THE
SYSTEM
P.
W.
HQ-Tl
RICHTER
TO
and
HIGH
C. W.
F. T.
PRESSURES* PISTORIUS
The r-Hg/Hg,Tl, eutectic temperature rises aith pressure P(kbar) according to the equation t(‘C) = -60.0 - 4.09P L 0.013iP”. The Hg,TlJ$-Tl eutectic temperature (0.9’C at atmospheric pressure) rises linearly with pressure with a slope of 3.6.5’C/kbar. So marked influence of pressure on the eutect ic Moderate extrapolation of these curves and the melting curves of Hg, compositions was observed. Hg,Tl, and Tl suggests that a f.c.c. high-pressure phase of Hg may appear above -65 kbar on the melting curve, and that a f.c.c. solid-solurlon series may stretch from Hg to beyond the Hg,Tl, composition. _ibove -90 kbar the Hg-Tl system can be expected to consist of a continuous f.c.c. soltd-solution series. ETUDE
DU
STSTEJIE
Hg-Tl
AUS
PRESSIOSS
ELEVEES
La temperature de l’eutectique z-Hg/Hg,Tl., augmente avec la pression P (kbars), suivant 1‘Cquation La temp&ature de l’eutectique Hg,Tl,/&Tl (0,9’C iL la pression t(Y) = -60,O Y- 4,09P A 0,0132P”. atmoaph&ique) augmente linkairement avec la pression, avec une pente de 3,6S’C/kbar. ducune influence nette de la presaion sur la composition des eutectiques n’a Qt6 observee. Si on estrapole de faton raisonnable ces courbes ainsi que les courbes de fusion de Hg, Hg,Tl, et Tl, on trouve qu’une phase c.f.c. de Hg & pression &levee peut apparaitre au-dessus de 65 kbar environ sur la courbe de fusion, et qu’une sbrie de solutions solides c.f.c. peuvent apparaitre depuis Hg jusqu’au-del& de la composition de Hg,Tl,. _iudessus de 90 kbars environ, on peut s’attendre & ce que le syst&me Hg-Tl consiste en une s&e continun de solutions solides c.f.c. DAY STSTEM
Hg-Tl BE1 HOHEX
DRUCKEN
Die eutekt.ische Temperatur van r-Hg/Hg5T1? nimmt mit dem Druck P(kbar) gemal der Gleichung (0,9% bei Atmost(‘C) = -60.0 - 4,09P + 0,0132P’ zu. Die eutektische Temperatur van Hg,Tl,/p-Tl phtirendruck) nimmt mit dem Druck linear zu; die Steigung der Geraden ist 3,65”C/kbar. Der EixAuD des Druckes auf die eutektische Zusammensetzung ist nur sehr klein. Eine Extrapolation dieser Kurven und der Schmelzkurven van Hg, Hg,Tl, und Tl deutet darauf bin, da0 oberhalb ~65 kbar auf der Schmelzkurve eine kubisch-fliichenzentrierte Hochdruckphase des Hg auftreten kdnnte und da13 sich eine kxbisch.fllchenzentrierte Legierungsreihe von Hg bis jenseits der Hg,Tl,- Zusammensetzung erstrecken kdnnte. Oberhalb -90 kbar kann man damit rechnen, da13 das System Hg-Tl aus einer kontinuierlichen Reihe kubisch-fltichenzentrierter Legienmgen besteht.
INTRODUCTION
The system Hg-Tl has attracted considerable interest , partly because the alloys are liquids at WC in the range 043 at. oA Tl. The system contains only one binary compound Hg,TI,, with a melting point of l-i.5’C. The x-Hg/Hg,Tl, eutectic is located at 8.5 to -6O’C, and t,he Hg,Tl,/$-Tl at. % Tl, -59’C eutectic at 40 at. % Tl, 0.6”C.(1) Solid Hg,Tl, is disordered f.c.c.,t2) and its lattice is capable of accommodating several percent of excess Hg or Tl. Thermod_ynamic(3) as well as liquid S-ray diffraction data(dT6) indicate that there is a more orderly arrangement in the liquid at the compound composition than at other compositions, and that the liquid retains some solid state characteristics with respect to short-range order. The maximum in t.he liquidus at the composition Hg,Tl, is broad and flat, with the liquidus line above 10°C from ~23 to ~35 at. % Tl. The high-pressure melting curves of Hg?“) Hg,Tl,,(*) and T1(g-lo) have been studied. By moderate estrapolation of the melting curve of Hg5Tl, it appeared that the melting curves of Hg and Hg5T12are tithin -10°C of each other from 25 kbar to at least 60 kbar, and possibly even beyond that.@) Furthermore, Hlel Received May 30, 1972. t Chemical Physics Group of the Kational Physical Sational Chemical Research Laboratories, P. 0. Box Pretoria, South Africa.
ACT_% METALLURGICA,
VOL.
21, APRIL
1973
and 395,
ment et al.“) concluded that the rhombohedral angle of the x-Hg unit cell (70.6”) would decrease with pressure along the melting curve, and suggested that the a-Hg structure continuously distorts toward f.c.c. with pressure. If this is the case, a point XTilleventually be reached, possibly via a discontinuous transition to a f.c.c. high-pressure phase of Hg, There the solidsolubility limits of f.c.c. Hg,Tl, will include Hg itself. This may result in the disappearance of the Hg/Hg5T12 eutectic point. The high-pressure pol_ymorph Tl III (above -9Okbar on the melting curve and above -37 kbar at P.5”C(g)) is also f.c.c.cll) Ultimately, therefore, it is possible that the system Hg-Tl at very high pressures may consist only of a continuous f.c.c. solid-solution series near the liquidus. Some inferential indications of such behaviour can be obtained from the effect of pressure on the eutectic temperatures in this system, and it xvas consequently decided to study these as functions of pressure. EXPERIMENTAL
Thallium rod with a stated purity of 99.999x, obtained from Koch-Light Laboratories, and triply distilled mercury, obtained from Johnson, Xatthey Bt Co., were .sveighed and thoroughly mised at room temperature in the two eutectic compositions. The samples obtained were stored under a nitrogen atmosphere. 391
ICTA
39’2
WETALLVRGICA.
generated in a piston-cylinder Pressures xere apparatus.(r”) Melting was observed by means of differential thermal analysis (DTX), using ChromelThe detailed esperimental Alumel thermocouples. procedure has been described before.(13) The samples were contained in stainless steel capsules, with no evidence of contamination. In order to prevent gross leakage, the pressure plate was first cooled to well below the eutectic points before pressure was applied to seal a capsule in situ. Heating-cooling rates were in the range 0.4-l .l”C/sec. Only melting temperatures are plotted. The eutectic melting curves obtained are believed to be correct x-ithin 2°C and ~1 kbar. Originally it was intended also to study the changes in the eutectic compositions brought about by pressure. This can, in principle, be done by completely melting the sample in every heat.ing-cooling cycle, and measuring the amount by which the beginning of freezing (i.e. the liquidus) exceeds the beginning of melting (i.e. the eutectic temperature). A comparison with the shapes of the intermediate liquidus curves then yields the effect of pressure on the eutectic composition, assuming one had started with the eutectic composition at atmospheric pressure. Even more accurate results could be obtained if runs are, in addition, made at compositions removed from the eutectic so as to yield information regarding the changes in the shapes of the liquidus curves with pressure. Unfortunately, however, we were unable to seal the capsules sufficiently well so as to preclude slight leakage of the samples after repeated complete heatingcooling cycles. Even the slightest leakage of the sample resulted in complete shorting of the thermocouples. It is suspected that the cause of leakage was minute amounts of liquid alloy trapped betxeen the capsule and its stopper, thereby preventing a complete Nevertheless, some isolated capsule-stopper seal. instances of complete heating-cooling cycles rrere obtained. In general, however, heating was stopped as soon as the sample started to melt, in order to prevent leakage.
VOL.
21.
2
?
1973
I 1
I ;
PilESSURE
FIG. 1. Effect
23
-
25
I
1
10
*5
KILOBARS
of pressure on the r_x-Hg/Hg,Tl, temperature.
eutectic
with a standard deviation of 0.8”C. The slope of the curve rises to 4.88 deg/kbar at 30 kbar. The highest pressure at which a complete meltingfreezing cycle was obtained without leakage was that of the cycle shown in Fig. 2. The pressure was 15.9 kbar, with an eutectic temperature of 9.2’C, whereas freezing started at 10.2% on the cooling cycle. The Hg5Tl,/$-Tl eutectic curve, shown in Fig. 3, is based on t1v-o separate consistent runs. The DTA signals obtained mere similar to, but somewhat sharper than, signals obtained for the a-HgiHg,Tl, eutectic. Our present atmospheric pressure eutectic point is 0.9 t O.S”C in good agreement with the literature.(l’ Within our present accuracy, no curvature on the eutectic line in the P-T plane could be observed, and
RESULTS
The x-Hg/Hg,Tl, eutectic curve, shown in Fig. 1, is based on several consistent and independent runs. Sharp and clear DTA signals (Fig. 2) were obtained over the pressure range studied. Our present atmospheric pressure eutectic point is -60 5 l°C in good agreement with the literature.“) The eutectic line has a slight but definite upwards (dsT/dP’ > 0) curvature in the P-T plane. The experimental points, lvith P in kbar, were fitted by t(“c) = -60.0
+ 4.09P + 0.0132P’
I
INCREASING
m
TIME
FIG. 2. Typical DT_A signal obtained at. 15.9 kbar for an original composition corresponding to the a-Hg/Hg,Tl, eutectic. Point d (9.YC) represents the eutectic temperature and point B the liquidus (102’C).
RICHTER
ASD
PISTORIUS
PRESSURE FIG. 3. Effect
the esperimental
THE
- KILOBAR
of pressure on the Hg,Tl,/B-Tl temperature.
points
SYSTEM
eutectic
were fitted by
t(“C) = 0.9 + 3.63P with a standard deviation of O.‘i’C. A complete melting-freezing cycle at 30.1 kbar resulted in almost exact agreement between the beginnings of melting and freezing.
Hg-Tl
TO
HIGH
393
PRESSURES
shifts lvith pressure towards a higher thallium content, the compositional change must be negligible. However, if the shift is in the opposite direction, even a change of 1 at. % would result only in -1’C difference between the liquidus and eutectic temperatures. Severtheless, even in this direction the shift cannot exceed this value. It can therefore be concluded that, at least in the pressure range studied, the assumptions of only a small effect of pressure on the eutectic compositions are justified. Positive curvature (i.e. d*T/dP” > 0) of the melting curve of a pure substance is an extremelv rare phenomenon. It is known for cerium, but in that case is almost certainly due to electronic changes. In the case of eutectic curves, however, positive curvature may be common, since even very slight changes in the eutectic composition with pressure could, in principle, give rise to this behaviour. The positive curvature observed for the c+Hg/Hg,Tl, eutectic curve is almost certainly due to such an effect. Figure 4 shows that the effect of pressure on the liquidus curves is one of a flattening-out of the maxima. At atmospheric pressure the x-Hg/Hg,T& eutectic is 74.5% below the melting point of Hg,Tl,, while at 40 kbar this difference has decreased to NX’C. Similarly, the Hg,Tl,/B-Tl eutectic at atmospheric pressure is 14°C below melting point of Hg5T12, while
DISCUSSION
It is now possible to construct a series of curves representing the liquidus lines of the Hg-Tl system at different pressures, using earlier data for the melting curves of Hg,(‘) Hg,Tl,(s) and Tl@-lO) in conjunction with the present results for the two eutectic curves. The assumption is made that the eutectic compositions do not change markedly lviiith pressure. The resulting curves are shown in Fig. 4. Since no experimental data are available at intervening compositions, the curvatures of the liquidus lines may change in a somem-hat different fashion to those indicated in the figure, but in essence this family of curves can be espetted to reproduce the high-pressure behaviour in this system. Several conclusions can immediately be drawn. The 1°C difference between the liquidus and eutectic temperatures of the r-Hg/Hg,Tl, composition at 15.9 kbar represent a change in the eutectic composition of only -0.03 at. %/kbar, but, of course, the direction of the change is not indicated. This effect is sufficiently small to be of littleimportance at present. In the case of the Hg5Tl,/&T1 eutectic, where essentially no difference was observed at 30 kbar between the liquidus and eutectic temperatures, it is obvious from Fig. 4 that if the eutectic composition
I 5CO
c
1
-‘OOo
”
”
I
I
I
10
20
30
’
“1
I8
40 At.
50 - %
1
I
I
I,
60
70
80
b
I 90
100
TO
FIG. 4. Liquidus lines in the system Hg-TI at various pressures. A: atmospheric pressure;“’ B: 10 kbar; C: 20 kbar; D: 30 kbar E: 40 kbar; F: Extrapolated to 50 kbar. Subsolidus relations are not shown, and the assumption (at least partly justified-see text) is made that the eutectic compositions do not change with pressure. The curvatures of the high-pressure lines (shown here as dashed curves) may be slightly in error.
ACT.1
394
at 40 kbar the difference
is only -4.X.
the Hg5TI,/$-Tl
xith
eutectic
at atmospheric
pressure
and
but due to the curvature the difference
of 302°C
beyond
-45
eutectic
kbar.
pressure
tively,
but above this pressure
these points are at ~ZO’C!,
olation
of melting
of extrapolation curvatures olation
curve
of Hg5Tl, at the same
of cr-Hg and the that
comparatively also small.
mainly
rapidly Further-
at 60 kbar
i.e. essentially
curves is hazardous, is
involved
would
kbar, ZWC.
It is here conceded
affect
x-Hg/
the extrap-
but the range
small,
and
the
Any errors in extrapthe
critical
pressure
obtained. It would therefore n-hat above the
z-Hg/HgjT1,
corresponding suggest,ing
at
may
to
maximum
of Hg,TI,
w-ill disappear,
pressures,
a continuous
stretch
This necessitates
f.c.c. high-pressure before.“)
higher
some-
corresponding
as well as the
to the melting series
at. % Tl.
the minimum
eutectic
that,
solid-solution ~40
appear that at a pressure
60 kbar
from
Hg itself
the appearance
to of a
phase of Hg, as has been predicted
Furthermore,
above -90
kbar Tl itself be-
comes f.c.c.,
and it can be expected
solid-solution
series above this pressure will include the
complete
range of compositions
that
the f.c.c.
in this system
from
Hg to Tl. Another,
somewhat
rhombohedral
less probable,
x-Hg transforms
phase via a higher-order
possibility
continuously
decreases
is that
to a f.c.c. high-pressure
transformation.
be the case if the cc-Hg rhombohedral lvith pressure
five-fold
greater
axis than perpendicular shape of the Hg-Tl
stifiness
to it.
How-
q-stern at high
woulcl be the same as in the case of a first-
order transition. ACKNOWLEDGEMEXTS
respec-
the difference
shows that
as the melting
eutectic.
pressures
moduli data(li-15’
are 21°C and
and 40 kbar,
of the melting eutectic
Simi-
with respect to the
after which it remains constant.
an approximately
ever, the eventual
decreases to disappear near -60
HgjTI,
suggest
curve of $Tl
curve of cr-Hg the differences
temperature
60’ is reached,
It should be noted that the elastic
of the melting
at atmospheric
extrapolation
1973
along the trigonal
will decrease
and the HgjT1.,/,3-Tl
and 369°C
exactly
?I,
respectively.
226°C
more,
to the melting
VOL.
40 kbar,
larly, for the X-Hg/Hg5Tl, melting
Considering
respect
of P-T1 itself, n-e find differences
MET_iLLCRGIC_i,
This would angle of 70.6”
until a value of
The
aut,hors
Pistorius fitting
x-ould like to thank
for witing
the data.
of t,his Institute
the computer
Thanks
apparatus
in good repair,
Martha
C.
used in
are due to Dr R. J. Murphy
for valuable
discussions.
and his staff and A. de Kleijn the manufacture
Jlrs
programs
J. Erasmus
and his staff kept the
and were responsible
of the furnace
parts.
for
Calculations
were carried out on the IBM 360/65H of the Sational Research
Institute
for Nathematical
Sciences.
REFERENCES 1. 11. HASSES and I<. ASDERKO, Co~wtitution of Bimry dllous. McGraw--Hill (19561. “. A. ~LKSDER, Z. Phys: Cheh. (Leipzig) A171, 45 (1935). 3. T. CLAIRE, R. CASTASET. H. TACHOIRE and 31. LAFITTE, BulZ. Sot. Chins. France 712 (1969). 4. F. QACERWALDand IV. TESKE, Z. ;112orq.C’hem. 210, ‘47 (1933). 5. F. SACERWALD and E. OSSWALD, Z. ilvorg. illlg. Chern_ 257, 19.5(194s). 6. R. E. SJL~LLZILSand B. R. T. FROST, dctcl Nel. 4. 611 (1956). 5. IV. KLEMEST, -1. ~J~Y.IFLU~ASancl G. C. KESSEDI., Phy;r. Rev. 131, 1 (1963). 8. P. W. RICHTER ancl C. W. F. T. PISTORK~, .?. lws-common Me~nZ.s.29, 215 (197”). 9. A. J~YAEMX~S, W. KLEMEXT, R. C. SEQTOS and G. C. KESXEDY, J. Phys. Chem. Solids. 24, 5 (1963). 10. P. S. ADLER and H. X.~GOLIS, Trm3. Jletall. Sot. d.1.M.E. 230, 1045 (1961). 11. G. J. PIERJL~ISI and C. E. WEIR, J. Rea. Snt. Bur. Sta&_ (L-S.) MA, 3% (1962). 12. G. C. KESSEDT and P. S. LAMORI, in Progress in Very High Pressure Research., eciiteclby F. P. BUSDY, W’. R. HIBBARD and H. 11. STROSC, p. 301. John Wiley (1961). 13. C. IV. F. T. PISTORICSancl J. B. CLARK, High Temp. High Press. 1, 561 (1969). 11. E. GR~XEISES ancl0. SCGELL, Ann. Phys. 19,38i (1934); Solid St. Phys. 7, “SA (19%). 15. \I-. H. ?hXLUILkSES, dcta &yet. 5, 19 (1952).