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E.S.R. of CO3-3-Li+ centre in irradiated synthetic single crystal calcite
G. Bacquet, J. Dugas, C. Escribe, L. Youdri, C. Belin
To cite this version:
G. Bacquet, J. Dugas, C. Escribe, L. Youdri, C. Belin. E.S.R. of CO3-3-Li+ centre in irradiated synthetic single crystal calcite. Journal de Physique, 1975, 36 (5), pp.427-429.
�10.1051/jphys:01975003605042700�. �jpa-00208268�
427
E.S.R. OF CO3-3-Li+ CENTRE IN IRRADIATED SYNTHETIC SINGLE CRYSTAL CALCITE
G.
BACQUET,
J.DUGAS,
C.ESCRIBE,
L. YOUDRI(*)
Laboratoire de
Physique
des Solides(**),
UniversitéPaul-Sabatier,
31077 Toulouse
Cedex,
Franceand C. BELIN
L.E.P., 3,
avenueDescartes,
94450Limeil-Brévannes,
France(Reçu
le 2 décembre 1974,accepté
le9 janvier 1975)
Résumé. 2014 Dans des monocristaux de calcite synthétique irradiés aux rayons X à la température ambiante, on observe le spectre de résonance d’un électron célibataire
piégé
sur un ion carbonate etcouplé à un noyau de lithium. Ce défaut qui a été identifié comme étant un ion moléculaire
CO3-3
stabilisé par un ion Li+ en
position
interstitielle, présente une symétrie axiale suivant l’axe c. Il est très stable à la température ambiante.Abstract. 2014 An E.S.R. spectrum of effective spin S
= 1/2
exhibiting a hyperfine structure quadru- plet has been observed in synthetic single crystal calcite X-irradiated at 20 °C. From the g values it is deduced that this spectrum is due to aCO3-3
molecular ion which is charge stabilized by aninterstitial Li+ ion. This defect which is axially symmetric along the crystalline c axis is very stable at room temperature.
LE JOURNAL DE PHYSIQUE TOME 36, MAI 1975,
Classification Physics Abstracts
8.632
In
naturally occurring single crystal
calcite severalparamagnetic species
createdby
irradiation wereidentified
by
means of the E.S.R.technique.
Somehave been shown to be molecular
ions, originating
from the ionization or
degradation
ofimpurities substituting
forCO23 -, by
Marshall et al. at theArgonne
NationalLaboratory.
Two others are para-magnetic
carbonate ions defect centres(C03
andCO33 -)
which areusually produced by
y or X-irradia- tion at 77 K[1].
Both exhibit poordegrees
ofstability
upon
warming. CO33 -,
which is the morestable,
bleaches out with a half-life of 10 hours at 300 K.
This latter molecular ion was also found to be stabi- lized
by Y3 +
in an interstitialposition
withequal probability
ofbeing slightly displaced
either above orbelow the
plane
of the normal divalent carb’onate ions[2].
On the otherhand,
in a recent paper, Casset al.
[3] reported
E.S.R. and E.N.D.O.R. spectra of amagnetic
centre stable at room temperature whichwas created
by
y irradiation of natural calcite.They proposed
that the defect is theHCO23-
molecularion
arising
from the ionization of bicarbonate ionimpurities.
(*) Détaché de l’Université Mohamed-V de Rabat, Maroc.
(**) Laboratoire associé au C.N.R.S.
The results
presented
here were obtained withspecimens
ofsynthetic single crystal
calcite grown at the L.E.P. of Limeil-Brévannes(France) by
meansof the
Travelling
Solvent ZoneMelting
methoddescribed
by
Belin et al.[4],
whereLi2CO3
was usedas a solvent.
Samples
of dimensions 0.4 x 0.3 x 0.3cm’
wereX-irradiated
(20 kV,
10mA)
at R.T.during
about15 hours and then studied in the X-band
using
aconventional 100 kHz field modulation
spectrometer,
at the same
temperature. Immediately
after the irra-diation,
several spectra due to different defects weresimultaneously
recorded. These last exhibitvarying degrees
of thermalstability
and this report is devoted to the most stable ofthem,
the E.S.R.patterns
of which are characterizedby
very narrow lines’
(AH
100mG)
which areeasily
saturated.When the Zeeman field vector lies in any
plane perpendicular
to thecrystalline
c axis(such
aplane
is
parallel
to theplanes containing
the host carbonateions)
the spectrum consists of three sets ofhyperfine quadruplets
where A = 2.55 G. The central set(Fig. la) being
about two hundred times as intenseas the two outer ones which are at a distance of 126
G,
thispermits
the observation of a much less intensehyperfine triplet (where
A = 1G)
betweenArticle published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:01975003605042700
428
FIG. 1. - Schematic representations of the ’Li+ stabilized
CO33-
molecular ion central spectrum for various orientations of the crystal
in the static field. Allowed lines are designated by a.
the two inner lines. The relative
intensity
andposition
of lines inside the central pattern indicate that the
unpaired
electron iscoupled
with one lithium nucleus which has twoisotopes having
different nuclearspins :
these are 7Li(I = 2,
92.6% and y
=3.256)
and ’Li
(I
=1, 7.4 % and y
=0.822).
When the
crystal
is rotated about any axis perpen- dicular to the c axis extra lines appear which canonly
be seen in the central set(Fig.
lb andlc).
Accord-ing
to theirpositions
andintensities,
it is clear that these are so calledforbidden hyperfine
transitions(AM,
=1, AMI
=1, 2, 3).
With the
magnetic
fieldparallel
to the caxis,
thecentral
pattern
isagain composed
of fourlines,
each of them
being
thesuperposition
of several transitions(Fig. Id). Only
the central line of the 6Lispectrum
is seen, the two othersbeing
hiddenby
thespectrum
of another stable defect. On the other hand the lineintensity
is too weak(see below)
topermit
the observation of the two satellites. The
experimental
line
positions
for ’Li aregiven
infigure
2.What can be said about the nature of the defect ? The
unpaired
electron isweakly coupled
with alithium nucleus and is
essentially
located on a carbo-nate as indicated
by
theobservation,
when H 1 c, of two sets ofhyperfine quadruplets
at a distance of 126 G dueto 13C
ofI = 1/2
with 1.1%
natural abun- dance. This value ofthe 13C splitting
isequal
to thatmeasured in the case of y3 1 stabilized
CO33 - (see
Table
I).
On the otherhand,
our measured gll andY.L values
(see
TableII)
are identical to those of bothCO33 -
andY3+
stabilizedCO33 -. Consequently
wecan assert that we are
observing
anaxially symmetric,
Li+stabilized, C03-
molecular ion.FIG. 2. - Experimental and theoretical (full lines) angular depen- dences of various lines when the magnetic field is rotated about an
axis perpendicular to c.
x AMI = 0 ; e AMI = 1 ; c:J AMI = 2; : AMI = 3 .
TABLE 1
13C
hyperfine coupling
constant valuesfor
variousC03 - defects
TABLE II
Spin
hamiltonian parametersof
’Li stabilizedCO33 -
molecular ionA and
Al. have the same sign which is unknown.In the case of ’Li for which all
experimental
dataare
available,
the observedspectra
may be inter-preted by
thespin-Hamiltonian :
Je=
PB H. g. S + S. Ã. 1 - PN ON H. 1 ( 1 )
where the nuclear Zeeman interaction is taken to be
isotropic,
and with S= 2
and I =2.
The various constants of(1)
are summarized in table II.It is worth while to underline here the
importance
of the nuclear Zeeman term. Its
value,
which isequal to 2 A Il’
enables one toexplain
theposition
(full
lines inFig. 2)
as welt as theintensity of forbidden
transitions.
They
can still occur when the static field is very close to the caxis,
but vanish when H and c arecarefully aligned.
We think that the insufficientintensity
of the lines infigure
1 d may beexplained
429
by a slight ( 10) misalignment
of thecrystal
insidethe
cavity.
It can be seen infigure
2 thatexperimental
and theoretical
angular dependences
are ingood agreement.
Theexperimental uncertainty ( ±
0.15G)
which seems
large
is due to the fact that we areobliged
to measure the field values
by
means of proton reso-nance outside the spectrum as even at the lowest level available the 50 Hz field modulation causes
broadening
of E.S.R. lines.The
hyperfine
tensor can be writtenÂ
=Aiso + Î,
where
T is
a traceless tensorand 1 Air,. 1
= 8.52 MHz.For an
unpaired
electronfully
localized in the lithium atom 2s orbital the Fermi contact terniA;SO,
calcu-lated from wave functions
given by
Clementi[5], equals
158.5 MHz.Comparing
these twovalues,
wefind that the
unpaired
electronspin density
in thelithium 2s orbital is 5.37
%.
In the case of a pureCOI
molecular ion
only
l.1%
of thespin density
is localizedon a nearest
neighbour Ca2+ [2].
This indicates that the lithium nucleus is closer to the carbonate than such a calcium. Since the Li+ stabilizedC03 -
mole-cular ion has an axial symmetry about the c
axis,
we suppose that the lithium ion lies in an interstitial
site,
either above or below acarbonate, approximately
in a
plane containing
calcium ions as shown infigure
3.With such a
configuration
the defect has a netdoubly
negative charge,
likeHCO23-
molecularion,
whichexplains
its greatstability.
It is necessary to warm thecrystal
up to 400°C for half an hour tocompletely
bleach out this
paramagnetic
centre.FIG. 3. - Schematic representation of the calcite structure showing
the proposed localization (shading line) of the interstitial lithium ion (r = 0.68
Á)
along the c axis above a carbonate ion.c’’0 = 17.020 A. White circles : oxygen; dashed circles : calcium;
Black circles : carbon. ’
References [1] SERWAY, R. A. and MARSHALL, S. A., J. Chem. Phys. 46 (1967)
1949.
[2] MARSHALL, S. A., MC MILLAN, J. A. and SERWAY, R. A., J. Chem. Phys. 48 (1968) 5131.
[3] CASS, J., KENT, R. S., MARSHALL, S. A. and ZAGER, S. A.,
J. Mag. Res. 14 (1974) 170.
[4] BELIN, C., BIUSSOT, J. J. and JESSE, R. E., J. Cryst. Growth 13-14 (1972) 597.
[5] CLEMENTI, E., Tables of Atomic Functions (1965).