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The exact equation for Brillouin shifts
V. Chandrasekharan
To cite this version:
V. Chandrasekharan. The exact equation for Brillouin shifts. Journal de Physique, 1965, 26 (11),
pp.655-658. �10.1051/jphys:019650026011065500�. �jpa-00206331�
THE EXACT
EQUATION
FOR BRILLOUIN SHIFTSBy
V.CHANDRASEKHARAN,
Laboratoire des Hautes Pressions, C. N. R. S., Bellevue.
Résumé. 2014 L’équation exacte des
deplacements
dans l’effet Brillouin est représentée par :$$
$$
03BDi est la fréquence de l’onde incidente, 03B8 l’angle de diffusion ; 03B2s = ns ve /c, 03B2i = ni ve/c où ns et ni sont les indices de réfraction pour l’onde incidente et l’onde diffusée, c la vitesse de la lumière dans le vide, et ve la vitesse de l’onde acoustique
responsable
de la diffusion.Les deux faits les
plus
importants sont l’effetd’anisotropie
dans les cristaux biréfringents, déjàdiscuté par l’auteur et l’effet dû au terme quadratique.
Dans le cas des cristaux isotropes et des
liquides,
on a :$$
Le terme quadratique conduit à des déplacements inégaux pour les composantes Stokes et anti- Stokes, correspondant à l’effet Doppler relativiste, plus un
petit
terme de dispersion.Pour la diffusion arrière dans le diamant, l’effet Brillouin quadratique pourrait être déterminé
expérimentalement ;
lesdéplacements
prédits pour les composanteslongitudinales
suivant la direction [111] valent, pour 03BB = 2 537 Å039403BDAS = + 12,79887 cm-1 0394vS = - 12,79370 cm-1.
Abstract, 2014 The exact equation for the Brillouin shifts is given by
$$
$$
where 03BDi is the
frequency
of the incident light, 03B8 the scattering angle, ns and ni are the refractive indices for the incident and the stcattered waves ,c thavelocity
of light in vacuum, 03BDe the velocityof the acoustic wave responsible for the scattering ; 03B2s = ns 03C5e/c, 03B2i = ni 03C5e/c. The two
main additional features are the anisotropic effect for birefringent
crystals
discussed earlier bythe author [3] and the quadratic term. In the case of isotropic
crystals
orliquids.
$$
The quadratic term leads to
unequal displacements
of anti-Stokes and Stokes components corresponding to the relativisticDoppler
effect but with a small dispersive term.In the case of backward scattering in diamond the
quadratic
Brillouin effect can be determinedexperimentally ;
the expected shifts for longitudinal components along the [111] directionare for 03BB 2 537, 039403BDAS = + 12.79887 cm-1, 039403BDs = - 12.79370 cm-1.
PHYSIQUE 26, 1965,
Introdtietion. - Several years ago a
systematic investigation
of Brillouinscattering
incrystals
wasundertaken
by
Krishnan and the author[1-5] using
2 537
A
resonance radiation of mercury. In thisconnection,
the author[3] generalized
the Brillouinequation
tobirefringent crystals
and showedthat,
in
general,
there would be 12pairs
of Brillouin com-ponents
instead of 3 as in the case ofisotropic
crystals.
Interest in this field has been revivedrecently, by
thediscovery
of the laser and thestimulated Brillouin
scattering [6].
In the usual
theory,
the smallchange
in wave-length
of the scattered radiation isimplicity igno-
red in the
equation
for conservation of momentum.It was considered worthwhile to take into account this second order effect in view of
high precision
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:019650026011065500
656
attainable with a laser source. The exact equa- tion for Brillouin shifts
is, therefore,
derived andapplied
to the case of diamond.Derivation of the exact
equation.
- After can-celling
out h in the elastic interaction ofphotons
and accoustic
phonons,
the conservation laws of energy and momentumyield
where the
subscript
i denotes theincident,
s thescattered
photon
and e the effectivephonon
res-ponsible
forscattering, v
is thefrequency
and Xthe
wavelength.
If n is the refractive
index,
ve is thevelocity
of the
phonon
and c thevelocity
oflight,
thenputting
Squaring (4)
to convert it into a scalarequation fi§ vg - 2fis fii eos 0 vs vi + fif v) = v)
(5) where 6 is theangle
ofscattering.
Combining equations (1)
and(5)
This is the exact
equation
for Brillouin shifts.Ignoring
terms to orderhigher than P2
Leaving
out the second order term in this equa- tion leads to thatdeveloped by
the author[4]
earlier for
birefringent crystals
If
further,
one setsps’= pi == P
then the usual Brillouinequation
results.In the usual derivation this
simplification
isusually
made inequation (4).
Discussion of the exact
equation.
- In the caseof an
isotropic
medium(ps
-Pi)
is a second order termarising
from thedispersion
of the medium.Let
pa 2013 pi
=ApiandN-ni
= AnThe second term arises from the fact that the
magnitude
of the momentum of the scatteredphoton
is different from that of the incidentphoton (vs
#vi)
even ifdispersion
isignored.
The lastterm is due to
dispersion
andApi
ispositive
for theanti-Stokes
component
andnegative
for the Stokescomponent. Denoting
themby
AS and S respec-tively,
The linear Brillouin shift
expressed
as the ave-rage Av in
equation (12)
remains the same as inthe usual
approximation.
But thequadratic
Brillouin shift
given by equation (14)
leads tounequal displacements
of the anti-Stokes and Stokescomponents,
the formerbeing larger
in fre-quency units. This is more
conveniently
expres- sed as apositive
shiftAvQ
of the averagefrequency
of the two
components
vQ withrespect
to the fre-quency vi.
Expressing
the shifts inwavelength
unitsIt is remarkable that the average
wavelength
ofthe two
components
xQ is alsolarger
than Xi sothat both
AXQ
andAVQ
arepositive.
Backward
scattering
and diamond. -- In thecase of backward
scattering
0 =180°,
the Brillouin shift and theasymmetric quadratic
term are bothlargest.
Even the exactequation (6) simplifies
to
Since the second order term could
only
beexperi- mentally
measuredwhen P
islarge,
diamond isextremely
favorable for such a test. On accountof the
exceptionally large velocity
of sound wavesin it and its
high
refractiveindex,
the Brillouincomponents
have been recordedby
Krishnan[1]
and the author
[3].
Using
the elastic constants of diamond[7],
wehave calculated in the
following
table I theexpected
shifts
using equation (15)
for the twowavelengths corresponding
to the gas laser andHg
198 reso-nance radiation :
p = 3.512
g/cm3, velocity
oflongitudinal
wave(L)
= 18 562mls along
the[111]
direction.Velocity
of transverse wave(T)
= 12 038m/s.
One notices that the anti-Stokes and Stokes shift differ
appreciably by
as much as 5 mK in the most favorable case. Thisquadratic
Brillouin effect is withinexperimental
means in view of modern pre- cisions of 5003BC-Å
or 0.4 mK attainable even in absolutewavelengths [8-9] : further,
this effect asmeasured
by AVQ
is different for the transverse andongitudinal components.
Thispermits
an accu-rate measurement even when the incident radia- tion is absorbed
by
a resonance filter in the scat- teredpath.
The
dis
ersion termvi
dn is racticall ne li- Thedispersion term - its practically negli-
ni d v p Y
gible
at 6328 A
but isappreciable
at 2 537A
andthis may also be
possibly
measured.Collimation effects. - If there is a finite diver- gence in the incident beam of A6 and a similar
divergence
in the scatteredbeam,
then theangle
of
scattering
varies between 1800 and1800 + AO/n
since the
divergence
inside thecrystal
is effective for backwardscattering ;
the first order effecton Brillouin shift is zero. In the second
order,
the
change
in shiftFor A6 = 10 this width amounts to
only
0.00008 crn7l. Further this
broadening
is sym- metrical towards v; and hence the effect of thison AVQ
is zero.Comparison
with relativisticDoppler
effect. --The Brillouin shift may be
interpreted [10]
as aDoppler
effectarising
from reflections oflight
waves
by progressive
sound waves.Extending
this
idea,
it isinteresting
to compare thequadratic
Brillouin effect to the
asymmetric
term in the rela- tivisticDoppler
shift[11],
TheDoppler
shifts oflight
emittedby
an atommoving
with avelocity
v
at anangle
00 to the observation directionare
given by
The
subscripts
B and R indicate blue and red shiftsrespectively.
Remembering
that in Brillouin effect the " mo-ving
mirror " isequivalent
to both the source andthe observer are
moving, p
inequations (21)
and(22)
must bereplaced by 2p;.
Then these equa- tions agree with(15)
and(16) respectively
if onesets 0 = 1800 in them and
ignores
thedispersion
term in
(16).
This demonstrates thevalidity
ofthe
analogy
and indicates that the observation of thequadratic
Brillouin effect in diamond would be658
TABLE I
a test of the
special theory
ofrelativity applied
toa
dispersive
medium.In conclusion the author wishes to express his thanks to Dr.
Oksengorn
for this kind interest.Discussion
M. BURSTEIN. - What are the widths of Brillouin
components ?
It would seem to me thatin
existing data,
the widthprobably
arises from the finite solidangle
subtendedby
the lens that collects the scattered radiation.’
The use of lasers should enable one to obtain detailed information about the widths of the Brillouin
components, including temperature
de-pendance
which should in term lead to information about thescattering
of acousticphonons
as a func-tion of
frequency,
up tokilomegacycle frequencies
as a function of
temperature
for a widevariety
ofmaterials,
which otherwise could not be studiedby kilomegacycle
acoustics. Also athigher temper-
rature it should
perhaps
bepossible
to observe"
higher
order Brillouinscattering " involving phonon-phonon
interactions.REFERENCES
[1] KRISHNAN (R. S.), Proc. Ind. Acad. Sc., 1947, A 26,
339.
[2] KRISHNAN (R. S.) and CHANDRASEKHARAN (V.), Proc.
Ind. Acad. Sc., 1950, A 31, 427.
[3] CHANDRASEKHARAN (V.), Proc. Ind. Acad. Sc., 1950, A 32, 379.
[4] CHANDRASEKHARAN (V.), Proc. Ind. Acad. Sc., 1951,
A 33, 183.
[5] KRISHNAN (R. S.), Proc. Ind. Acad. Sc., 1955, A 41,
91.
[6] CHIAO (R. Y.), TOWNES (Ch.) and STOICHEFF (B.
P.),
Phys. Rev. Letters, 1964, 12, 592.[7] McSKIMIN (H. J.) and BOND (W. L.), Phys. Rev., 1957, 105, 116.
[8] SCHWEITZER (W. G.), J. O. S. A., 1963, 53, 1055.
[9] KAUFMAN (V.), J. O. S. A., 1962, 52, 866.
[10] BRILLOUIN (L.), Ann. Physique, 1922, 17, 88.
[11] MANDELBERG (H. I.) and WATTEN (L.), J. O. S. A., 1962, 52, 529.