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Submitted on 1 Jan 1988
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Analysis of the absorption and emission spectra of U4+
in α-ThBr 4
E. Simoni, S. Hubert, M. Genet
To cite this version:
1425
Analysis
of the
absorption
and
emission
spectra
of
U4+ in 03B1-ThBr4
E.
Simoni,
S. Hubert and M. GenetInstitut de
Physique
Nucléaire,
Laboratoire de Radiochimie, 91406Orsay,
France(Requ
le 3 dgcembre 1987,accepté
le 13 avril1988)
Résumé. 2014 La forme basse
température 03B1-ThBr4
a une structure de type scheeliteI41/a
danslaquelle
l’uranium tétravalent se substitue au thorium(symétrie
de siteS4).
En faisantl’hypothèse
que l’état fondamental est03934
comme dans la forme03B2-ThBr4,
les spectresd’absorption
polarisés
à 4,2 K montrent queD2d
est une bonneapproximation.
Cette matrice a laparticularité
d’exalter de très nombreuses fluorescences deU4+,
cequi
permet d’indexer quatre niveaux Stark de l’état fondamental3H4 : 03935
à 110cm-1,
03931 à
473cm-1,
03931 à
623cm-1
et
03935 à
830cm-1.
30 niveaux ont été indexés et lesparamètres
dechamp
cristallins deU4+
(5f2)
ont été calculés dansl’approximation D2d:
B20
= - 382,
B40
= - 3262,
B44
=1 734,
B60
= - 851 etB64
= - 1828cm-1.
Il est intéressant de montrerqu’une légère
distorsion dans lastructure scheelite
03B1-ThBr4
comparée
avec la structure zircone03B2-ThBr4
induit unchangement
important
surles
paramètres
dechamp
cristallin.Abstract. 2014 The low temperature form
03B1-ThBr4
has a scheelite structureI41/a
in which the tetravalent uraniumoccupies
the thorium site which isS4. Assuming
that theground
state remains03934
as in the03B2-ThBr4
form, thepolarized absorption
spectrum at 4.2 K shows thatD2d
is agood approximation.
Apeculiarity
of this host is the exaltation of very numerous fluorescences ofU4+
whichpermit
toassign
four Stark levels of theground
state3H4 :
03935
at 110cm-1,
03931
at 473cm-1,
03931
at 623cm-1
and03935
at830
cm-1.
30 levels have beenassigned
and thecrystal
field parametersof U4+
(5f2)
have been calculated in theD2d
approximation :
B20 = -
382,B40 = -
3 262,B44 = - 1734,
B60
= - 851 andB64 = - 1828
cm-1.
It isinteresting
to note that a small distortion in the scheelite structure of the03B1-ThBr4
compared
with the zirconstructure
03B2-ThBr4
inducesimportant
changes
in thecrystal
field parameters.J.
Phys.
France 49(1988)
1425-1434 AOÚT 1988,Classification
Physics
Abstracts 71.70C - 78.60t
1. Introduction.
Thorium tetrahalides
(X
=Cl,
Br)
possess numerousproperties
which make them attractive candidatesfor
chemical,
physical
andspectroscopic
studies.Thorium tetrabromide and thorium tetrachloride
have two
polymorphic
forms[1]
with a transform-ationtemperature
of 426 °C for the former and405 °C for the latter
[2-3].
Thehigh
temperature
formJ3 - ThBr4 isomorphous
toJ3 - ThCl4
ischarac-terized
by
thetetragonal
zircon structure(space
group
14,/amd)
[4]
andundergoes
aphase
transition at 90 K[5]
with an incommensurate modulatedstruc-ture below this
temperature
[6].
The lowtempera-ture form
a-ThBr4
isomorphous
toa-ThCl4
has thescheelite structure
(space
group141/a)
[1].
From
previous
investigations
of the solid state chemicalproperties
of structuraltype
[7],
thoriumhas a
D2d
sitesymmetry
in the/3-form
of zirconstructure, and
S4
sitesymmetry
in the a-form ofscheelite structure
type.
Large
single
crystals
of pureand
doped Ï3-ThBr4
may be growneasily by
theBridgman
method[8],
while the a-form isrelatively
difficult to prepare as a
single
crystal
since the final form obtainedby
this way is the¡3-form.
Additional studies of pure8 -TbBr4
have included X ray[9],
neutron diffraction[6],
Ramaninvestigations [5]
andcomplete analysis
ofcrystal
fieldparameters
onU4 +,
Pa 4+,
pr3 +
diluted in the incommensuratemodulated
phase
[10,
11,
12]
ofJ3-ThBr4.
On the other hand
only
structural studies have beenreported
on the a-form of thorium tetrahalides[1,
2, 3,
7].
Recently
nuclearquadrupole
resonanceinvestigations
of Br-[13]
have shown thata-ThBr4 keeps
the same structure from roomtempera-ture down to 10 K and Raman
scattering
[14]
hasconfirmed this result.
Some
spectroscopic properties
of trivalent rareearth ions in
crystals
with a scheelite structure have beenalready reported
and the main interest incrystals
likeLiYF4,
PbMo04
andCaW04 [15, 16]
lies in theirproperties
for laser materials. However these host materials are not the best candidates tostudy
thespectroscopic properties
of tetravalentactinides in the scheelite structure.
Only
tetravalentneptunium
has been studied inPbMo04,
and for the first time fluorescence has been observed[17,
18].
Like scheelite structure
materials,
these purecrystals
exhibit
good
fluorescence when excitedby
U.V.radiation in the blue for
13-ThBr4
(zircon structure)
[19]
and red fora -ThBr4
(scheelite structure) [20].
Thusa -ThBr4
was chosen as a host material forspectroscopic
properties
of tetravalent uranium be-cause it has the same structure and similar chemical andoptical
behaviour as the better knownscheelite-structure
tungstates
andmolybdates.
On the other hand it isinteresting
to compare thespectroscopic
properties
ofU4 I
between8-ThBr4
which has anincommensurate structure below 90 K with multisite
continuum
going
fromD2d
toD2 [10]
anda-ThBr4
which hasonly
oneS4
site.In the
present
study, optical
absorption
andemis-sion,
Zeeman effect studies have beenperformed.
Some fluorescence ofU4 +
hasalready
beenreported
in 8 -ThBr4
[21], f3-ThCI4 [22]
andCs2ZrBr6 [23],
however ina -ThBr4,
numerous and verystrong
fluorescence lines fromU4 +
in thevisible,
as well as in the near infrared and infrared have been observed for the first time. The data have allowed reasonable energy levelassignments.
Parametersdescribing
spin
orbitcoupling
andcrystal
field interactions wereadjusted using
a least squares minimizationpro-cedure in the
D2d point
groupapproximation.
The
calculations were made
using
a fulldiagonalization
of the Hamiltonian matrix in the(LSJJz)
represen-tation. Goodagreement
was obtained between theobserved and the calculated
energies
inspite
of theD2d
approximation,
as hasalready
beenreported
in several papersconcerning
the scheelite structure materials[15,
24,
25].
2.
Experimental procedure.
The a
phase
ofdoped
ThBr4
wassynthetized
by
twotechniques.
Polycrystalline
materials could beeasily
obtained
by
heating
U4+
doped
f3-ThBr4 single
crystals
orpowder
at 400 °Cduring
one week. In any cases the final form waspolycrystalline.
On the otherhand,
only
one green coloredsingle
crystal
ofa -ThBr4 doped
with about 25 ppm ofU4 +
has beenobtained
by
theBridgman
method with the sameconditions as for the
/3-form
[8].
Thissingle crystal
waslarge enough
to obtain linearpolarization
of theabsorption
spectra
in the directionsperpendicular
and
parallel
to thecrystal
axes.All the
samples
used forspectroscopic
studies wereanalysed using
X raypowder
diffraction. In all the cases the X raypatterns
showed a pure «phase.
Samples
werehygroscopic
and less stable than thephase
and were handled in an argonatmosphere
glove
box and enclosed in a silica tube under helium pressure.The
absorption
and emissionspectra
in the visible and infrared were measured with thecrystal
excitedby
the fulllight
emissionproduced by
a 100 W iodinelamp
andusing
ahigh
resolution JOBIN YVON HR 1000spectrometer
(with
areciprocal dispersion
of about 8A/mm)
at differenttemperatures
ranging
from 4.2 K up to 300 K. Fordetection,
a Hamamatsu R374photomultiplier
was used in the visibleregion
and a PbSphotodiode
was used in the infraredregion.
In the latter case theoptical
source waschopped
and the detectorsignal
measuredby
a PAR Model 186 A lock inamplifier.
Thewavelength
readouts of thespectrometer
were calibratedusing
various lines of the first and second order ofHg
emission lines.
Samples
were introduced in a variabletemperature
optical
Dewar(Oxford Instrument) operating
be-tween 4.2 and 295 K. A
temperature
controller was used to set thetemperature.
Laser excited fluorescence measurements were
performed using
apulsed Sopra
tunabledye
laserpumped
with aSopra nitrogen
laser.Using
asuperconducting
magnet,
Zeemansplit-tings
were recorded in the visible at 4.2 K with thecrystal
in amagnetic
field of 6 T.3.
Theory
andsymmetry
considerations.The
Th4 +
ions in«-ThBr4
which are substituted forby U4 +
haveS4 point
symmetry
as in the well known scheelite structure.An
analysis
of thecrystal
fieldparameters
for the rare earth ions in scheelite calculated inD2d
and’S4
symmetry
[15, 16]
shows thattaking S4
symmetry
asD2d
is a reasonableapproximation.
For this new host matrix we will showby
selection rules in bothsymmetries
thatD2d
is agood
approximation.
In theD2d
symmetry
all thecrystal
fieldparameters
arereal,
whereas in theS4
symmetry,
the loss ofsymmetry
elements results in the introduction ofimaginary
terms in the Hamiltonian :imB1
andi mB4.
Assuming D2d
forS4
symmetry
amounts toneglect
of both the
imaginary crystal
fieldparameters.
The energy levels will be fittedby
simultaneousdiagonali-zation of the free ion and
crystal
field HamiltonianHFI’ H CF
as described below.1427
The
Fk
and’Sf
represent
respectively
the radialparts
of the electrostatic andspin
orbit interactionbetween 5f
electrons,
a,{3,
y are theparameters
associated with thetwo-body
effectiveoperators
ofconfiguration
interaction. TheMk
andP k
parameters
represent
thespin-spin
andspin
other orbit interac-tions.The classification of the
experimental
energy levels was madeby analysing
thepolarisation
data.According
to the transformationproperties
of the electricdipole
operator,
identical axial and apolarized
spectra
require
the use of electricdipole
selection rules while identical axial and 7Tpolarized
spectra
require
the use ofmagnetic dipole
selectionrules. Since axial
spectra
could not berecorded,
we assumed that electricdipole
transitionspredominate
as forU4 +
in/3-ThBr4
[21], 13-ThC14 [22]
andThSi04 [27].
In
examining
thespectra,
we will consider selec-tion rules forD2d point
symmetry
(S4
is asubgroup
ofD2a)
as it has been made in the scheelite structure for the rare earth. IfU4 +
ion is in aD2d
symmetry
site,
thecrystal
field states are eithersinglet
(T1,
r2, F3, F4)
or doublets(T5)
and certain transitions would be forbidden as shown in table I. Thecorre-sponding
identifications of theD2d
levels inS4
notation are listed in table II.Table I. - Electric
dipole
selection rules inS4
andD2d.
Table II.
- Identi fication of
the irreductiblerepre-sentations
of
theD2d point
group inS4
notation.When the local site
symmetry
isperturbed by
a lowersymmetry
environment such asS4,
some of theforbiddenness should be lifted like
F4 ->
T 2
tran-sition in the
D2d
representation
(t2 -> ri
transition inS4
representation).
4.
Experimental
results andanalysis
of thespectra.
Figures
1 show theabsorption
and emissionspectra
of tetravalent uranium in thevisible,
near infrared and infrared range at 4.2 K. The u and 7Tpolari-zations were obtained for the
strongest
lines since it was recorded withsingle crystal doped
withonly
25 ppm of
U4 + .
Unfortunately
we did not observepolarization
on the emission lines.This is the first time that so many intense
fluor-escence lines are observed.. We note that in the
a-form,
the lines aresharp
(5-15
cm-1),
this was notthe case in the incommensurate
phase
off3-ThBr4
(40-80
cm-1
for alines)
[10].
Nevertheless the
absorption
spectra
ofU4 +
ina -ThBr4
haveroughly
the same trend as inf3-ThBr4-
Moreover someabsorption
linespresent
aphonon
sideband structure on thehigh
energy side below 200cm- 1
which indicatesstrong
coupling
between the electronic and vibronic states as in the d elements.
If we
interpret
thespectra
under theassumption
thatD2d
is agood
approximation
forS4
symmetry
and that the
3H4
ground
state isF4
as forU4 +
inf3-ThBr4
[10], ThCl4 [22], ThSi04 [27],
weexpect
13 7T zerophonon
lines and 19 a zerophonon
lines inthe range 4 000-25 000
cm-1
deriving
fromr4
T1
andF4 -+ F5
transitions. We observed 14strong
7T lines and 9
strong a
lines in thisregion
and some weak lines thepolarisation
of which could not be observed. The transitionF4 -+
r 2
forbidden inD2d
should be allowed in theS4
symmetry
(r 2
-+-T 1 transitions),
which should raise the number of wpredicted
lines to 21.In the
region
22 000-19 000cm- 1
the 7r line at21 601
cm - 1
and the 2 a lines at 20 034cm - 1
and 19 529cm-1
were attributed to3P2
andlI6
compo-nents.
By
comparing
thespectra
ofU4 +
ina-ThBr4
with those ofU4 +
inf3
-ThBr4,
3P1
is theonly
multiplet
well isolated at about 17 000cm - 1.
In theor
spectrum,
we observed the3P1
(r s )
level at17 083
cm-1
while in the 7Tspectrum
the3P1
(r2 )
ismissing.
Thismissing
7T transition as others(r 4 -+- T2)
can beexplained by considering
theU4 +
to be inS4
symmetry
site which isnearly
D2d.
The observed emission line at 16 907cm- 1
has been attributed to the3P1
(F2) _
3H4
(r s )
transition since when thetemperature
is raised(80 K),
anabsorption
line appears at the same energy. At thesame
time,
some additional lines appear andparticu-larly
another one near the3P1
(T5 )
state at16 973
cm- 1.
This hot line at 16 973cm- 1
wasas-signed
to the3H4
(F5) _
3P1
(r s)
transition. As amatter of
fact,
the observation of alarge
number of hot lines in the visible and infrared from 40 K indicates that the first excitedground
state sublevelat 110
cm- 1
could beT5 like
asU4 +
in f3-ThBr4
[10],
Fig.
1.- Absorption
and emission spectra ofa -ThBr4 : U4+
in the visible and infraredregion
at 4.2 K.The Zeeman
spectra
proved
to beparticularly
useful in
identifying
theF5 lines. Using
themagnetic
field of 6 T at 4.2
K,
Zeemanexperiments
indicated that theabsorption
line at 17 083cm- 1
issplit
which confirms theassignment
of3p,
(F5)-
Moreoverby
exciting
thecrystal
with U.V. radiation from anitrogen
pumped
laser,
Zeemansplitting
was alsoobserved at 4.2 K in the emission
spectrum.
Inparticular
the emission line at 16 907cm- 1
as well astwo others at 19 329 and 14 219
cm-1
wereclearly
split
into twocomponents.
These linescorrespond,
as we assumedabove,
to transitions betweensinglet
states and thedoubly
degenerate
state’H4
(r5)
at110 cm-1.
In the 15 000-16 000
cm- 1 region,
3strong
7r lines1429
multiplets.
Thestrong
7T lines at14 601, 14 573,
14 529 and 14 506
cm - 1
were notassigned
for thefitting.
For
U4 +
inI3-ThBr4’
the3Po,
1D2
and1G4
are closetogether.
By
comparison,
theposition
of the3po
(T 1 )
was established in the 7Tspectrum
at14 389
cm-1,
while thestrong o,-
line at 14 427cm-1
was attributed to
ID2
(Ts ).
A
peculiarity
of theabsorption
and emissionspectra
ofU4 +
in this new host material is that mostof the
absorption
lines likelI6
(Ts)
at 19 529cm-1,
the
3p,
(rs )
at 17 083cm-1,
theID2
(T1 )
at14 389
cm- ,
theH6
(F5)
at 10 647cm ,
the3F3
(r5)
at 8 558cm-1
and the3Hs
(T 1 )
at 6 076cm-1
are followed on the low energy sideby
aset of
2,
3 or 4strong
fluorescent lines. When thecrystal
is excited with theSopra nitrogen
laser,
thelI6
(T 5 ),
the3p,
(T 5 )
and the3Po
(T 1 )
fluorescenceas
well,
but with a weakintensity.
In each group ofemission,
the energy difference between thefluores-cent lines is the same as indicated in table III :
363,
Table III. - Observed
fluorescences of
U4 +
ina -ThBr4 at
4.2 K towards3H4
ground
state Stark levels.(a)
Zeemansplitting
observed.(b)
Lines for which anabsorption
line rises when thetemperature increases.
513 and 720 cm-
1.
When thetemperature
is raisedfrom 4.2 K to 100
K,
thehighest
energy emissionlines from each group decrease faster in
intensity
than the other ones, andabsorption
lines rise up atthe same energy like for
3P1
(T2).
All thesefluores-cent lines come from different
singlet
excited levels near those labelledabove,
to reach 4ground
stateStark levels
including
the lowlying
one3H4
(r s)
at110
cm-1.
Then we could deduce three other Starklevels to be at
473,
623 and 830cm-1.
No Zeemansplitting
was observed for the emission linesreaching
these Stark levels. The fluorescences from each group
reaching
the3H4
state at 830cm-1
could notbe tested
clearly
sincethey
aregenerally
broad and weaker. However aslight
broadening
withmagnetic
field has been observed on one of them.Selective excitation
experiments
with a tunabledye
laser showed that each group of fluorescencelines comes from forbidden
singlet
excited levels very near the allowed lines observed in theabsorp-tion
spectrum.
FromD2d
selectionrules,
and the energyposition
of the hot lines observable at 80K,
we could reach forbidden states andassign
lI6
(r4)
at 19 439cm-1,
3p,
(F2)
at 17 017cm-1,
ID2
(T4)
at 14 355cm-1,
iD2
(F3)
at 14 329cm-1,
3H6
(T4 )
at 10 504cm-1,
3F3
(r4)
at 8 170cm-1
and3H5
(T4 )
at 5 765cm-1. Figure
2represents
thev
partial
energy leveldiagram
for fluorescenttran-sitions
reaching
the3H4
levels inD2d
representation.
The3H4
ground
state Stark levels consist of 2T1
+T 2
+T 3
+T 4
+ 2T 5
forD2d point
groupsymmetry.
In the case where the emission lines arecoming
fromr4
states(group
1, 3, 5, 6,
7)
the observation of 3 or 4 emissions indicates that these lines shouldcorre-spond
toF4 --+
r1
1 andT 4 ->
rs
transitions. In the case where the emission lines arecoming
fromF2
orr 3
states,only
two fluorescent lines are observed andcorrespond
toF2 --I’ rs
orr3 -> F5
transitions. However in this case, the allowed tran-sitions
r 2 ->
r 3
orr 3 -> T 2
aremissing.
From theseconsiderations we attributed the
r s
symmetry
to the3H4
Stark levels determined at 110 and 830cm-1
and
Table IV. - Observed
energy levels caracteristics
for a -ThBr4 :
u4+.
(*) Asterics indicate energy levels deduce.d from the
fluor-escence lines or from hot lines.
the
T1
symmetry
to the3H4
Stark levels deduced at473 and 623
cm- 1
Results of fluorescence and
absorption
measure-ments are summarized in table IV. The table
pre-sents the line
frequency
in vacuo, thepolarization,
D2d
andS4
symmetry
assignment.
5. Discussion.
The levels were fitted
by
simultaneousdiagonali-zation of the free ion
Hn
andcrystal
fieldH CF
Hamiltoniansdescribing
the energy levels ofU4 +
inD2d
symmetry.
Fitting
theexperimental
levels withthe
starting
parameters
obtained forf3 - ThBr 4 :
U4 +
[10]
gives
a verylarge
rms deviation fora -ThBr4. Using
thef3-ThBr4 :
U4 +
parameters,
wediagonalized
the matrices with various values ofB 0 2.
Only
B 0 2
400cm-1
gave the correct separ-ation between the3pl
F2
andF5
levels. With this value forBo,
we tried to fitseparately
T1
andT5
levels. Both fits gave a different set ofparameters.
While the 11
assigned F5
levels led to an rmsdeviation of 62
cm-1,
the11 r 1
levels were fitted with an rms deviation of 72cm- 1. Finally
the best fit for the 22 levelstogether
was obtained with thestarting
values for theT1
levels. From the calculated energylevels,
30 transitions could beassigned
withgood
agreement
between the calculated and measuredenergies.
TheBq
were firstvaried,
then theFk
and £
parameters.
Finally
all theparameters
were varied
simultaneously.
For the fit with 30 levels an rms deviation of 77cm-1
was obtained with11
parameters
varying.
In this fit three levels couldnot be well
fitted,
theF5
level at 19 529cm-1
and the twoground
state Stark levels3H4
at 473 and623
cm-1
attributed toT1
states. Moreover 4strong
7T lines in the
region
of the3Po
(14 500-14
600cm-1)
could not be attributed to calculated levels. The calculated energy levels and
eigen
vectors aregiven
in table V and the final values of theparameters
aregiven
in table VI.Compared
with thespectroscopic
parameters
ofU4 +
inf3-ThBr4
[10]
andf3-ThCI4 [22],
the calcu-latedparameters
ofU4 +
ina -ThBr4
aredifferent,
particularly
Bo
which is smaller and thesign
ofBo
andB4
which becomesnegative.
If the rmsdeviation is not as
good
as inf3-ThBr4’
thecrystal
fieldparameters
are however determined with anuncertainty
of about 10 %except
Bo
andBo.
Moreover a decrease in theFk parameters
especially
forF4
isobserved,
whichgives
a ratioF4/F2
smallercompared
to the values obtained forf3-ThBr4.
The Auzelparameter
[28]
N v
can be introduced to1431
Table V. - Calculated and
experimental
energy levelsof a -ThBr4:
U4 + .
Table V
(continued).
Table VI. -
Spectroscopic
parameters
for
U4 +
ina-ThBr4
incomparison
with thoseof
13-ThBr4-(1)
TheMk
andP k
values were fixed :Mo
= 0.99,M2
= 0.55,M4
= 0.38,P 2 = P 4 = p 6
= 500,y value
was fixed.1433
Though
theparameters
are very different from theJ3-form,
thecrystal
fieldstrength
has almost the same value for a and8-ThBr4
(Tab. VI).
This set of
parameters
however is notcompletely
satisfactory
because it isdisturbing
that three intensetransitions
(the
two3H4
Stark levels at 473 and 623cm-1
well determined from several fluorescencelines and the
TS
at 19 529cm-1)
fit sopoorly.
Moreover the w line at 21 601cm-1
has adiscrepancy
with the calculated level of 234
cm-1
which is muchmore than the average
discrepancy (39
cm-1 ).
Infact this level fits very well when all the
T1
levels arefitted. From the studies of Naik
[29],
Auzel et al.[30]
and Schoenes
[31],
we can assume that theproximity
of the 6d band to the 5f ones couldprovoke
aninteraction between both
configurations,
which isnot taken into account in the Hamiltonian. It could shift the energy of the
highest
levelsrl
(19 529
cm-1)
andri
(21601
cm-1).
Many
fits weretried from various
starting
parameters
andparticu-larly
the one obtained forJ3 - ThBr4,
butthey
result in pooragreement
with all the levels. Another reasonfor these
discrepancies
can be due to the fact that the sitesymmetry
forTh 4,
in this matrix isS4
and that we made theapproximation
ofD2d
symmetry.
The difference obtained in the
crystal
fieldcalcu-lation between both matrices a and
8-ThBr4
indi-cates
that,
although
tetravalent uranium ion issurrounded
by
the sameligands,
the mostimportant
difference in the two forms
namely
the relativeorientation of the coordination
polyhedron
within the structure, the distances U-Br and theangles
Br-U-Br(Tab. VII)
play
animportant
role in thecrystal
fieldparameters.
Table VII. -
Principal
bond distances(A)
andangles
in thepolymorphic forms of ThBr4
andJ3 - ThCl4
(Ref. [1])
a,J3 - ThBr 4°
In the
0-form,
the axes of thepolyhedron
lie in the(100)
plane
of the unit cell while in the a-structure,the
polyhedron
has been rotatedby
about45°,
the c axis and thepolyhedron
axis lie somewhat outsidethe
(110)
planes.
This rotation allows for a moreefficient
packing
of the Br- atoms in the a-form.Moreover,
the metalligand
distances areapproxi-mately
all the same fora -ThBr4
while there existtwo different Th-Br bond distances for
13 -ThBr4.
Fora -ThBr4
all the bond distances Th-Br can be seen asintermediate between the
longest
and the shortestones in
f3-ThBr4.
6. Conclusion.
The
optical
spectra
ofU4 +
ina-ThBr4
have beenanalysed
with 30 transitionsassigned
in theD2d
approximation.
Although
both matrices a andf3 - ThBr 4
looksimilar,
it appears that thespectro-scopic
properties
of the uranium tetravalent ion arequite
different from one matrix to the other. As amatter of
fact,
U4 +
ionsgive
verystrong
fluor-escences in the visible and infrared
region
in the aform while
only
2 weak fluorescence lines wereobserved in the
J3-form.
On the other hand thecrystal
fieldparameters
obtained in thisstudy
arevery different from those calculated in the
{3-form.
Since the sameligands
surround the uraniumion,
itseems that the
change
in the structureplays
animportant
role for thecrystal
field even if the sitesymmetry
in the a-form which isS4
can beapproxi-mated
by D2d.
It isinteresting
to show that a smallchange
in the structure with the same ionsproduces
an
important change
in thecrystal
fieldparameters
and that this scheelite structure material induces somany intense fluorescence lines for
U4 +
as the others scheelites do for rare earth ions andtetrava-lent
neptunium
[17].
The fact that thehighest
energy levels ofU4 +
do not fit as well as the others could be due to 5f-6dconfiguration proximity.
Acknowledgments.
We wish to thank Dr. G. Goodman for
helpful
discussions and Dr. N. Edelstein forproviding
us with the matrix elements and least squares program.References
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