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X-ray absorption near edge structure of quartz.
Application to the structure of densified silica
P. Lagarde, A. Flank, G. Tourillon, R. Liebermann, J. Itie
To cite this version:
P. Lagarde, A. Flank, G. Tourillon, R. Liebermann, J. Itie. X-ray absorption near edge structure of
quartz. Application to the structure of densified silica. Journal de Physique I, EDP Sciences, 1992, 2
(6), pp.1043-1050. �10.1051/jp1:1992113�. �jpa-00246584�
Classification Physics Abstracts
61.10D 61.40 62.50
X-ray absorption
nearedge structure of quartz.
Application to the structure of densified silica
P-
Lagarde ii),
A. M- Flankii),
G- Tourillonii),
R. C. Liebermann(2)
and J. P- Itie(3)
II)
LURE (CNRS, CEA, MENJS) Bit. 209d, Centre Universitaire, 91405Orsay,
France (2) Center forHigh
Pressure Research, StateUniversity
of New York,Stony
Brook, New York11794, U-S.A.
(3)
Physique
des Milieux Condens£s, Universit£ P. et M. Curie, 4place
Jussieu, 75230 Paris Cedex 05, France(Received 20
January
1992, revised andaccepted19
March 1992)Abstract.
X-ray absorption
spectra of quartz(10T0),
pure silica and densified silica underpressure have been recorded at the silicon and oxygen
K-edges.
The spectra of quartz show intensepolarization
effects which have beeninterpreted
on thesingle scattering approximation,
using geometrical considerations. Thecomparison
between the spectra of silica and densified silica, on the basis of thisinterpretation, gives
some information on the structural effect sufferedby
the silica network under pressure.Introduction.
X-ray absorption
spectroscopy(XAS)
has been, and isstill,
apowerful
tool for theunderstanding
of the local order inamorphous systems.
This comes from thesensitivity
of the ExtendedX-ray Absorption
Fine Structure(EXAFS)
to the very local order due to the 2 k-dependence
of theoscillatory signal [I], despite
the fact that the structural disorder becomes often a verystrong
limitation to the extraction of a reliable radial distribution function[2].
Forinstance EXAFS
analysis
inamorphous
metallicalloys
has been able to show thesplitting
of the first coordination shell into two different subshells[3]
and this accuratedescription
of the local order could not be achievedby
any other method : in that case EXAFS appears to beshort-range
limitedcompared
toscattering techniques
but at the sametime,
much more sensitive to fine details of the local order. Whenapplied
to covalentglasses
oroxides,
thistechnique
does notyield
useful information : the first shell is well defined because of thestability
of the valence bondangles
and it is very close to itscrystalline
counterpart ; however the distribution of the dihedralangle
is wideenough
to eliminate thesignal
from the medium range order.Nevertheless,
someinteresting pieces
of information can begained
from a more detailed dataanalysis
in somespecial
cases[4]
orby taking
into account the threebody
correlation function
[5],
at the cost ofincreasing
thecomplexity
of the calculations.1044 JOURNAL DE PHYSIQUE I N° 6
At the same time it is also well known that the
X-ray
NearEdge
Structure(XANES)
part ofthe spectrum contains much more information on the
medium-range
order[6]:
itsquantitative analysis
is still a very difficult task which hasonly
beenattempted
in someselected cases
[7, 8], primarily crystalline
materials with asimple symmetry
andclosely
relatedamorphous
systems.Among
the numerousglasses,
silica is ofparticular
interest because of its natural abundance as well as its wide range of industrialapplications
nevertheless its structure is still notfully
elucidated. Since it is one of the most abundant materials in the earth'sinterior,
the behavior of the structure of thisglass
when submitted tohigh temperature
and/orhigh
pressure is of a fundamental interest in
geophysics. Finally,
silicon and silicon oxide and sub- oxides are present in all the electronic devices based on the MOStechnology
; the structure of the first oxidelayers
on thetop
of a silicon substrate[9],
the structure of silicon suboxides[10]
and that of different kinds of silicas obtained
through
thesol-gel
route[I
I are still thesubject
of fundamental research in materials science
by
XAS-All of these reasons make the
understanding
of theX,ray absorption
of the silicon in anoxidized environment very valuable. Since the
analysis
of the EXAFS data has not been able togive
much more than the first oxygen shell around the silicon atom, we have focused our attention to the nearedge part
of the spectrum with thegoal
ofextracting
somesignature
onthe
absorption
spectra from themedium-range order,
which could then be used to understand the structure of an unknown material.Therefore,
we started with theinterpretation
of the X- rayabsorption spectra
ofquartz, keeping
in mind that thespectra
of theamorphous
state is sometimes reminiscent of that of thecrystalline
material. As anillustration,
thechange
on the middle range of silica when densified under veryhigh
pressure will beanalyzed.
This firstapproach
will becompleted by
a fullmultiple scattering analysis
which is now in progress toquantify
these conclusions.1.
Experimental techniques.
XANES spectra of quartz, silica and densified silica have been taken at the silicon and the oxygen
K-edges.
In the case ofquartz, polarized spectra
have been recorded with the z-axis of thecrystal aligned parallel
or normal to thephoton
electric field. Theexperiments
have beendone at
SuperAco
: silicon spectra have been taken on the SA32 softX-ray
beam lineusing
the two
crystal
monochromatorequipped
withInsb(ill) crystals.
Theexperimental
resolution is then of the order of 0-7 eV ; the
absorption signal
is collectedby measuring
thetotal electron
yield
with a channeltron in thecounting
mode while theincoming
flux ismonitored
by
an ion chamber.Oxygen spectra
have been collected on SA72using
a TGMmonochromator in that case, the
experimental
resolution is of the order of 0-3 eV. Threesamples
have been run : aquartz (1010)
set normal to thephoton
beam and rotatedalong
an axisparallel
to thephoton beam,
a pure silicaglass
and a densified silica. This densifiedsample
wasproduced
at theStony
BrookHigh
PressureLaboratory compressing
rods ofnormal
a-Si02
in an uniaxialsplit-sphere
apparatus up to pressures of 16GPa at roomtemperature.
Fromdensity
measurement, the densification can be estimated to about 20 fb- The twoamorphous samples
were set at the same incidenceangle.
2. Results and discussion.
2-1
QUARTZ. Figure
I shows the two silicon nearedge spectra
of the(lfl0) quartz
: the(1010) plane
is oriented normal to thephoton
beam and the c-axis has been orientedparallel
or normal to the electric field of the
photon.
These twospectra
are raw data since the1850 1860
E(eV)
Fig. I. Silicon XANES spectra of quartz I do with two orientations of the
crystal
i,ei,ins thephoton
electric field I: solid line I
perpendicular
to the z-axis, crosses : Iparallel
to the =-axis.incoming
flux is monitored at eachexperimental point by
the ion chamber and thequantity I/Io
is known to beproportional
to theabsorption
coefficient, While the two white linesappears to be identical there are considerable differences between the two
spectra
in the first 40 eVbeyond
theedge
whichobviously correspond
topolarization
effects due to the electricdipole
operatorentering
the matrix element[I]-
Figure
2 shows the structure of the quartz(1010) plane
whereonly
one unit cellalong
the direction normal to thisplane
has been taken into accountdepending
on the orientation ofe
Fig.
2. View of the quartz(ld0) plane.
Silicon atoms are small circles.Only
one unit cell has been usedalong
the x-axis and thefigure
has been rotatedslightly
around they-axis
forclarity.
The z-axis ishorizontal. The labels refer to the text.
1046 JOURNAL DE
PHYSIQUE
I N° 6the electric field with
respect
to the z-axis we obtain the situations describedby figure
I. The XASspectra
isgovemed by
Fermi'sgolden
rulep cc
£ )(I)I,r) f))~6(E~-E;-hw)
where
I)
andf)
are the initial and final states. Because the matrix element contains the scalarproduct
I r where I is thephoton
electric field and r the interatomic vector which links theabsorbing
atom and theneighbors, only
these interatomic vectors which have a non-zeroprojection
onto thephoton
electric field will appear on the spectrum. Examination offigure
2 shows that :I)
the first and the second shell must contribute almost with the same amount to the twopolarized
spectra : around the silicon atom A forinstance,
the first shell of four oxygen atoms at 1.6I
hasa pure tetrahedral symmetry and the four-second
neighbor
atoms at 3.06/k
mustcontribute more or less
isotropically-
This is in accord with the observation that theshape
resonance at 865 eV has almost the same energy and the same
intensity
for the two spectra.From
multiple scattering calculations,
this resonance has been attributed to the 9 atoms clustercomposed
of one silicon atom, the four oxygennearest-neighbors
and the four siliconnext-nearest
neighbors [12]
it)
the main differences in the local environment of one silicon atomprojected
onto the electric field comes from outer shells which are active in one orientation and not in the otherone- The most obvious effect comes from the atoms at 4-9
/k
labelled B and B'along
they-axis
and the atoms A and A' at 5.4
/k along
the z-axis : alarge polarization
effect is to beexpected
from this situation since there is no
intervening
atom between the central and thescattering
ones. To a lesser extent the
third-neighbor
oxygen atoms alsoproduce
apolarization
effectwhich appears in
figure
2 : while the thirdneighbors
at3-6i (atoms c)
are distributed
isotropically
around the central atomA,
this is not the case for those at 3.9I (atoms d)
or at 4-1
I (atoms e)
; the former will be influential when the electric field is
parallel
to the z-axis and the latter when the field ispolarized
normal to the z-axis.To a first
approximation,
each group ofscattering
atoms at onegiven
distance willcontribute to the
absorption spectrum by
ashape
resonance. The energyposition
AE of such a resonance, when measured from the
edge
energy, scales with the interatomic distance R as[13]
:AE *R ~
= constant
Therefore we can
interpret
the structurespresent
in the XANES quartz spectra in thefollowing
way :the two lines at 1853 and 855 eV
correspond
to thescattering by
the silicon atomsalong
the z and they-axis respectively,
at 5-4 and 4.9I,
the two resonances at 857.4 and 859 eV are due to the oxygen third
neighbors,
thefirst one
being
attributed to those atoms at 4.II
while the second featurecomes from the
oxygens at 3.9
I- Using
this identification for these four resonances we obtain the same value of 843 eV(within
I eVaccuracy)
for the energy oforigin.
This energy is thelow,energy
limitof the white
line,
as
previously
indicated the wideshape
resonance around 865 eV is due to the Flrst and secondneighbors
of the silicon.2.2 SILICA AND DENSIFIED SILICA. The two spectra of silica and densified
silica,
in thesame energy range as that of the
quartz,
are shown infigure
3- These spectra have been normalized to the sameedge step
taken at the maximum of theshape
rdsonance at 865 eV-1850 1860
E(eV) Fig.
3. a) solid line= silicon XANES spectrum of the pure silica
glass,
b) crosses= silicon XANES spectrum of the densified silica. The two spectra have been normalized at the same values before the white line and at 1865 eV-
The most
significative
differences between them and with thequartz
spectra are thefollowing:
I)
in both cases the white line appears at the same energy as in thequartz
but it isslightly
wider in silica than in quartz. It is even wider in the case of the densified silica
it)
in the range 850-1 860 eV some structures are still present which vary from one silica to the other one. Thesechanges
havealready
beenreported
without anyexplanation [12]
iii)
the structure at 1865 eV is stillpresent,
in anequal
amount, in bothspectra
and itkeeps
some resemblance with that of thecrystalline
material.2-3 DiscussioN- The white line
corresponds
to the ls-
3p
transition. Since quartz is aninsulating
material with4sp3 hybridization,
the first level above the gap is of strong p character and it is empty,leading
then to a strongabsorption
coefficient. This white line is of the sametype
as the discrete resonances due to thepromotion
of a core electron into a low-lying
empty molecular orbital which have been observed in tetrahedral molecules likeSiC14, SiF4
orSi(CH~)4 l14]. Therefore,
the short range order alonegives
the main character of this final level and theposition
of the white line and its width remain in firstapproximation
thesame since the elemental
Si04
unit is considered to remainunchanged
ingoing
from quartz to silica : fullmultiple scattering
calculations of a 5 atom cluster[15] composed
of one central silicon atom and its foursurrounding
oxygens show that this white line can beexplained by
this local environment.
Nevertheless,
thelong
range order must determine the exact value of the width of this level and we expect therefore the width of the silica white line to be greaterthan that of the
quartz.
Thechange
in theshape
but not the energy of this line after densification is therefore asignature
of thebroadening
of the3p
statesfollowing
aslight
distorsion of the tetrahedron which occurs without any
significant change
of the interatomic distances for the Si-O firstneighbors.
This is in line with neutron diffraction results on thesame
sample
where nochange
in the Si,O and O-O mean distances have been detected whereas the width of the distribution of this last distance wasenlarged [16]-
It could also indicate that the disorder is even morepronounced
in the case of the densified silica.That the two
shape
resonances around 865 eV are similar in both silica and rather close to that on quartz appears to indicate that thehigh-pressure cycle
does notaffect,
in first1048 JOURNAL DE
PHYSIQUE
I N° 6approximation,
the close environment of the silicon atoms up to the second shell apart for theslight changes
which have been discussed above. Infact,
fullmultiple scattering
calculations[17]
at the siliconedge
show that thisspectral
feature is almost insensitive to the Si-O-Si bondangle
in theexpected
domain of variation of thisangle
uponamorphisation
or densification.While little
insight
can be obtained from the siliconK-edge,
some information comes from the oxygenK-edge
shown infigure
4 : it iscomposed
of a wide white line at 540 eV followedby
ashape
resonance at about 560 eV whichslightly
shifts tohigh energies
in the case of thedensified silica. XANES calculations
[17]
have attributed this resonance to the Si-Si secondneighbor
distance related to the Si-O-Si bondangle
an increase of thisangle
leads to an increase of the energysplitting
between this resonance and the main white line. Therefore the variation we observe in the densified silica asinterpreted
on the basis of thiscalculation,
seems not in agreement with other results
[18],
which conclude to a decrease of the Si-O-Siangle,
but definite conclusions from XAS need more accurateexperimental
and theoretical results.a
a Si02
b
ji
b densfied Si02§
d
z a
o
#
~ o b~i
535 540 545 560 565 570 575 580
ENERGY (ell~
Fig.
4.Oxygen K-edge
XANES of silica and densified silica. Notice the shift in energy of theresonance at 560 eV.
The main modifications between the
crystal
and theglass,
and between the twoglasses,
appear in the XAS spectra between 1850 and 1860 eV and thus comes from interatomic
distances
beyond
the third shell. In order toclarify
thispoint,
we have shown infigure
5 the differencespectra
:figure 5,
curvea)
is the difference between the quartz spectrum in theparallel
andperpendicular
orientations(Fig. I)
whilefigure 5,
curveb)
shows the differencebetween silica and densified silica after
being
normalized to the sameedge step (Fig. 3)-
Inthis latter case,
only
thepart
between 1850 and 1870 eV has beenplotted
because thedifference between the two white line
yields meaningless
values in the range 840 to848 eV. Two main features appear in
figure 5,
curvea)
at 853 and 859 eV we attribute them to the structural differences describedpreviously
on the(1010) plane
of the quartz : thefirst one comes from the silicon atoms at 5,4 and 4.9
I along
thez and
y-axis respectively
while the second feature comes from oxygen third
neighbors.
Without calculation of the XAS spectrum, it is notpossible
to be morespecific, Figure 5,
curveb)
shows the firstspectral
1858 1866 E(eV)
Fig.
5. Differences between the normalized silicon XANES spectra : curve a) crosses quartzparallel
to the z-axis minus quartz normal to the z-axis. Curve b) solid line : pure silica minus densified silica.
Only
the energyregion beyond
the white line has beenplotted.
feature and
perhaps
some hint of the second one ; thisimplies
that the oxygen environment of the silicon at around 4/k
isonly slightly changed
upon densification and that theprincipal
modification of the structure at this
mid-range
interatomic distance affects the Si-Si at about 5/k-
This suggest that the silicon atoms at about 5-4I (which
existonly
for 6-members oflarger rings),
move to aposition
similar to the atoms situated in the xyplane
ofquartz
at 4-9I la position
which canonly
be obtained for smallerrings).
This result could be an indication fora
change
in therings
statistic upondensification,
with an increase of the concentration of low- memberedrings,
ingood agreement
with the data obtained from neutronscattering
results on the samesample [16],
Conclusions.
A
comparison
between XASspectra
of quartz in twopolarisations,
of normal silica and densified silica at both the silicon and the oxygenK-edges
has led us to thefollowing
conclusions :
the XANES structures of
quartz
have been attributed tospecific
interatomicdistances,
Si-O at 3.9 and 4, II,
Si-Si at 4.9 and 5,4I.
These results have to be confirmedby
a
multiple scattering approach
;the white line, due to the
Si04
tetrahedron, isunchanged
from thecrystalline
to theamorphous
state but isslightly
wider upondensification,
an indication for aslight
distorsion of thisSi04
unit under pressure ;the oxygen
K-edge
shows a smalldisplacement
of the resonance at 560 eV tohigh
energies
upondensification,
difficult tointerpret
in terms of the Si-O-Si bondangle
variation ; in the Sispectrum
of normalsilica,
there exists asignature
from Si,Siresulting
fromlarge-membered rings.
This interatomic distance of 5.4I
decreases incompression
to a value close to thatpresent
in thecrystal along
the xyplane (I,e.
4.9h).
1050 JOURNAL DE PHYSIQUE I N° 6
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