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Phase transitions in lawsonite: a calorimetric study

Abstract

The specific heat of lawsonite, \ce{CaAl2Si2O7(OH)2.H2O}, has been measured in the temperature range $[\SI{125}{\kelvin},\SI{325}{\kelvin}]$. An anomaly is seen at \SI{273}{\kelvin}, which is related to the $\mathrm{Cmcm} – \mathrm{Pmcn}$ phase transition. The magnitude of the total excess entropy associated with this transition is not reproducible, varying in the range $[\SI{5.93}{\joule\per\kelvin\per\mole},\SI{6.24}{\joule\per\kelvin\per\mole}]$. On heating, the specific heat anomaly is consistent with a tricritical phase transition. However, on cooling, significant hysteresis is observed, and the form of the $C_p$ anomaly is quite different. In all measurements extensive pre-transitional effects are observed above $T_c$. Analysis of existing specific heat data in the temperature range $[\SI{75}{\kelvin},\SI{175}{\kelvin}]$ shows an anomaly associated with the $\mathrm{Pmcn} – \mathrm{P2_1cn}$ phase transition. The excess entropy associated with this transition is \SI{6(1)}{\joule\per\kelvin\per\mole}. These data are interpreted as showing that both transitions are caused by the interaction of proton ordering and displacive changes in the aluminosilicate framework. The standard entropy of lawsonite at 298 K is recalculated, incorporating the effects of the two transitions. Two methods are used for this recalculation, giving values of $S^0_{298} = \SI{233.27}{\joule\per\kelvin\per\mole}$ and and $S^0_{298} = \SI{234.96}{\joule\per\kelvin\per\mole}$ respectively.

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Phase transitions in lawsonite: a calorimetric study

Author: Martín Olalla, José María; Hayward, Stuart A.; Meyer, Hinrich-Wilhem; Ramos Vicente, Saturio; del Cerro Gonzalez, Jaime; Carpenter, Michael A.
Publisher: E. Schweizerbart’sche Verlagsbuchhandlung
Year: 2001
DOI: 10.1127/0935-1221/01/0013-0005
Source: https://idus.us.es/bitstreams/33d29cc6-05c4-49b5-9f58-c93739921b48/download
This is he Au ho s’ accep ed manusc ip . ©2001 E. Schweize ba ’sche Ve lagsbuchhandlung. D-70176 S u ga
The Ve sion o Reco d is a ailable a Eu opean Jou nal o Minea ology 13 5–14 (2001) unde doi:10.1127/0935-1221/01/0013-0005
Phase ansi ions in lawsoni e: a calo ime ic s udy
J M Ma ´ın-Olalla,1, ∗S ua A. Haywa d,1Hin ich-Wilhem Meye ,2Sa u io Ramos,1Jaime del Ce o,1and
Michael A. Ca pen e 2
1Depa amen o de F´ısica de la Ma e ia Condensada, ICMSE-CSIC,
Uni e sidad de Se illa. Apa ado de Co eos 1065 E-41080 SEVILLA SPAIN
2Depa men o Ea h Sciences,
Uni e si y o Camb idge,
Downing S ee , Camb idge, CB2 3EQ,
Uni ed Kingdom
(Submi ed: 26 June 2002; Accep ed 12 No embe 2002; Published: 27 Decembe 2002)
The speci ic hea o lawsoni e, CaAl2Si2O7(OH)2·H2O, has been measu ed in he
empe a u e ange [125 K,325 K]. An anomaly is seen a 273 K, which is e-
la ed o he Cmcm–Pmcn phase ansi ion. The magni ude o he o al excess
en opy associa ed wi h his ansi ion is no ep oducible, a ying in he ange
[5.93 J K−1mol−1,6.24 J K−1mol−1]. On hea ing, he speci ic hea anomaly is con-
sis en wi h a ic i ical phase ansi ion. Howe e , on cooling, signi ican hys e esis
is obse ed, and he o m o he Cpanomaly is qui e di e en . In all measu emen s
ex ensi e p e- ansi ional e ec s a e obse ed abo e Tc. Analysis o exis ing speci ic
hea da a in he empe a u e ange [75 K,175 K] shows an anomaly associa ed wi h
he Pmcn–P21cn phase ansi ion. The excess en opy associa ed wi h his ansi ion
is 6(1) J K−1mol−1. These da a a e in e p e ed as showing ha bo h ansi ions a e
caused by he in e ac ion o p o on o de ing and displaci e changes in he aluminosilica e
amewo k. The s anda d en opy o lawsoni e a 298 K is ecalcula ed, inco po a ing
he e ec s o he wo ansi ions. Two me hods a e used o his ecalcula ion, gi ing
alues o S0
298 = 233.27 J K−1mol−1and and S0
298 = 234.96 J K−1mol−1 espec i ely.
I. INTRODUCTION
In oduc ion Lawsoni e, CaAl2Si2O7(OH)2·H2O, is a
common cons i uen o high-p, low-Tme amo phic ocks,
such as blueschis s. As a ela i ely dense hyd ous min-
e al, lawsoni e has equen ly been in es iga ed as p o-
iding a po en ial mechanism o ca y wa e deep in o he
Ea h’s in e io . These s udies (Cha e jee and Leis ne ,
1984; Pawley, 1994; Schmid and Poli 1994) ha e indi-
ca ed ha lawsoni e emains s able down o he p es-
su e and empe a u e condi ions o he man le. Wa e
in he lawsoni e s uc u e is signi ican o ano he ea-
son. X- ay di ac ion and in a edspec oscopy expe -
imen s (Libowi zky and A mb us e , 1995; Libowi zky
and Rossman, 1996) ha e shown ha lawsoni e unde -
goes phase ansi ions a low empe a u es, associa ed
wi h he o ien a ion o he H2O molecules and hyd oxyl
g oups wi hin he lawsoni e s uc u e. These ansi ions
a e in e es ing since hey allow he in e ac ion be ween
hyd ogen a oms and an aluminosilica e amewo k o be
s udied.
The oom- empe a u e s uc u e o lawsoni e has space
g oup Cmcm. A 273 K, he H2O molecules o a e
a ound [100], educing he symme y o Pmcn. The sec-
ond phase ansi ion, a 120 K, educes he symme y
o he s uc u e o P21cn. This ansi ion is associa ed
∗[email p o ec ed]; h ps://o cid.o g/0000-0002-3750-9113;
h ps:// o .o g/03yxnpp24
wi h a u he o a ion o he H2O molecules a ound a
di e en axis.
Two dis inc mechanisms may be en isaged o his
ansi ion. In a displaci e model o he ansi ion, hese
o a ions occu as a unc ion o empe a u e below he
ansi ion. In an o de -diso de ansi ion, he o ien-
a ion o he wa e molecules hops be ween a numbe
o almos ixed posi ions; he c ys al s uc u e obse ed
expe imen ally is hen a dynamic a e age o he a -
ious o ien a ions. Fo a pu ely o de -diso de ansi-
ion, he excess en opy o he ansi ion may be cal-
cula ed di ec ly using con igu a ional mixing models. In
a displaci e ansi ion, he excess en opy comes om
changes in phonon equencies associa ed wi h he s uc-
u al changes, which a e a he less simple o calcula e.
In o de o in es iga e hese e ec s u he , a single
sample o lawsoni e has been cha ac e ised by a numbe
o di e en me hods. The expe imen al quan i ies mea-
su ed ha e been elas ic cons an s, dielec ic cons an s,
bi e ingence, mac oscopic dila a ion (Sonde geld e al.,
2000), la ice pa ame e s and in a ed spec a (Meye
e al., 2000). In his a icle, we epo he esul s o
calo ime ic measu emen s ac oss he 273 K ansi ion,
and ela e hem o some o hese o he da a. A numbe
o o he calo ime ic s udies o lawsoni e ha e been pe -
o med (King and Welle , 1961; Pe kins e al., 1980) bu
he pu pose o hese s udies was o unde s and he s a-
bili y o lawsoni e in me amo phic eac ions. As a esul ,
he da a close o he ansi ions a e a he scan y.
Typese by REVT
EX
2
II. EXPERIMENTAL METHODS
A. Sample desc ip ion
The lawsoni e sample used in his s udy came om
Valley Fo d, Sonoma Coun y, Cali o nia, and is no.
120943 o he Ha a d Uni e si y mine al collec ion. This
sample was gene ously p o ided by D . C. F ancis (Ha -
a d Uni e si y, USA). In handspecimen, he sample con-
ained a ein se e al cm wide consis ing p edominan ly
o in e locking lawsoni e g ains, along wi h a small p o-
po ion o calci e. A small disc app oxima ely 10 mm in
diame e and 3.9 mm hick was cu om his ein o he
calo ime ic measu emen s. The mass o his sample was
0.9 g.
A e he calo ime ic measu emen s we e comple ed
he disc was cu in o ci cula slices and moun ed as hin
sec ions. Poin coun ing o hese sec ions in a pe o-
g aphic mic oscope ga e he olume ac ions o law-
soni e and calci e as 97.95 % and 2.05 % espec i ely.
Elec on-mic op obe analysis (EDS) showed he majo
ca ion elemen s in lawsoni e o be Ca, Al, Fe, and Si only.
Analyses o Ti, C , Mn, Ni, Mg, Na, K, Cl, P and S we e
also ca ied ou , bu hese elemen s we e only p esen a
le els less han 1σon coun ing s a is ics. Wa e con en
o his ma e ial was de e mined using he mog a ime y
(S. Ma ion, pe s. comm.); wi hin expe imen al e o he
sample is ully hyd a ed.
P e ious analyses (Dee e al. 1992, and e e ences
he ein) indica e ha he wa e con en does no a y
subs an ially be ween na u al lawsoni es; he quo ed
wa e con en s a e in he ange 10.61 o 11.70 (w
%). Using he a e age o ou p obe analyses, he
composi ion o he lawsoni e phase in his sample is
Ca1.00Al1.95Fe0.05Si2.00O7(OH)2·H2O.
B. Calo ime ic expe imen s
The sample was placed in a conduc ion calo ime e o
a ype desc ibed p e iously (del Ce o, 1987; del Ce o e
al., 1987). The calo ime e consis s o a la ge block o alu-
minium, which ac s as a he mal ese oi . Two luxme-
e s, each consis ing o 48 he mocouples, a e placed elec-
ically in se ies and he mally in pa allel. The ou e
junc ion o each luxme e is ixed o he calo ime ic
block, and he sample is p essed be ween he inne junc-
ions. The con ac s be ween he luxme e s and he sam-
ple a e sil e pla es, o ensu e good he mal con ac and
homogenisa ion. The en i e assembly is e acua ed o
10−5mba , and placed in an alcohol ba h. This ba h
may be cooled om oom empe a u e o liquid-ni ogen
empe a u e. The sample empe a u e may be adjus ed
by hea ing o cooling he alcohol ba h. By cooling he
sys em slowly, equilib ium may be main ained be ween
he sample and he hea ba h.
FIG. 1 Expe imen al measu emen s o speci ic hea as a unc-
ion o empe a u e in lawsoni e. Pa a) shows he da a
o e he whole empe a u e ange o he expe imen s, and
pa b) is a magni ca ion o he da a in he icini y o he
Cmcm–Pmcn ansi ion. The ou solid lines show he da a
o he wo hea ing and wo cooling uns pe o med in his
s udy, and he ci cles show he da a ob ained by Pe kins e
al. (1980) o hea ing a di e en lawsoni e sample.
The Cpmeasu emen s a e pe o med using a small
hea e a ached o he luxme e s. The sample is hea ed
un il a s eady s a e is a ained, a which poin he hea e
powe is cu o . The elaxa ion o he sample back o
equilib ium wi h he hea sink depends on he hea capac-
i y o he sample, and so CP may be measu ed as a unc-
ion o empe a u e. In his expe imen , ou measu e-
men uns we e ca ied ou . The sample was quenched
om oom empe a u e o 125 K. Measu emen s o he
speci ic hea we e ca ied ou as he sample was hea ed
slowly (ca. 0.6 K h−1) o 320 K ( un 1). Fo he second
un, he sample was cooled a he same a e o 200 K.
The sample was hen hea ed back o oom empe a u e,
again a he same a e ( un 3). Finally, he sample was
cooled o 260 K, again a he same empe a u e a e ( un
4). In each case, he e was a minimal ime in e al be-
ween he a ious measu emen uns.
3
III. EXPERIMENTAL RESULTS FOR THE Cmcm −Pmcn
TRANSITION
A. Speci ic hea as a unci on o empe a u e
Fig. 1 shows he speci ic hea as a unc ion o em-
pe a u e o each o he ou expe imen al uns. These
da a a e no co ec ed o he sample pu i y. The da a
o Pe kins e al. (1980), which we e measu ed using a
di e en 95 % pu e lawsoni e sample om Valley Fo d,
Cali o nia, a e also shown o compa ison.
Examina ion o he da a close o Tc(Fig. 1b) indica es
ha he speci ic hea anomaly in lawsoni e has wo pa s.
The e is a dis inc change in he Cp(T) slope a ca. 295 K,
which is e idence o a p onounced ail in he hea capac-
i y anomaly abo e Tc. Simila e ec s ha e been seen in
o he ypes o expe imen s; Sonde geld e al. (2000) no e
p e- ansi ional e ec s in bi e ingence measu emen s up
o ∼200 K abo e he ansi ion empe a u e. The ail
is qui e ep oducible be ween he di e en expe imen al
uns, o bo h hea ing and cooling he sample.
A he ansi ion empe a u e, a dis inc peak is ex-
pec ed, bu he magni ude o his peak a ies g ea ly
be ween he expe imen al uns. In pa icula , he peak
is a mo e p onounced when he sample is being hea ed
han when i is cooled.
B. Excess en opy calcula ions
Analyses o bi e ingence, dielec ic cons an , elas ic
cons an and co-elas ic spon aneous s ain da a (Son-
de geld e al., 2000), as well as in a ed spec oscopic
da a (Meye e al., 2000) a e consis en wi h a Landau
model o he Cmcm–Pmcn ansi ion, whe e he ansi-
ion is close o he ic i ical poin . Addi ional accoun
mus be aken o he ails seen abo e Tc. Calcula ion
o he excess en opy as a unc ion o empe a u e p o-
ides a u he es o his model. In addi ion, we may
compa e he o al excess en opy wi h he en opy p e-
dic ed o a dipole o de -diso de p ocess. In o de o
eliably calcula e excess quan i ies associa ed wi h he
phase ansi ion, i is necessa y o know accu a ely he
“baseline” beha iou o he expe imen al da a ( ha is,
in he absence o he phase ansi ion). This issue is pa -
icula ly p oblema ic o calcula ions o excess en opy
om Cpda a. Well below Tc, he speci ic hea anomaly
is small, and so e en small e o s in he baseline spe-
ci ic hea may ha e a la ge sys ema ic e ec on he inal
en opy calcula ion.
Fo his s udy, we ha e he e o e used a wos age p o-
cess o de e mine he excess en opy associa ed wi h he
ansi ion. Fi s , we ha e used a simple in e pola ion
me hod o gene a e a “p elimina y” baseline. Because
his p elimina y baseline is well-ancho ed by expe imen-
al da a om jus abo e he ansi ion empe a u e, i
FIG. 2 Tempe a u e dependence o (T/∆Cp)2 o lawsoni e.
Fo a ansi ion obeying Landau heo y, his unc ion is ex-
pec ed o be linea . The de ia ions om linea i y a low em-
pe a u e a e likely o be due o small e o s in he p edic ion
o he baseline Cp0.
is expec ed o be easonably accu a e immedia ely be-
low he ansi ion empe a a u e. In any case, he la ge-
ness o ∆Cpnea Tcmeans ha he unce ain ies in he
baseline a e p opo iona ely less signi ican he e han a
low empe a u es. We hen use a heo e ical model o
he ansi ion (pa ame e ised by hese ini ial esul s), o
de e mine he beha iou o ∆Cpa lowe empe a u es.
F om his, we de e mine a “back-calcula ed” Cpbaseline,
whose o m may be in o mally checked o i s plausibil-
i y. The excess en opy is hen calcula ed wi h espec
o his back-calcula ed baseline.
I can be shown (see, o example, Salje, 1990) ha ,
o any phase ansi ion desc ibed by a s anda d 2:4.6
Landau po en ial, whe he i s o de o second o de ,
he speci ic hea anomaly may be linea ised as
T
∆Cp2
∝(T–T2),(1)
whe e he di e ence be ween Tcand T2is a measu e o
he closeness o he ansi ion o he ic i ical poin ;
o a ansi ion which is s ic ly Landau ic i ical (i.e.
∆S∝Q2;Q∝ |Tc−T|1/4), Tcand T2a e equal. In
any case, we may es he alidi y o Equa ion (1) close
o Tcusing he p elimina y baseline. I his p o es o
be easonable, Equa ion (1) hen de ines he beha iou
o ∆Cpa lowe empe a u es, whe e he de e mina ion
o he baseline is mo e p oblema ic. A p elimina y em-
pi ical baseline Cp0was easily de e mined by i ing a
pa abola hough he da a o he i s expe imen al un
o T > 315 K and T < 150 K. Since ∆Cpis expec ed o
be non-ze o a low empe a u es, his p elimina y base-
line is no o ally co ec . The e o will be mos sig-
ni ican a lowe empe a u es, whe e he ue alue o
∆Cpwill be sys ema ically la ge han we ob ain wi h
he p elimina y baseline. The main consequence will be
4
FIG. 3 Tempe a u e dependence o excess en opy in law-
soni e. Abo e 260 K (solid line), his cu e is calcula ed by
simple in eg a ion o (∆Cp/T). Below 260 K (b oken line), i
is assumed ha he linea i y o (T/∆Cp)2seen in Fig. 2 may
be ex apola ed.
ha he o al excess en opy o he ansi ion will be
unde es ima ed. Howe e , he e o close o Tcwill be
smalle and we can use he p elimina y baseline o s udy
he beha iou o ∆Cpin he icin iy o Tc. Fig. 2 shows
he dependence o (T/∆Cp)2on empe a u e o he i s
hea ing cycle ( his being he expe imen whe e he peak
in ∆Cpwas mos p onounced). The igu e clea ly shows
he linea beha iou close o he ansi ion poin and he
in e cep ion o he s aigh line wi h empe a u e axis
gi e us T2= 275.3(1) K. The la ges alue o ∆Cpis ob-
se ed a T= 272.8(4) K. The posi ion o he ∆Cppeak
p o ides one de ini ion o Tc, albei a somewha p oblem-
a ic one in a ansi ion wi h a signi ican ∆Cp ail abo e
he ansi ion empe a u e. I is clea , howe e , ha he
ansi ion is e y close o he Landau ic i ical poin .
This p elimina y baseline may hen be imp o ed by
aking accoun o Fig. 2. I we assume ha he obse ed
linea i y should con inue o lowe empe a u es, we may
calcula e he expec ed alue o ∆Cpa any empe a u e.
This, in conjunc ion wi h he expe imen al da a Cp(T)
allows he baseline o be calcula ed om Cp0=Cp–∆Cp.
The b oken line in Fig. 1 shows he esul ing baseline, a -
e he back-calcula ed Cp0(T) has been smoo hed. Close
o he ansi ion empe a u e, he p elimina y and back-
calcula ed baselines ag ee well. A lowe empe a u es,
he back-calcula ed baseline is lowe han he p elimina y
baseline, bu i is mo e ealis ic as i akes accoun o he
small (bu non-ze o) ∆Cpexpec ed o any heo y o he
ansi ion.
Gi en he empe a u e dependence o Cpand Cp0, he
o al excess en opy as a unc ion o empe a u e is cal-
cula ed in Fig. 3. In Fig. 3, he con e sion om mass
uni s o mola uni s includes a co ec ion o he calci e
impu i ies in he expe imen al sample. Fo he pu poses
o his calcula ion, i has been assumed ha he linea
FIG. 4 Tempe a u e dependence o excess en opy o wo
hea ing and wo cooling uns in lawsoni e.
beha iou o (T/∆Cp)2may be ex apola ed o 0 K. Two
a gumen s indica e ha his is no wholly ealis ic.
Fi s ly, i akes no accoun o he endency o he o -
de pa ame e o app oach a cons an alue a absolu e
ze o (Salje e al., 1991). Secondly, i igno es he e ec o
he phase ansi ion a 120 K. The classical ex apola ion
is s ill use ul, howe e , since i p o ides he bes es ima e
o ∆Sbe ween he high- empe a u e phase and he s uc-
u e a ze o kel in. As shown in Fig. 3, he ex apola ed
alue o ∆Sa absolu e ze o is 5.93(1) J K−1mol−1.
The andom e o in his quan i y is small (i depends
only on he e o in he g adien o he s aigh line i
in Fig. 2, which is o he o de o 1 %). The sys ema ic
e o s, due o he wo ac o s gi en abo e, a e p obably
la ge , bu di icul o quan i y.
C. Analysis o subsequen expe imen al uns
Fig. 4 shows he empe a u e dependence o he ex-
cess en opy o all ou expe imen al uns pe o med in
his s udy. The wo hea ing expe imen s show e y sim-
ila , almos ic i ical beha iou ; he e ec o he di e -
ence in he heigh be ween he wo ∆Cppeaks is a he
small. I he excess en opy in he second hea ing ex-
pe imen ( un 3) is ex apola ed o 0 K, he esul ing
∆S= 6.24(1) J K−1mol−1. This esul may simply be
an a e ac o he i ing me hod used; he low empe -
a u e ∆Cp alues a e sligh ly highe o un 3 han o
un 1. Fi ing bo h da a se s o a single baseline has a
signi ican e ec o he inal calcula ion o en opy.
Howe e , compa ison be ween he wo hea ing cu es
and he wo cooling cu es (which a e e y simila o
each o he ) indica es a signi ican deg ee o hys e esis in
he ansi ion. The o m o he cooling cu es is no
consis en wi h ic i ical beha iou , and he magni udes
o ∆Sa e also inconsis en .
5
FIG. 5 Tempe a u e dependence o en opy (solid line) and
co-elas ic spon aneous s ains a) e1 and b) e2 (solid poin s)
in lawsoni e. The b oken line shows he beha iou expec ed
o bo h hese quan i ies o s ic ic i ical beha iou (Q4∝
|Tc−T|). The empe a u e scales in he wo expe imen s ha e
been adjus ed such ha he ansi ion empe a u e Tcis he
same in each case.
D. Compa isons wi h o he expe imen al da a
Fig. 5a and 5b compa e he empe a u e dependence o
he en opy obse ed in un 1 wi h measu emen s o he
co-elas ic spon aneous s ain (Meye e al., 2000). In o -
de o compa e he a ious da a, i was necessa y o add
a cons an o se o all he empe a u es o he spon a-
neous s ain da a. This may be due o di e en empe -
a u e calib a ions in sepa a e appa a us. This cons an
was ixed by de e mining he empe a u e a which linea
ex apola ions o bo h (∆S)2and e2
i(bo h o which a e
p opo ional o Q4) wen o ze o.
Fa om Tc, he expec ed Landau ela ionship (∆S∝
ei∝Q2) is obeyed o all h ee componen s o he s ain
enso . Howe e , e1 de ia es om his ela ionship o e a
ange o ca. 20 K below Tc. The mos p obable eason o
his is ha he simple ela ionship be ween sho - ange
o de and long- ange o de is no applicable o small
FIG. 6 Speci ic hea da a o lawsoni e in he icini y o he
Pmcn −P21cn ansi ion, aken om Pe kins e al. (1980).
The da a shows a s ep anomaly, consis en wi h a second o de
phase ansi ion.
deg ees o long- ange o de . F om Fig. 5, i is appa -
en ha e1 is a he mo e sensi i e o sho ange o de
han e2. The ail in e1 abo e Tcis signi ican ly mo e
p onounced, and co ela es well wi h he en opy in his
empe a u e ange (which, since he long- ange o de pa-
ame e is ze o, mus be om sho - ange o de ).
E. Reanalysis o he Pe kins e al. (1980) da a o he
Pmcn–P21cn ansi ion
P e ious calo ime ic s udies o lawsoni e (King and
Welle 1961; Pe kins e al., 1980) no ed wo anomalies
in he Cp(T) cu e. As we ha e shown abo e, he e is a
good co ela ion be ween he lambda peak a 273 K and
o he da a o a phase ansi ion a his empe a u e.
The empe a u e o he second anomaly no ed by Pe kins
e al. (1980) is app oxima ely 130 K. This is close o he
empe a u e o he Pmcn–P21cn ansi ion, de e mined
as 120 K by Sonde geld e al. (2000).
Fig. 6 shows he da a o Pe kins e al. (1980) in he
icini y o his ansi ion. The ansi ion shows limi ing
second-o de beha iou (based on X- ay di ac ion mea-
su emen s, Sonde geld pe s. comm.); he expec ed o m
o he Cpanomaly in his case is a s ep, a he han a
lambda peak. F om Fig. 6, he magni ude o his s ep a
he ansi ion empe a u e is 6(1) J K−1mol−1. Thus he
es ima ed ∆S o he Pmcn–P21cn ansi ion a comple-
ion is 6(1) J K−1mol−1.

6
IV. DISCUSSION
A. Implica ions o s anda d en opy calcula ions
In his s udy, we ha e shown ha he anomalies in
he speci ic hea cu e o lawsoni e a e associa ed wi h
wo phase ansi ions unde gone by his mine al. They
a e hus an in insic pa o he beha iou o lawsoni e,
and hei e ec should be included in calcula ions o he
s anda d en opy a 298 K, S0
298. I was no possible o
simply in eg a e ei he o he exis ing da a se s o de-
e mine S0
298; he da a o Pe kins e al. (1980) do no
con ain su icien poin s close o he 275 K ansi ion o
p ope ly cha ac e ise he peak, whe eas ou expe imen
did no measu e Cpbelow 125 K. We used wo me hods
o deal wi h his di icul y; i s , combining he da a om
he wo expe imen s, and second, using ou knowledge o
he cha ac e o he ansi ion o p oduce an in e po-
la ion h ough he Cpda a measu ed by Pe kins e al.
(1980).
Ou Cpda a ag ee well wi h hose o Pe kins e
al. (1980) in he empe a u e ange [140 K,180 K] (e.g.
Fig. 1(a)), and so we used ou da a in he empe a u e
ange [160 K,298 K], and he da a o Pe kins e al. (1980)
in he ange [0 K,160 K]. Nume ical in eg a ion o hese
da a ga e a alue o S0
298 = 233.27(1) J K−1mol−1. The
disad an age o his me hod is ha i is no clea ha
he wo da a se ies may be combined in his way; di e -
en samples we e used o he wo expe imen s, and he
Cppeak is appa en ly highe in he Pe kins e al. (1980)
sample han in he one used in his s udy (Fig. 1(b)).
We he e o e also i ed he Cpda a o Pe kins e al.
(1980) o a lambda peak cha ac e is ic o a Landau i-
c i ical phase ansi ion. This was done by he same
me hod used abo e, and he esul ing in e pola ion is
shown in Fig. 7.
In eg a ion o he cu e in Fig. 7 leads o a alue o he
s anda d en opy, S0298 = 234.96(1) JK-1mol-1. Bo h
me hods o calcula ion lead o a highe alue o S0298
han p e iously published (S0298 = 230.19 JK-1mol-1,
Pe kins e al., 1980).
B. Signi icance o he magni ude o he excess en opy
Bo h obse ed phase ansi ions in lawsoni e a e as-
socia ed wi h appa en o a ion o he H2O molecules
b eaking a symme y plane; he (001) plane a ca. 275 K,
and (100) a 120 K. As a esul , each H si e in he
Cmcm s uc u e becomes wo si es in he Pmcn s uc-
u e, each o which unde goes a u he wo old spli ing
in he P21cn s uc u e. The e is e idence om neu on
di ac ion s udies (Lage e al., 1998) o u he H-si e
spli ing a low empe a u es, bu his is no di ec ly im-
plica ed in he phase ansi ions.
The excess en opy associa ed wi h bo h o he phase
FIG. 7 Speci ic hea da a o lawsoni e, de e mined by
Pe kins e al. (1980), wi h an in e pola ion (solid line) con-
sis en wi h a Landau ic i ical phase ansi ion.
ansi ions has wo main possible sou ces. The i s is he
con igu a ional en opy associa ed wi h mixing he wo
possible s uc u al con igu a ions as wo dis inc si es in
he high- empe a u e phase become indis inguishable in
he low empe a u e phase. In a simple B agg-Williams
model o hese wo phase ansi ions, we would expec he
excess en opy associa ed wi h each ansi ion o be solely
he con igu a ional en opy, which would imply ∆S=
5.76 J K−1mol−1 o each ansi ion.
A con ibu ion o he en opy may also come om he
e ec o he spon aneous s ain on he phonon equen-
cies. This excess ib a ional en opy is expec ed o scale
as he squa e o he o de pa ame e , bu i is no i -
ial o calcula e i s magni ude. I is also unclea how
much ib a ional en opy is equi ed o d i e a ansi ion
om con igu a ional beha iou (e.g., B agg-Williams) o
he Landau limi . In he case o albi e, he excess o
he expe imen ally es ima ed en opy o e he calcula ed
con igu a ional en opy is only abou 10 % (Ca pen e ,
1988), and his appea s o be su icien .
In bo h ansi ions, he obse ed excess en opy is ap-
p oxima ely 6 J K−1mol−1. Thus he measu ed en opy
in lawsoni e is no inconsis en wi h a model o he an-
si ions whe e dipole o de ing is modi ied by s ain e ec s.
C. Hy e esis in calo ime ic measu emen s
The e is a signi ican deg ee o hys e esis in he calo i-
me ic measu emen s o his phase ansi ion, which is
no obse ed in o he expe imen s. One signi ican ac-
o is ha he measu emen s o quan i ies such as he
spon aneous s ain depend on bo h he o ien a ional o -
de ing o H2O molecules, and he esponse o he es
o he s uc u e o his o de ing. The absence o o -
de on he leng h scale o he amewo k esponse may
well mask signi ican sho - ange o de . One o he bes -
7
FIG. 8 Tempe a u e dependence o speci ic hea in lawsoni e,
compa ed wi h a Landau model. Poin s show expe imen al
da a ( i s hea ing un), he solid line is a Landau i , and he
b oken line shows he baseline unc ion Cp0.
documen ed examples o his is he s udy o co die i e
by Pu nis e al. (1987), in which NMR measu emen s o
(Al, Si) o de ing we e compa ed wi h spon aneous s ain
da a. In co die i e, he expec ed ela ionship be ween he
s ain and he deg ee o o de (Q∝ε) was only ound o
Q > 0.9; less wello de ed samples showed no mac oscopic
s ain. The e a e some pa allels be ween his beha iou
and he obse a ion ha he s ain componen s e1and
e2in lawsoni e beha e somewha di e en ly o small de-
g ees o long- ange o de .
The applica ion o his concep o he Cphys e e-
sis in lawsoni e may be seen by s a ing wi h a ully
o de ed s uc u e. On hea ing, he deg ee o o ien a-
ional o de dec eases, and he emainde o he s uc u e
elaxes owa ds he high- empe a u e s uc u e. The
ag eemen be ween he calo ime ic da a and he spon-
aneous s ains implies ha his p ocess is essen ially ho-
mogeneous.
On cooling, howe e , he si ua ion appea s o be di -
e en . The elaxa ion o he s uc u e is e e sible, bu
he speci ic hea measu emen s indica e ha he en opy
does no scale wi h Q2 in he expec ed way. This im-
plies ha he local aspec o he ansi ion ( he H2O
o ien a ional o de ing) is no pe ec ly coupled wi h he
long ange displaci e changes in he lawsoni e s uc u e
o small deg ees o o de . Fu he expe imen s o s udy
his hys e esis a e planned.
D. Anomalies close o Tc
As Fig. 2 shows, he hea capaci y anomaly de ia es
om he p edic ions o Landau heo y some 2 K o 3 K
below he ansi ion empe a u e. Fig. 8 shows he same
e ec o he ac ual anomaly, a he han he linea ised
unc ion in Equa ion (1).
Fig. 8 emphasises ha he e a e wo de ia ions om
he Landau model; immedia ely below Tc, he expe i-
men al Cpda a a e lowe han Landau heo y p edic s,
and abo e Tc, he Cpda a a e highe han he model.
The con ibu ions o hese wo e ms o he excess en-
opy associa ed wi h he ansi ion e y nea ly cancel
each o he ou .
E. H o de ing as a ic i ical Landau p ocess
Calo ime ic da a o he ansi ion a e consis en
wi h o he expe imen al da a in indica ing ha he
Cmcm–Pmcn ansi ion in lawsoni e ollows a Landau
model, close o he ic i ical poin . The excess en opy
associa ed wi h he ansi ion appea s o be somewha
a iable, which may indica e ha he ei he o bo h he
deg ee o dipole o de a low empe a u es, and diso de
a high empe a u es, a e incomple e. In any case, he
∆S o he ansi ion is sligh ly highe han we would
p edic o a simple o de -diso de model.
Quali a i ely simila esul s ha e been ob ained o
o de -diso de ansi ions in a numbe o mine al sys-
ems, including omphaci e (C2/c −P2/n, Ca pen e e
al., 1990), calci e (R3m–R3c, Red e n e al., 1989), and
albi e (C2/m −C1, Salje e al., 1985). As no ed abo e,
he ac ha he he modynamics o hese ansi ions ap-
pea o ollow a Landau model o he en opy, a he han
a con igu a ional model, is ela ed o he ole o he i-
b a ional en opy and i s dependence on he spon aneous
s ain.
ACKNOWLEDGMENTS
We would like o hank D . C. F ancis (Ha a d Uni-
e si y, USA) o he lawsoni e sample used in his s udy,
and D . S. Ma ion (Cen e o Ma e ials Science, Uni-
e si y o Oslo) o he mog a ime ic da a o his law-
soni e sample. We a e g a e ul o P o . A. Na o sky
and wo o he e iewe s o hei help ul commen s on
his manusc ip . This p ojec is suppo ed by he EU
TMR Ne wo k “Mine al T ans o ma ions” (ERBFMRX-
CT97-0108).
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