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A new phase transition in LiNH4SO4 : an x-ray study
T. Simonson, F. Dénoyer, R. Moret
To cite this version:
T. Simonson, F. Dénoyer, R. Moret. A new phase transition in LiNH4SO4 : an x-ray study. Journal
de Physique, 1984, 45 (7), pp.1257-1261. �10.1051/jphys:019840045070125700�. �jpa-00209862�
1257
A new phase transition in LiNH4SO4 : an X-ray study
T. Simonson, F. Dénoyer and R. Moret
Laboratoire de Physique des Solides (*) Université de Paris-Sud, Bâtiment 510, F-91405 Orsay, France
(Reçu le 6 janvier 1984, révisé le 7 mars, accepté le 26
mars1984)
Résumé. 2014 Une étude par rayons X de LiNH4SO4 entre 295 K et 10 K montre l’existence d’une transition de
phase à 11 °C, et
unenouvelle transition entre 27 K et 28 K, qui semble du second ordre. Entre 284 K et 28 K, la symétrie est P21/c. Entre 27 K et 28 K, il apparaît
unesurstructure de vecteur d’onde q
=(1/2, 1/2, 0), qui double
la maille primitive, et donne la symétrie Cc.
Abstract.
2014X-ray studies of LiNH4SO4 between 295 K and 10 K show
aphase transition at 11 °C, and
a newtransition between 27 K and 28 K, which seems to be 2nd order. Between 284 K and 28 K, the symmetry is shown
to be P21/c. Between 27 K and 28 K,
asuperstructure of wave-vector q
=(1/2,1/2, 0) appears, doubling the pri-
mitive cell, and leading to the symmetry Cc.
J. Physique 45 (1984) 1257-1261 JUILLET 1984,
Classification
Physics Abstracts
61.60
-77.80
-81.30
1. Introduction.
The room temperature form of lithium and ammo-
nium sulfate is pseudo-hexagonal and closely related
to that of tridymite Si02. Its space group was deter- mined by Dollase [1] to be the polar, orthorhombic group Pc2, n or C’,, c being the macroscopic pseudo- hexagonal axis.
Till now, three phase transitions were known, one
at 186.5 OC, one at 11 °C, and one at room tempera-
ture at 7 kbars. We shall report the existence of a
new phase transition at 27 K, which had probably
been indirectly observed already by infrared absorp-
tion measurements [2]. The room temperature phase
has been shown to be ferroelectric [31. The phase
below 11 OC has been variously described as polar
and non-polar. According to Kruglik et al. [4], the
structure is antiferroelectric, with space group PI 2,/cl (C). References [31 and [5] also find the structure to be non-polar. However, references [2] and [61 both report detection of either a pyroelectric or a piezo-
electric signal below 11 °C.
To clarify this, and search for other phase transitions,
we did X-ray experiments between room temperature and 10 K on LiNH4SO4. We shall describe separa-
tely the experiments and results relative ,to the 11 °C and 27 K transitions.
(*) Associe
auCNRS.
2. Experimental : the 11 OC transition.
Between 295 K and 95 K, X-ray experiments were
done using the Burger precession technique, which gives an undeformed picture of a plane of reciprocal
space.
Monochromatic MoKa radiation (A
=0.709 A)
was selected by the (002) reflection of a pyrolithic graphite mono chromator. We were supplied with pre-oriented single-crystals by X. Gerbaux (1).
These were cooled by a flow of temperature-
regulated nitrogen gas. We were able thereby to
examine temperatures between 295 K and 95 K with a stability of approximately ± 0.5 OC.
Differential thermal analysis was also done between 480 K and 120 K. It revealed no phase transitions other than those at 186.5 OC and 11 "C.
Figure la shows highly overexposed pictures of
the reciprocal planes (hko), (hol) and (okl) above the 11°C transition. We can verify the extinction rules of Pc2l n. We also observe diffuse intensity, and particularly around the points (h
=± 3, k
=0,
1
=± 1/5) and (h = 0, arbitrary k, 1 = 2 p + I ± 1/5).
Microdensitometer measurements show the maxi-
mum of these diffuse spots to be located at G + qo, qo
=0.18 C* (G is the nearest reciprocal lattice
(’) Laboratoire Infrarouge Lointain, Universite de
Nancy I, C.O. 140, 54037 Nancy Cedex, France.
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:019840045070125700
1258
Fig. 1.
-Precession photographs of reciprocal planes (hol), (okl), (hko) at room temperature (ax and at various temperatures below 11 °C (b) : (okl) at 3 OC, (hol) at - 36 °C and (hko) at - 20 OC. Monochromatic Moka radiation
wasused (A
=0.709 A).
The small dots at (h
=± 3, 1 = 0) and (h
=0, odd) in (a) are due to contamination by the first harmonic A/2 of the beam.
vector). Their intrinsic width is approximately c*/5 by a* /3.
Figure lb shows the same planes below the transi- tion. The c glide plane has disappeared and the (0, k, odd I ) points are now visible; what’s mo.re,
new points have appeared in between these, showing
that the unit cell has doubled along the c direction.
The (k
=0, odd 1) reflections are invisible, as well
as the (h = 1 = 0, odd k) ones. Therefore the 2, axis
has been preserved and a c glide plane has appeared,
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orthogonal to it. The symmetry group is thus non-
polar : successive pseudo-hexagonal layers bear opposite dipole moments along the b axis. Nor is the group a sub-group of the high-temperature one :
the transition has no order parameter. The exact space group is easily found to be PI 21/cl, in agree- ment with Kruglik et al.
3. Discussion.
Since the transition is without an order parameter,
we cannot relate the fluctuations responsible for the
diffuse spots in figure 1 to a simple transition mecha- nism. They may be critical fluctuations relative to a
transition which could be induced by an external parameter, like mechanical strain. Or they may be due to a transition to a phase so limited in tempera-
ture as to be impossible for us to detect. We have not yet studied the variations of the diffuse intensity
with temperature.
In the latter case, despite the absence of dynamical data, one might associate tentatively the fluctuations with a vibrational mode Wj(qo) of very low frequency.
This mode would thus pilot a displacive transition
to a modulated phase of wave-vector not far from qo.
Several compounds of the tridymite family present such a transition : RbLiS04 [7] and K2SeO4 [8], for
instance. A group analysis of the dispersion branches
at the Brillouin zone boundary points shows that they
c* c*
are degenerate at k1 = 2 + yb* and k - 2 + za*.
Therefore they are not required by symmetry to have
zero slopes, and the Lifschitz criterion has no reason to be verified. A continuous transition is thus theo-
retically possible with a wave-vector of the form ac* + yb* or ac* + za*.
4. Low temperature experiments.
Preliminary photos were taken with the fixed-film
fixed-crystal method, with a cryocooler, between
100 K and 20 K. Between 30 K and 20 K, additional intense reflections appeared on the films, and we were
led to do a more elaborate experiment, using a Displex cryocooler on a 3-circle X-ray diffractometer in the normal beam geometry. The crystal was mounted in
a vacuum, on a copper support.
The temperature was measured by a chromel-Au-Fe
thermocouple attached to the sample holder. The actual crystal temperatures are estimated to differ from the temperature readings by less than 1 degree.
Copper radiation was used (A
=1.54 A ) and we were
able to observe the planes k
=0, k
= -1 and k
=1,
down to 10 K.
At 100 K, the space group is still PI 21/cl. At
10 K, however, superstructure reflectians of wave
vector q
=(1/2,1/2, 0) have appeared. Their intensity
is much smaller than that of basic reflections : at 10 K, I(1/2,1/2, - 7)
=2 290, 1(3/2, 3/2, - 9)
=210
and I(l, 1, - 7)
=12 120 (arbitrary units). The new primitive translations are a + b, a - b and c.
The c glide plane is still present, since the (k=O,
odd I) reflections are invisible. The cell is thus mono-
clinic, and the conventional basic cell is quadruple : (2a, 2b, c), the C face being centred (Fig. 2). We found
the monoclinic angle to be fl
=90.180.
In order to locate the critical temperature, we did series of scans around the reciprocal points (1/2, 1/2,
-
7) and (3/2, 3/2, - 9) with varying temperature.
The intensities and widths of these reflections are
shown as functions of temperature in figure 3. The
transition takes place between 27 K and 28 K. The intensity at (1/2, 1/2, - 7) goes continuously to zero,
and we found the same intensities and widths on
raising and on lowering the temperature. This indi- cates, within the precision of our measurements, a second-order transition.
Our geometry didn’t enable us to examine the 21
extinctions. However, the only subgroup of P2,/c
which explains the c extinctions and the centring of
the C face is Cl cl or Cf : the disappearance of the
b translation has done away with the 21 axis. We
cannot observe the symmetry of the H atoms, nearly
invisible to X-rays. Except for this, successive pseudo- hexagonal layers are still exchanged by the c glide plane, so that there should be no resultant electric moment along the b axis.
Aside from the transition discussed, a striking
feature of figure 3 is the sharp decrease in intensity at (1/2, 1/2, - 7) and (3/2, 3/2, - 9) between 13.2 K
and 16.4 K, as well as the slight, but distinct, broaden- ing of the latter reflection. These features require
further and more specific investigation.
Fig. 2.
-The change of primitive translations at the 27 K transition. A pseudo-hexagonal layer is shown. The tetra- hedra centres
areoccupied by sulfer (small tetrahedra) and
lithium (large tetrahedra) atoms alternately. The room temperature parameters
are a =9.14 A, b
=5.28 A,
c =