Authors: Veneta Grigorova, Dimitar Roussev, Stephane Jobic
Abstract: In the present paper we studied the thermodynamical behaviour under high pressure of
two MTe2-type compounds (M = Pd, Pt) by applying the thermodynamical method, which we
elaborated in previous studies [1,2]. The two discussed compounds are representatives of the CdI2
structure type, which is bi-dimensional and as such is atypical for the big family of lamellar MQ2-
type dichalcogenides (Q=S, Se, Te). Specific of lamellar structure is the strong ionicity of the
bonds. Its direct consequence is cleavage obtaining, lubrication properties, anisotropic physic
properties. One of the most interesting points stands on the possibility for realising interactions
between the layers of different types of ions. That could be done under high pressure by any of the
following transformation processes: (i) a phase transition to the typical pyrite structure; (ii) a phase
rearrangements changing the parameters of the crystal cell but keeping the 2D-type structure. The
computation of the volumetric thermodynamical functions showed that both PdTe2 and PtTe2 do not
undergo any classical phase transition [1]. But we observed a curious difference in their stability:
PtTe2 loosed its stability quite fast and PdTe2 was quite stable. Aiming to clarify if the difference in
the volumetric entropy generation was due to different phase rearrangements, we calculated the
longitudinal thermodynamical functions. In such a way we detected that both PdTe2 and PtTe2
undergo a phase rearrangement. The change along one of the space axis in both compounds was
compensated by the reverse change along the other space axis. Like this no changes at the
volumetric level were observed. The longitudinal calculations gave an explanation for the
differences in entropy generation at volumetric level: beyond the rearrangement point PdTe2
decreases its entropy generation, i.e. its new arrangement is somehow stable under increasing
pressure. While, beyond its rearrangement point PtTe2 increases its entropy generation, i.e. even in
the new arrangement it loses stability under increasing pressure. We conclude that both PdTe2 and
PtTe2 do not undergo a classical phase transition at volumetric level. At longitudinal level both
compounds undergo phase rearrangement. A difference between PdTe2 and PtTe2 is observed in
their entropy generation beyond the rearrangement point.
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Authors: Veneta Grigorova, Dimitar Roussev
Abstract: In the present study we elaborated a thermodynamical model for analysis of isothermal
phase transformations under high pressure. Our study was provoked by the necessity to characterise
the behaviour of MTe2 chemical compounds (M = Pd, Pt) while subjected isothermally to high
pressure. As known [1] MTe2 powders are representatives of the CdI2 structure type. This structure
type is a bi-dimensional one and as such is atypical for the big family of lamellar MQ2-type
dichalcogenides (M = Pd, Pt; Q = S, Se, Te). Specific of lamellar structure is the strong ionicity of
the bonds. One of the most interesting points stands on the possibility for realising interactions
between the layers of different types of ions. That could be done under high pressure by any of the
following transformation processes: (i) phase transition to the typical pyrite structure; (ii) phase
rearrangement changing the parameters of the crystal cell but keeping the 2D-type structure. In this
framework our aim was to elaborate a thermodynamical model for analysis of such isothermal
phase transformations under high pressure. Our analysis model is designed to answer the following
questions: (i) if the treated compound undergoes a classical phase transition or a phase
rearrangement; (ii) which is the order of the phase transition or the phase rearrangement,
respectively; and (iii) what is the degree-of-stability of the treated compound under high pressure.
To detect if the transformation process is a phase transition or a rearrangement, we compute both
volumetric and longitudinal Gibbs free energies and their partial derivatives. We recognise the
transformation to be: (i) a phase transition when it affects the volumetric Gibbs free energy and its
partial derivatives; (ii) a phase rearrangement if it affects the longitudinal Gibbs free energy and its
partial derivatives. The order of the transformation process (phase transition or rearrangement,
respectively) is determined by the order of the partial derivative of the Gibbs free energy
(volumetric or longitudinal, respectively), which is discontinuous in the transformation point.
Hence, we compute the two first partial derivatives (i.e., the first one and the second one) of the
Gibbs free energy (both volumetric and longitudinal). For characterising the degree of stability of
the treated compound under high pressure we calculate its entropy generation (volumetric and
longitudinal, respectively) during the treatment process. The established model was further applied
to PdTe2 and to PtTe2 while subjected isothermally to high pressure.
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