1959
DOI: 10.1021/j150582a030
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Polymorphism of Rare Earth Disilicides

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Cited by 64 publications
(11 citation statements)
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“…. Eremenko et al reported the polymorphic transition between α‐Pr 5 Si 9 (orthorhombic) and β‐Pr 5 Si 9 (tetragonal) at Pr‐rich Pr 5 Si 9 to be at 157°C and the temperature was 57°C at 0.353 mole fraction Pr However, Perri et al reported the polymorphic transition temperature of the Pr 5 Si 9 phase was −123 ± 15 ºC, and what's more, Boutarek et al found three individual phases in the range of 0.333 to 0.385 mole fraction Pr using XRD and metallographic techniques. Recently, Pinguet et al studied the structural chemistry, magnetism, and electrical properties of binary Pr‐silicide.…”
Section: Literature Reviewmentioning
confidence: 99%
“…. Eremenko et al reported the polymorphic transition between α‐Pr 5 Si 9 (orthorhombic) and β‐Pr 5 Si 9 (tetragonal) at Pr‐rich Pr 5 Si 9 to be at 157°C and the temperature was 57°C at 0.353 mole fraction Pr However, Perri et al reported the polymorphic transition temperature of the Pr 5 Si 9 phase was −123 ± 15 ºC, and what's more, Boutarek et al found three individual phases in the range of 0.333 to 0.385 mole fraction Pr using XRD and metallographic techniques. Recently, Pinguet et al studied the structural chemistry, magnetism, and electrical properties of binary Pr‐silicide.…”
Section: Literature Reviewmentioning
confidence: 99%
“…There is an agreement that GdSi 2 has vacancy on the Si site so that the more accurate formula is GdSi 2−x ; a composition close to GdSi 1.4 was estimated by Perri et al [8] based on chemical analyses, X-ray and density measurements but the homogeneity was uncertain. A small range of homogeneity were reported ranging from 64 to 68 at.% Si [9] and 63.2 to 65.4 at.% Si [5], which corresponds to the formula GdSi 1.78-1.94 [9] and GdSi 1.72-1.89 [5], respectively; GdSi 2−x was also discovered to be dimorphic with a low temperature of orthorhombic structure and a high temperature of the ␣-ThSi 2 [10] tetragonal structure.…”
Section: Introductionmentioning
confidence: 99%
“…The line compound Gd 5 Si 3 is formed by the peritectic reaction: L + Gd 5 Si 4 → Gd 5 Si 3 at 1700 • C, while the other one Gd 5 Si 4 melts incongruently at 1725 • C. On the contrary, the monosilicide GdSi melts congruently at 1830 • C and does not have a significant homogeneity range. Both phases GdSi 2−x and GdSi ∼2 were the subject of controversy in literature [2][3][4][5][6][7][8][9]. Indeed, the stoichiometric composition of the silicide GdSi 2−x of AlB 2 type was attributed to the formula Gd 2 Si 3 (GdSi 1.5 , 60 at.% Si).…”
Section: Introductionmentioning
confidence: 99%