Phase Equilibria in the ZrO2–La2O3–Sm2O3 System at 1100°C
Phase equilibria and structural transformations in the ternary ZrO 2 –La 2 O 3 –Sm 2 O 3 system at 1100°C were studied by X-ray diffraction over the entire composition range. Fields of solid solutions based on the hexagonal (A) modification of La 2 O 3 , cubic (F) modification with fluorite-type str...
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Veröffentlicht in: | Powder metallurgy and metal ceramics 2020-07, Vol.59 (3-4), p.224-231 |
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Zusammenfassung: | Phase equilibria and structural transformations in the ternary ZrO
2
–La
2
O
3
–Sm
2
O
3
system at 1100°C were studied by X-ray diffraction over the entire composition range. Fields of solid solutions based on the hexagonal (A) modification of La
2
O
3
, cubic (F) modification with fluorite-type structure and tetragonal (T) and monoclinic (M) modifications of ZrO
2
, monoclinic (B) modification of Sm
2
O
3
, and an ordered intermediate phase with pyrochlore-type structure, Ln
2
Zr
2
O
7
(Py), were established to exist in the system. The boundaries of phase fields and lattice parameters of the phases were determined. In the zirconia-rich corner, solid solutions based on the tetragonal modification of ZrO
2
are formed. The solubility of La
2
O
3
in T-ZrO
2
is low and amounts to ~0.5 mol.%, which is evidenced by X-ray diffraction and microstructural analyses. The solid solutions based on the tetragonal modification of ZrO
2
cannot be quenched from high temperatures in the cooling conditions. The X-ray diffraction patterns recorded at room temperature show peaks of the M-ZrO
2
monoclinic phase. The ordered pyrochlore-type phase, Ln
2
Zr
2
O
7
(Py), is in equilibrium with all phases that exist in the ternary ZrO
2
–La
2
O
3
–Sm
2
O
3
system at 1100°C and forms substitutional solid solutions with phases of the binary systems. In the system, an infinite series of solid solutions form from the Ln
2
Zr
2
O
7
(Py) phase. The isothermal section of the ZrO
2
–La
2
O
3
–Sm
2
O
3
phase diagram at 1100°C contains three three-phase regions (T + M + Py, T + F + Py, A + B + Py) and eight two-phase regions (A + B, A + Py, B + Py, F + Py, F + T, T + M, T + Py, Py + M). New phases were not found to form at 1100°C. |
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ISSN: | 1068-1302 1573-9066 |
DOI: | 10.1007/s11106-020-00154-5 |