Inorganic Materials, Vol. 38, No. 12, 2002, pp. 1224–1227. Translated from Neorganicheskie Materialy, Vol. 38, No. 12, 2002, pp. 1444–1447.
Original Russian Text Copyright © 2002 by Ivanov, Baranov, Oleinikov, Tret’yakov.
Fractal Surfaces of ZrO , WO , and CeO Powders
2
3
2
V. K. Ivanov, A. N. Baranov, N. N. Oleinikov, and Yu. D. Tret’yakov
Kurnakov Institute of General and Inorganic Chemistry, Russian Academy of Sciences,
Leninskii pr. 31, Moscow, 119991 Russia
e-mail: van@igic.ras.ru
Received July 11, 2002; in final form, July 16, 2002
Abstract—The surface fractal properties of ZrO , WO , and CeO powders prepared by the thermal decom-
2
3
2
position of ZrO(NO ) , (NH ) W O , and (NH ) Ce(NO ) , respectively, were studied by mercury porosim-
3
2
4 4
5
17
4 2
3 6
etry. The results demonstrate that these oxides may, in principle, have fractal surfaces owing to topochemical
processes of the type A(s)
B(s) + C(g). The surface fractal dimension of individual crystallites and their
aggregates are determined.
INTRODUCTION
intrusion curve under the assumption that the pores had
a cylindrical shape. The contact angle between mercury
and the material was assumed to be 130°.
Earlier results on the surface structure of Fe O
2
3
powders differing in thermal history suggest that, when
conducted under relatively mild conditions to avoid
defect annealing and grain growth, the decomposition WO
The fractal dimension D of the ZrO , CeO , and
2
2
powders was extracted from Hg porosimetry data
3
of metal salts accompanied by gas release may yield using the Neimark formula [2]
oxide powders with fractal surfaces [1]. To verify this
V
assumption, we studied the surface fractal structure of
D = 2 + d log pdV /d(log p)
ZrO , CeO , and WO powders prepared by decompos-
2
2
3
∫
0
(
1)
ing ZrO(NO ) , (NH ) W O , and (NH ) Ce(NO ) ,
3
2
4 4
5
17
4 2
3 6
respectively.
=
2 + d(log f (p))/d(log p),
where V is the Hg intrusion volume, p is the applied
EXPERIMENTAL
V
pressure, and f(p) = p dV.
∫
0
ZrO samples were prepared by heating crystalline,
2
reagent-grade ZrO(NO ) to 315°C at 5°C/min, fol-
3
2
lowed by isothermal holding for 3 h.
RESULTS AND DISCUSSION
WO samples were prepared by heating crystalline,
3
According to XRD and Hg porosimetry data, the
thermal decomposition of zirconyl nitrate and ammo-
nium cerium nitrate at 315°C yields single-phase ZrO2
and CeO powders characterized by a high porosity and
specific surface (table; Figs. 1b, 1c). The WO powders
reagent-grade (NH ) W O to 580°C at 5°C/min, fol-
4
4
5
17
lowed by isothermal holding for 3 h.
CeO samples were prepared by heating crystalline,
2
2
reagent-grade (NH ) Ce(NO ) to 315°C at 5°C/min,
4
2
3 6
3
followed by isothermal holding for 3 h.
The powders were characterized by x-ray diffrac- smaller specific surface and a lower percentage of small
tion (XRD) on a DRON-3M diffractometer (CuK radi- (d < 0.03 µm) pores (Fig. 1a). Clearly, high-tempera-
ation) at a scan rate of 1–2°/min. The results were ana-
lyzed using JCPDS Powder Diffraction File (PDF2)
data.
obtained at a higher temperature (580°C) have a
α
ture defect annealing has a profound effect on the
microstructure of the materials.
An analysis of the Hg intrusion curves with the use
of the Neimark equation indicates that the WO powder
Microstructures were examined by scanning elec-
3
tron microscopy (SEM) on a JEOL JEM-2000FXII has a fractal surface with a fractal dimension D = 3.00 ±
instrument (accelerating voltage, 200 kV; magnifica- 0.02 (Fig. 2a), which is characteristic of the pore struc-
tions, up to ×20000).
ture of loose aggregates consisting of weakly bonded
oxide particles [1]. The same is evidenced by the limits
of the self-similarity range: 0.11 to 1.15 µm.
The porosity of preevacuated (1.3 Pa) samples was
determined by Hg intrusion porosimetry at pressures
from 0.3 to 220 MPa (Micromeritics PoreSizer 9300).
Fractal analysis of the curves obtained for zirconia
Cumulative and differential pore size distributions and powders reveals two distinct linear portions (d = 0.14–
specific surface areas were found by analyzing the 0.77 and 0.02–0.14 µm) with slopes corresponding to
0
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