S.V. Stankus et al. / Journal of Alloys and Compounds 290 (1999) 30–33
33
Moreover, the relative differences between the densities of
the orthorhombic and the hypothetical (nonexistent in pure
salts) hexagonal phases of TbF3, DyF3, and HoF3 also lie
in this range [3]. (b) The mean TECs of the hexagonal
phases of the fluorides over the range from 293 K to the
smaller than the size of Gd31. Therefore, the first-order
solid–solid transitions in these salts had to occur at
temperatures much higher than 1310 K (Tt for GdF3). But
because TbF3 –HoF3 melt at 1420–1430 K, the first-order
transition is not observed in these compounds [2,9,13].
That is, TbF3, DyF3, and HoF3 conventionally remain in
the structure of b-YF3 type over the whole solid state
range. But actually, according to our evaluations [13], the
densities of the orthorhombic and hypothetical hexagonal
phases of DyF3 near the melting point are practically equal
to each other. In other words, in the vicinity of the melting
temperature the transformation in this compound (and,
probably, in TbF3 and HoF3) has already been completed
entirely by a continuous mechanism.
melting point are of the same order (|731025
K
21) and
in turn are significantly larger than those of the ortho-
rhombic modifications (|531025 21), so the difference
K
between the densities of two modifications decreases with
temperature. (c) The temperature of polymorphic trans-
formations in the SmF3 –GdF3 series rises (consequently,
the absolute value of the relative density change on
transition is diminished), as the size of cation decreases.
(d) The enthalpies of solid–solid transformations in SmF3 –
GdF3 are very small (about 10 times less than the
enthalpies of melting) [2].
To check the model of phase transformations in the
solids SmF3 –HoF3 proposed in this work, high-tempera-
ture investigations of the crystal structures of the rare earth
fluorides are required. We hope that our article will attract
interest to the research in this field.
These facts suggest that the distinctions between the
crystal structures of the orthorhombic and hexagonal forms
of the fluorides are also diminished with increasing
temperature. In fact, it has been demonstrated by
Garashina et al. [12], that the crystal lattices of b-YF3 type
and LaF3 type arise as a result of distinct distortions of a
common prototype structure (‘idealized’ lattice of LaF3
type). Therefore, the transformation from one form to the
other has a deformational mechanism and may occur over
a broad temperature range. This led us to propose that the
transformation from an orthorhombic form into a hexagon-
al one actually proceeds in two stages: first, over the
interval from 293 K to Tt the progressive deformation of
the crystal lattice of the b-YF3 type occurs; second, at the
transition temperature Tt a sharp change of lattice parame-
ters takes place. The first stage manifests itself by the fact
that the mean TEC of the orthorhombic phase is lower
when compared with that of the hexagonal one, resulting in
a decrease of the difference between the densities of two
modifications with increasing temperature. The second
stage shows itself as a first-order phase transition. As the
size of cation involved in the composition of the fluorides
of the SmF3 –GdF3 series is reduced, the value of Tt rises.
Consequently, the absolute value of the relative density
change at the first-order solid–solid transition is dimin-
ished, and the contribution of the continuous stage to the
overall process of transformation increases.
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The sizes of the cations in TbF3, DyF3, and HoF3 are