ARTICLE IN PRESS
H.K. Poswal et al. / Journal of Solid State Chemistry 182 (2009) 136–140
139
˚
pressure marker (gold) and the gasket (tungsten). This indicates
that Zn(CN)2 transforms to an amorphous phase at ꢀ11 GPa. To
test whether this amorphous phase transforms to any crystalline
phase if overdriven, pressure was further raised up to ꢀ14 GPa.
However, our results show that it remained amorphous. On
release of pressure the diffraction pattern did not show any
reappearance of the crystalline structure, establishing irreversible
PIA of Zn(CN)2.
2.68 A. Due to the broad nature of these peaks, the diffraction
pattern could not be indexed [30]. However, careful analysis
shows that the broad peaks under non-hydrostatic pressures are
not the overlapped broadened peaks of hydrostatic experiments.
Thus the new phase observed under non-hydrostatic stresses is
distinct from that obtained under hydrostatic conditions. At still
higher pressures, the diffraction peaks became very broad and our
data suggests that by ꢀ10.5 GPa the sample became substantially
disordered and remained so upto ꢀ11.7 GPa. On release of
pressure, the sample remained in the disordered state i.e., did
not revert to any crystalline phase, much like in the hydrostatic
experiments. We should note that the disordered phase under
non-hydrostatic conditions still has some persistent diffractional
features at ꢀ11.7 GPa, at variance with the results obtained under
hydrostatic conditions where the sample became essentially
amorphous at ꢀ11 GPa. These results imply that under non-
hydrostatic conditions, the structure may not be as disordered as
under hydrostatic pressures and this difference may have its roots
in the fact that the preceding structures are different in these two
cases [31]
Several high pressure studies have earlier been carried
out on various cyanide compounds [32–34]. Raman investi-
gations on K2Hg(CN)4 show several phase transitions, proposed
to be related to the modifications of tetrahedra as well as
bending of C–Hg–C and Hg–C–N angles [32]. Hg(CN)2 has
substantially different structure but still undergoes several
high pressure phase transitions [33]. As mentioned in Section 1,
earlier high pressure investigations on Zn(CN)2 suggested
PIA of this compound at ꢀ1.6 GPa [23]. However, due to the
usage of laboratory X-ray source, the diffraction pattern had
poor signal/noise ratio and hence the present study supersedes
those results.
Before we present the results under non-hydrostatic pressure
conditions, it would be useful to state here a few general points.
As the non-hydrostatic conditions in a DAC are necessarily due to
the heterogeneous stress distribution, it is likely that the
diffraction peaks would be broader in this case. While, in
principle, non-hydrostatic stresses can change the nature of phase
transformation ([4,5,29] and reference therein), one should also
take care of the fact that the heterogeneity in stress distribution
can bring about multiple phase co-existence. However, when the
size of the grains in the powdered sample is orders of magnitude
smaller than the dimensions of the sample contributing to
diffraction pattern, one may expect a reasonable degree of
reproducibility in the experimental results. With these general
points, we present the diffraction patterns for Zn(CN)2 under non-
hydrostatic pressure conditions in Fig. 6. In this case the initial
cubic phase persisted up to ꢀ2 GPa, indicating somewhat
extended stability region of the cubic phase than under the
hydrostatic pressures. On further increase of pressure diffraction
peaks continued to broaden. At ꢀ3.5 GPa diffraction pattern
showed new, but broad, diffraction peaks at 4.75, 4.28, 3.65 and
The studies carried out so far do not elucidate the mechanism
of PIA of Zn(CN)2. We may mention that in some materials such as
in ice and quartz, softening of a transverse acoustic branch (and
hence an appropriate elastic constant) has been proposed to be
the mechanism for the PIA [35–37]. In such cases amorphous
phase may be viewed as an assemblage of a large number of
incommensurate states [38]. Such a mechanism for the amorphi-
zation would imply that this transformation should get completed
over a very small range of pressure, if not at a specific value of the
pressure. For Zn(CN)2, the amorphous/disordered phases arise
over a pressure range of ꢀ2 GPa, suggesting that softening of
elastic constants may not be the mechanism for Zn(CN)2. In any
case, for such a mechanism for Zn(CN)2, the computed elastic
modulus must be shown to vanish in the phase just preceding the
amorphous phase, necessitating its unambiguous structural
determination. A more general interpretation of PIA is that the
amorphous state is a kinetically preferred state brought about by
the inability of the compound to reach a higher coordinated
crystalline state [10]. A recent investigation on Zr(WO4)2 suggests
a similar mechanism is operative even for other compounds
showing NTE (which have a large number of low frequency
modes) [39]. This should encourage further studies on Zn(CN)2 at
high pressures and temperatures.
In conclusion, under the hydrostatic pressures, we have
observed three phase transformations i.e., cubic-orthorhombic
-cubic-II-amorphous. PIA is observed to occur at
ꢀ11 GPa, at variance with the results published earlier
where it was claimed to take place at ꢀ1.6 GPa [21,23]. In contrast,
under non-hydrostatic conditions, Zn(CN)2 undergoes two
structural transformations i.e., cubic phase to a partially dis-
ordered crystalline phase followed by an evolution to a substan-
tially disordered phase. Moreover, the disordered phase in
this case is different from that obtained under hydrostatic
conditions.
Fig. 6. X-ray diffraction patterns of Zn(CN)2 at a few representative pressures
under non-hydrostatic conditions. Open circles and asterisks represent the
diffraction peaks from tungsten gasket and gold pressure marker, respectively.