reasonable agreement with the average particle size
°С
(
D
BET) found as DBET
=
6/
ρ
SBET, where
ρ
is the theoꢀ
in the Y2O3ꢀbased cubic solid solution. The considerꢀ
able weight loss (up to 30%) in the sample at temperaꢀ
retical density (g/cm3) of the Y1.84Yb0.16O3 solid soluꢀ
tion and SBET (m2/g) is the BET specific surface area of
the precursor pyrolysis products (lowꢀtemperature
nitrogen adsorption measurements on a Micromeritꢀ
ics TriStar analyzer).
tures from 302 to 662 С is due to the decomposition of
°
the surface carbonates formed as a result of the
adsorption of the gaseous pyrolysis products (CO2) on
the large surface of quasiꢀdimensional monoclinic
yttria particles.
Thermal analysis was carried out with a Qꢀ1500
As the synthesis temperature is raised from 600 to
thermoanalytical system between 20 and 1200
°С at a
1100 С, the XRD peaks of our samples become stronꢀ
°
heating rate of 15 C/min. Gaseous products were
°
ger (Fig. 3), indicating an increase in the degree of
crystallinity, accompanied by an increase in crystallite
size from 18 to 47 nm, and improvement in the strucꢀ
tural perfection of the cubic Y2 – xYbxO3 substitutional
solid solution (bixbyite (Fe,Mn)2O3 structure, sp. gr.
identified by mass spectrometry on an STA 409 Luxx
thermal analyzer connected through a capillary to a
Netzsch QMS 403 Aëolos quadrupole mass spectromꢀ
eter (20–1200 , heating rate of 10
°
С
°C/min).
Microstructures of ceramic samples were examꢀ
ined by scanning electron microscopy on a Carl Zeiss
T 7
, Z = 16). No other crystalline phases were
)
h
Ia3
(
LEO 1420 and by optical polarizing microscopy in detected in the XRD patterns of the samples calcined
INORGANIC MATERIALS Vol. 47
No. 4 2011