H.-N. Girisha,
G.-Q. Shao*a and
B. Basavalingub
aState Key Laboratory of Advanced Technology for Materials Synthesis and Processing, Wuhan University of Technology, Wuhan, Hubei 430070, China. E-mail: gqshao@whut.edu.cn; Fax: +86 27 87879468
bDepartment of Studies in Earth Science, University of Mysore, Mysore, Karnataka 570006, India
First published on 17th August 2016
LaCrO3 based materials are currently utilized in a variety of electrical applications at high temperature. However, the morphology of LaCrO3 powder is much less understood as compared to its bulk counterpart. In this work, LaCrO3 powder was synthesized from LaCrO4 precursor by a supercritical hydrothermal technique (SHT). The majority exhibited a pure orthorhombic phase with well-monocrystallized grains of 3–9 μm. This work confirms that dominating faces in LaCrO3 grains are {0 1 0} and {0 1 1} surfaces, which have equivalent surface-energy due to the similarity of their surface structure.
Yoshimura et al.10,11 prepared LaCrO3 powder via SHT using La2O3 and Cr(OH)3·xH2O as starting materials. Pure orthorhombic LaCrO3 with irregular grains (0.7 ± 0.2 μm) was obtained (700 °C/3 h/100 MPa). Their work is innovative but has obvious imperfections. The oxide of La2O3 reacts heterogeneously with the hydrate of Cr(OH)3·xH2O. The obtained grains are irregular. The hydrate can easily absorb CO2 from atmosphere, thus introducing impure LaCO3OH phase. Another work by Rivas-Vázquez et al.12,13 may be considered as a quasi-SHT using LaCl3·7H2O, Cr(NO3)3·9H2O and NaOH as starting materials, because its temperature (350–425 °C) is in the vicinity of the supercritical point. Pure orthorhombic LaCrO3 with irregular grains (∼0.3 μm) was obtained. The reaction temperature and autogenous pressure are not high enough and the time is too short (1–2 h). The precursor from the strong alkaline solution contains Na+ which is difficult to be eliminated.
Considering the supercritical water is a poor solvent for polar molecules but excellent for non-polar ones due to its low dielectric constant and poor H-bonding, many non-polar compounds could be completely miscible.8,9,14 Higher pressure than the supercritical point is beneficial to enhance the reaction rate and supersaturation during nucleation and crystallization, but it would arouse the dielectric constant increasing. Otherwise, the Cr–O bond with [CrO4] tetrahedra in LaCrO4 has a stronger covalent character than that with [CrO6] octahedra in LaCrO3, and the La–O bond in LaCrO4 is more ionic than that in LaCrO3.15 Therefore, this work is to synthesize LaCrO3 powder via SHT under the condition (700 °C/200 MPa) which is different from those just beyond the supercritical point, and using a non-hydroxide of LaCrO4 precursor as the starting material. The phase purity, crystallization, particle size distribution and morphology are highly concerned.
The reaction process was studied by a differential scanning calorimetric and thermo-gravimetric instrument (DSC/TG, Netzsch STA 449C, Germany) at 10 °C min−1 in N2 (20 mL min−1). Phase determination was carried out by X-ray diffraction (XRD) at room temperature (RT), using a D8 Advance diffractometer (Bruker, Germany) at 0.02° s−1 (Cu Kα, 40 kV, 40 mA). The microstructure and composition of samples were examined by a field-emission scanning electron microscope (FESEM, HITACHI S-4800, Japan) and a transmission electron microscope (TEM, JEM-2100, JEOL, Japan) with selection area electron diffraction (SAED), equipped severally with an X-ray spectrometer for energy dispersive spectroscopy (EDS) analyses.
For the precursor, the endothermic peak at 814.7 °C, mass loss of −7.11 wt% (theoretical value −6.28 wt%) and DTG valley ranging 650–850 °C correspond to the decomposition:
![]() | (1) |
This is in agreement with the reported (663–840 °C).15,18,19 The endothermic peak at 1083.1 °C corresponds to the transition of LaCrO3 from rhombohedral phase to cubic one, in agreement with the reported by Gupta et al. (1000–1300 °C)20 but not with that by Hofer et al. (1550–1600 °C).21
For the powder via SHT, the endothermic peak at 240.1 °C corresponds to the transition of LaCrO3 from orthorhombic phase to rhombohedral one, in agreement with the reported (236–290 °C).5,6,12,13,19,20 The exothermic peak at 710.5 °C, mass loss of −0.35 wt% and DTG valley correspond to the crystallization of trace La-rich compounds aroused by SHT (Fig. 2 and 3, Table 1, eqn (4) and (5)). The endothermic peak corresponding to the transition of LaCrO3 from rhombohedral phase to cubic one has been merged in the wide valley. The exothermic peak at 1152.7 °C, mass increase of 1.45 wt% and DTG peak correspond to La2Cr3O12 formation from the relieved O2 and La2O3/Cr2O3 impurities which induced by the unexpected LaCrO4 decomposition:15
![]() | (2) |
![]() | ||
| Fig. 2 XRD patterns of the precursor (a) and powder via SHT (b) determined at RT. The inset is the enlargement from 30° to 80° for the powder via SHT. | ||
| EDS mapping microarea | Grain size (μm) | La/Cr (mol%) | Particles quantity |
|---|---|---|---|
| No. 1 | 0.1–0.4 | ∼1 | Trace |
| No. 2 | 0.5–1 | 1.4–1.7 | Trace |
| No. 3 | 1–3 | 6–8 | Trace |
| No. 4 | 3–9 | ∼1 | Majority |
| No. 5 | >9 | ∼1 | Trace |
The precursor resultant exhibits a pure monoclinic LaCrO4 (pdf 89-0448, CSD 81938).18,19
For the powder via SHT, the identified double peaks can tell that the powder is nearly a pure orthorhombic LaCrO3 (pdf 89-4504, CSD 50755)22 with trace impurities. Here the peaks ranging 90–140° for LaCrO3 powder were identified according to the refinement based on CSD 50755, and the refined lattice parameters are a = 5.5162(3) Å, b = 5.4802(6) Å, c = 7.7583(3) Å. The reaction can be expressed as:
![]() | (3) |
ln
PO2 and ΔG0 = 85731 − 85.096T.15 When ΔG = 0, the LaCrO4 starts to decompose: ln
PO2 = −20
623/T + 20.471. Initially these equations satisfied an open system, while this work involved a closed one. Considering that supercritical water is completely miscible with non-polar oxygen,14,23 the above equations could then be imported in our system. At the supercritical point of 373.946 °C, PO2 is equal to 10−5 atm. At the process temperature of 700 °C, PO2 is 0.48 atm. These indicate the SHT is a favorably thermodynamic system. If it reacted completely, the oxygen partial pressure built up inside the capsule (0.45 mL) would arrive at ∼6.7 MPa by the decomposition of precursor (0.19 g) at 700 °C. So the water pressure would be under ∼193.3 MPa, which remains all the same at the supercritical state. Otherwise, the formation of tiny impurity phases of La2CrO6 and Cr2O3 etc. (Fig. 2 and 3, Table 1, eqn (4) and (5)) would relieve the oxygen pressure. During the decomposition of LaCrO4 to LaCrO3, oxygen coordination around La atom(s) changes from 9 to 12 and around Cr atom(s) from 4 to 6. The major structural rearrangement during decomposition is thus mainly linked to high activation energy (∼18 kJ mol−1)24 and slow kinetics.15
}, {1
0} and {
0} (Fig. 3a). This is different with the reported10–13 in which irregular particles attained by SHT. Through ordinary MHT, LaCrO3 particles are with a cubic habit.5,6 Our work confirms first that dominating faces in LaCrO3 grains are {0 1 0} and {0 1 1} which have equivalent surface-energy due to the similarity of their surface structure.25 Such morphology could previously only be found in sintered samples through high temperature (e.g. 1450 °C/10 h/air),20 indicating a drastically-increasing sinterability through SHT process.
Particles with small (0.1–0.4 μm, No. 1) or very large (>9 μm, No. 5) sizes are also pure LaCrO3 (La/Cr ≈ 1). Two kinds of La-rich particles were found. One has a grain size of 0.5–1 μm with a La/Cr ratio of 1.4–1.7 (No. 2). The other is 1–3 μm with a La/Cr ratio of 6–8 (No. 3). The crystallite formation, growth and crystallization, from the LaCrO4 precursor to LaCrO3 grains, are initially as:15
![]() | (4) |
Being more amphoteric, the Cr3+-hydroxide condenses less readily than the La3+-hydroxide at a given alkalinity.6 The oxidation product of tiny CrO42− ions could be dissolved in the supercritical water and washed out later. This explains the large La/Cr ratio of 1.4–1.7 in La-rich particles.
Next, La2CrO6 decomposes to a mixture of LaCrO3 and La2O3:15
![]() | (5) |
Same analysis in eqn (4) can be applied in eqn (5). The large La/Cr ratio of 6–8 is due to the La2O3 resultant. The crystallization of one oxide in ordinary MHT proceeds by a dissolution–crystallization mechanism. However, the crystallization of LaCrO3 in SHT proceeds simultaneously with the decomposition of LaCrO4.12,13 The supercritical water gives a favorable reaction field for particle formation, owing to the enhancement of reaction rate and large supersaturation during nucleation and crystallization through lowering the solubility of LaCrO3 resultant. The process lasted 96 h and the reaction equilibrium is sufficient.
TEM images and SAED patterns of two typical LaCrO3 grains (a and b) are shown in Fig. 4. The dark contrast is aroused by large size of grains (∼5 μm for Grain-a in Fig. 4a-I, and ∼9 μm for Grain-b in Fig. 4b-I). Both grains have a La/Cr ratio close to 1 by EDS (not show here). From the SAED pattern of Grain-a (Fig. 4a-II), it can only be indexed as [0 0 1] zone axis of the orthorhombic LaCrO3. By tilting 18.85°, the [
3] zone axis was obtained (Fig. 4a-III). For Grain-b, the [
2] (Fig. 4b-II) and [0
3] (Fig. 4b-III) zone axes with tilting degree of 19.7° can also be indexed to the orthorhombic phase. These SAED analyses have unambiguously confirmed the crystal symmetry of orthorhombic structure in LaCrO3 samples by SHT. No cubic LaCrO3 particles were observed. LaCrO3 particles with single crystallites give a promising prospect for better properties comparing to those with polycrystallites.
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