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Traversal Time as a Function of the Size of the Wavepacket
J. Ruiz, M. Ortuño, E. Cuevas, V. Gasparian
To cite this version:
J. Ruiz, M. Ortuño, E. Cuevas, V. Gasparian. Traversal Time as a Function of the Size of the Wavepacket. Journal de Physique I, EDP Sciences, 1997, 7 (5), pp.653-661. �10.1051/jp1:1997182�.
�jpa-00247351�
Traversal Time
as aFuuction of the Size of the Wavepacket
J. Ruiz
(~,*),
M.0rtuilo (~),
E.Cuevas (~)
and V.Gasparian (~)
(~)
Departamento
deFisica,
Universidad de lvfurcia, Murcia,Spain
(~)Department
ofPhysics,
University ofYerevan,
Yerevan, Armenia(Received
29July
1996, received in final form 22January 1997,
accepted 28Jauuary 1997)
PACS.41.20.Jb
Electromagnetic
wavepropagation;
radiowavepropagation PACS.42.25.-p
Waveoptics
Abstract. We calculate
numerically
the transmission coefficient and the traversal time for finite Gaussianwavepackets
as a function of their widths. We considerelectromagnetic
wavescrossing
a slab and aperiodic
structure. We find that the periodic structure can be crossed atsuperluminal
velocities for wavenumbers in theoptical
gap and sizeslarger
than the thickness of the system. Thecorresponding
transmission coefficients are very small. Thelong
wavepacketlimit of the traversal time coincides with
previous analytical
results for the real component of the interaction time. Theimaginary
component of this timeonly
affects thechange
in size of the wavepacket.The
question
of the time spentby
aparticle
in agiven region
of space has received agreat
deal of interestrecently [1-5].
The final transmissionamplitude through
aregion
is the super-position
of differentpaths,
due tomultiple
reflectionsand/or
topartial
wavescrossing along
differenttrajectories.
Eachpath corresponds
to a different traversaltime,
and so interference effects maydrastically change
the final traversal time. Theproblem
has beenapproached
frommany different
points
ofviews,
as shown in the recent review on thesubject by
Landauer and Martin[I].
One can associate the traversal time with the time
during
which a transmittedparticle
interacts with the
region
ofinterest~
as measuredby
somephysical
clock which can detect theparticle~s
presence in theregion.
Forelectrons,
thisapproach
can utilize the Larmorprecession frequency
of thespin, produced by
a weakmagnetic
fieldacting
within the barrierregion,
as firstproposed by
Baz'[6j.
The amount ofprecession
clocks the characteristictunneling
time rr, the so-called Bfittiker-Landauer time[7, 8].
Forelectromagnetic
waves, weproposed
anoptical
clock based onFaraday
rotation[9j.
The most direct method to calculate the traversal time of a
particle through
aregion
is to follow the behavior of awavepacket
and determine thedelay
due to the structure of theregion.
In thisapproach
one has to be careful with theinterpretation
of theresults, since~
for
example,
anemerging peak
is notnecessarily
related to the incidentpeak
in a causative way[10].
For more discussion of thisproblem
see e.g.[llj
and references therein. Martin andLandauer
[12]
studied theproblem
of the traversal time of classical evanescentelectromagnetic
waves
by following
the behavior of a1N.avepacket
in awaveguide.
(*)Author
for correspondence(e-mail: jrmtlfcu.um.es)
@
Les(ditions
dePhysique
1997654 JOURNAL DE
PHYSIQUE
I N°5One of the most
interesting
aspects of thisproblem
is thepossibility
ofachieving superluminal
velocities with evanescent waves. Nimtz's group was the first one to measuresuperluminal
velocities[13]. They
concentrate onexperiments
on microwave transmissionthrough
undersizedwaveguides. Steinberg
et al. foundsuperluminal
velocities forelectromagnetic
waves in thephotonic
band gap ofmultilayer
dielectric mirrors[14j. Spielman
et al.[lsj
observe that the barrier traversal time ofelectromagnetic wavepacket
tends to becomeindependent
of the barrier thickness for opaque barriers. Thisphenomena closely
relates with the Hartmans theoreticalprediction
for the electrontunneling [16j.
One controversial aspect of this
problem
is thecomplex
nature of the traversaltime,
which arises both for electrons and for classicalelectromagnetic
waves. Sokolovski and Baskin[17]
obtained a
complex
traversal time with theFeynman path-integral technique. They
define a functional that measures the time spentby
aFeynman path
in aregion
and then sum thisquantity
over allpossible paths
with theweighting eis/~,
where S is the action. In theoptical clock,
the realpart
of the time is related to theangle
ofrotation,
while theimaginary
part isrelated to the
ellipticity.
Differentphenomena
can be associated with one of thecomponents
of time. One of the aims of this paper is to establish therelationship
between thecomponents
of time and thedelay (or acceleration)
of thepeak
and thechange
of width of the transmittedpacket.
In this paper we
study
theproblem
of the timespent by
a classicalelectromagnetic
wavein a slab and in a
layered system
as a function of the size of thewavepacket
when we takeinto account the effects of
multiple
reflections. We simulatenumerically
the time evolution ofa finite size
wavepacket
that crosses theregion
of interest and measure thedelay
of thepeak
of the transmitted wave as a function of the size of theoriginal packet.
We also calculate thechange
in size of thepacket.
1. Method of Calculation
We have a three-dimensional
layered system
with translationalsymmetry
in the Y-Zplane.
We consider N
layers
labeled I=
I,
,
N between two
equal
semi-infinite media with a uniform dielectric constant ~lo. Eachlayer
is characterizedby
an index of refraction ~li. The boundaries of the I-thlayer
aregiven by
xi and zi+i, with xi" 0 and zN+i =
L,
so that theregion
ofinterest
corresponds
to the interval 0 < z < L.Later,
we will concentrate on thespecific examples
of a slab(N
=
I)
and of aperiodic arrangement
oflayers.
A Gaussian
wavepacket
ofspatial
width aI is incident from the left on theregion
of interest.This
packet
is characterizedby
a wavefunction of the form:~(z, t)
=
~
C exp[-(k ko)~/2(/hk)~j
exp[ikz i~tj
dk(1)
where C is a normalization
constant, ko
the centralwavenumber,
~=
ck/no,
c is the vacuumspeed
oflight,
and /hk=
I/viaI
is thespread
of thepacket
in the wavenumber domain.This wavefunction
~(z,t)
can represent one of thecomponents
of either the electric or themagnetic
field. The time evolution of thiswavepacket
isgoverned by
Maxwellequations
with theappropriate boundary
conditions.Nevertheless,
the results aredirectly applicable
to anyother classical
wave and toquantum wavefunctions,
aslong
asdispersion
isneglected.
Part of thepacket
considered is transmitted and continuestraveling
toward theright.
Its wavefunction isgiven by:
~(x~ t)
=
j" cjt(k)
jet<(ki
expj-(k ko)2 /2(/~k).2j
expjikx iwti
dk(2)
t(k)
is theamplitude
of transmission and#(k)
itsphase.
As the two semi-infinite mediaare
non-dispersive,
thewavepacket
travels with a well-definedvelocity
in both of them. Wenumerically
simulate this time evolution of thewavepacket
and calculate the time takenby
thepacket
to cross theregion
of interest. Inparticular~
we measure the averagepositions
Ii and Y2 of the square of the modulus of thewavepacket
at two values oft,
ti andt2,
such that thepacket
is very far to the left of the structure atti
and very far to theright
at t2. Theseaverage
positions
are defined asTit)
=/~ xi i~lz, t)
i~ dz. 13)
The traversal time of the
wavepacket through
theregion
of interest isequal
to:r = t2 ti ~~~ ~~
~~~°
(4)
c
We also measure the standard deviation of the transmitted
wavepacket.
We
systematically study
the behavior of the traversal time as a function of the central wavenumberko
and of the size aI of thepacket.
We can obtain closeexpressions
for the timein the two extreme cases of very
long
and very shortwavepackets,
ascompared
with L. In aprevious work,
we obtained the traversal time for verylong wavepackets
in terms of derivatives withrespect
tofrequency
as[9j:
T # -I
~~~~ j
0w w
(5)
where r is the
amplitude
of reflection of theregion
considered. As we will see, the real part of thiscomplex
time is associated with the traversaltime,
aspreviously defined,
and theimaginary part
is related to the shift in the central wavenumberko.
The derivative of the time with respect tofrequency
is associated with the distortion of thewavepacket.
2. Results for a Slab
Let us first consider a slab confined to the
segment
0 < z < L and characterizedby
an index of refractionn. The transmission
amplitude
t of the slab isgiven by [18j:
y~2 y~2 2
~~~
t = I + ° sin u
exp(itfi), (6)
2nno
and the
phase
ifiby
~~~'~ ~~~~~
~~~~' ~~~where u
=
wnL/c.
The reflectionamplitude
r isequal
to:(y~j
~2)
~ ~~
2non
~~~~' ~~~Substituting
theseexpressions
for t and r inequation (5)
we obtain for the two timecomponents
in thelimiting
case oflong wavepackets
thefollowing:
~~ ~
2cno
~4nnow
~~~~~ ' ~~~656 JOURNAL DE
PHYSIQUE
I N°5o 10
.00
Fig.
1. Ti and T2 as a function of k forlong wavepackets crossing
a slab. The values of the parameters are L= 10, n = 2 and no
= 1. We choose c
= 1. The dot corresponds to k
=
81ir/80,
the square to k =
41ir/40
and thetriangle
to k=
21ir/20.
The horizontal line represents the average value of Ti with respect to k.and
T2 =
T~
'~° ~ ~ ~°sin~
u +
~~~ ~°~
sin 2u
(10)
nno~ wnn~ cno
~where T
=
jtj~
is the transmission coefficient.Throughout
the paper, Ti and T2 will represent the real andimaginary parts
of T in thelong wavepacket limit,
definedby equation (5).
In
Figure
I we represent Ti and T2,given by equations (9, 10),
as a function of k. The width of the slab considered is L= 10 and its index of refraction is
equal
to2,
while the index of refraction outside the slab is I. We choose c= I. In some wavenumber ranges, the
oscillatory
character of the second term on the RHS ofequations (9, 10)
results in traversaltimes
significantly
smaller than the onecorresponding
tocrossing
the slab at the groupvelocity
in the medium. The three
symbols
represent the value of Ti for each of the wavectors considered in the nextfigure.
The horizontal linecorresponds
to the average value of Ti withrespect
to k.In the lower
part
ofFigure
2 we show the results of the numerical simulations of the traversaltime versus the size of the
wavepacket
for three different values of the central1i>avenumber,
k =
81ir/80,
41ir/40
and 21ir/20.
These wavenumbers are chosen so that sin 2u=
1,
sin u= 1
and sin u
=
0,
and so Ti is a centralvalue,
a minimum and amaximum, respectively.
We can check that thelong wavepacket
limit of these resultscorresponds
to Ti,given by equation (9).
In the lower
part
ofFigure
2 we represent the transmission coefficient for the same situationas in the upper
part
of thefigure.
We can note thesimilarity
in the behaviour of the traversal time and of the transmission coefficient.The short
pulse
limits areequal
to20.8, independently
of the central wavenumber considered.This value is the classical
crossing time, taking
into accountmultiple reflection,
which for1.00
0.90
~=
0.80 ~-'-
0.70
0.60
24.0
22.0 :.."
~
20.0 "'---_____
18.0
16.0
io ioo iooo
q
Fig.
2. Traversal time(lower graph)
and transmission coefficient(upper graph)
versus the size of thewavepacket
for three different values ofthe central wavenumber, k =81r/80 (dashed line), 41ir/40 (solid line)
and21ir/20 (dotted line).
The values of the parameters are the same as inFigure
1.the slab is
given by:
The transition between the two limits
I.e. the width of the slab.
We
can calculate theaverage
of riexactly and
check that it is equalto
Ln/c,sponds
to
the classicalcrossing time ithout ncluding reflection, I.e., to the
time
3. Periodic Structure
We now consider a
periodic arrangement
oflayers. Layers
with index of refraction ni and thicknessdi
alternate withlayers
of index of refraction n2 and thicknessd2
The wavenumbers in thelayers
of the first and second type areki
"wni/c
andk2
"wn2/c.
Let us call a to thespatial period,
so a=
di
+d2.
Theperiodicity
of thesystem
allows us to obtainanalytically
the transmission
amplitude using
the characteristic determinant method[19j:
tN
"e~'~i~i cos(Nfla/2)
I~~~~~~~~~~ sin~ pa
+~~
~~sin
2d2j
~,
(12)
sin
pa
2ki
k2~
658 JOURNAL DE
PHYSIQUE
I N°51.oo
0.75
~ 0.50
0.25
iso
~~
100
50 F'
o ..-...:. ..."..,_,:~'~:
___~___
.,_:."... ..:... ....-..
50 ~c
""~
100
3.0 3.5 4.0 4.5 5.0
k
Fig.
3. Transmission coefficient(upper graph)
and Ti(solid
line, lowergraph)
and T2(dotted
line, lowergraph)
as a function of k forlong wavepackets crossing
aperiodic
system with N= 20 interfaces.
The horizontal line corresponds to the average value of Ti with respect to k.
where
fl plays
the role ofquasimomentum
of thesystem,
and is definedby
cos
pa
= coskidi
cosk2d2 ~~/ k2~
~~ sinkidi
sink2d2 (13)
When the modulus of the RHS of
equation (13)
isgreater
thanI, fl
has to be taken asimaginary.
This situation
corresponds
to a forbiddenfrequency
window.We concentrate in the
simplest periodic
case, whichcorresponds
to the choicenidi
=
n2d2
This case contains most of the
physics
of theproblem
and is also used in mostexperimental setups [14].
We consider asystem
of19layers IN
=
20)
withalternating
indices of refraction of 2 andI,
and widths of 0.6 and1.2, respectively.
InFigure
3 werepresent
Ti and T2 for thissystem
as a function of k. In theoptical
gaps, the traversal times aresignificantly
smaller than thecrossing
time as the vacuumspeed
oflight equal
to 16.8. The twobig
dotscorrespond
to the value of Ti of the two wavectors considered in the nextfigure,
The average of Ti withrespect
lE+o
iE-i
lE-2
~ lE-3
E.4
E-5
ioo
~
ioi
o-i i-o io,o ioo.o iooo.o
q
Fig.
4. Transmission coefficient(upper graph)
and traversal time(lower graph)
versus the size of the wavepacket for two values of the central wavenumber, k= 3.927
(solid line)
and 4.3(dashed line).
The values of the parameters are the same as in
Figure
3.to wavenumber is
equal
to 22.8(horizontal line),
and coincide8 with the classicalcros8ing
time withoutincluding multiple
reflections.In the lower
part
ofFigure
4 werepresent
the traversal time versus the size of thewavepacket
for two values of the centralwavenumber,
3.927 and 4.306. These wavenumberscorrespond
tothe center of the gap and to a resonance. The time needed to cross the
system
at the vacuumspeed
oflight
isequal
to 16.8. In the upperpart
of thefigure
we show the transmission coefficient for the same cases as in the lowerpart.
We can note thesimilarity
in the behaviour of the traversal time and of the transmission coefficient.Again
thelong wavepacket
limit of thetraversal time coincides with Ti, while the short
wavepacket
limit isindependent
of wavenumber andequal
to 29. In the case ofelectromagnetic
wavestunneling trough
undersizedwaveguides analogous
results were obtained[20j.
We
always
haveinterference,
even forextremely
shortwavepackets,
betweenpath
corre-sponding
to the same traversal time. Forstrictly periodic
structures we can neverreach
660 JOURNAL DE
PHYSIQUE
I N°5ioo
io
io ioo iooo
q
Fig.
5.al a~
asa function of the size of the wavepacket. The values of the parameters are the
same as in
Figure
3.the classical
limit,
with no interference effects. Forexample
the N Ipaths consisting
on two successive reflectionsland
transmission in all otherinterfaces)
all add upconstructively.
The ratio between theheights
of the first and the second transmittedpeaks
isequal
to(N -1)~ (R(
~,where
(R(
is the reflectioncoefficient,
instead of(N I)jRj~,
result that one wouldexpect
in the absence of interference.We note that the
speed
issuperluminal
for a wide range of sizes. The minimum size of thepackets
that travel faster thanlight
is about9,
so that thecorresponding 2aI
is very much thesame as the size of the system.
Superluminal
velocities occur when the transmission coefficient is very small. We are at presentinvestigating
thisrelationship.
In the
optical
gap, the width of the transmittedpacket
aT isslightly
smaller than the width of the incidentpacket
aI.Up
to second order inperturbation theory,
we obtain that thischange
in widthdepends
on the derivatives with respect tofrequency
of Ti and T2. As the first of these derivatives isequal
to zero in the centre of the gap, we arrive at:In
Figure
5 weplot al a(
as a function of the size of thepacket.
Thelong wavepacket
limit agrees very well with 11
/2)(dT2/dw),
obtained from the characteristicdeterminant,
and which isequal
to 36.7. We check that second orderperturbation theory
worksadequately
for the sizes for which one obtainssuperluminal
velocities.4. Discussion
Our results
apply
to anynon-dispersive
wave. The real component oftime,
Ti,corresponds
to the traversaltime,
and the main effect of theimaginary
component, T2, is tochange
the size of thewavepacket.
In thedispersive
case there is a correction to the traversal time due to theshift in wavenumber
produced by
T2.Acknowledgments
We would like to thank G. Nimtz for
helpful
discussion and criticalreading
of themanuscript,
the Direcc16n General de
Investigac16n
Cientifica yTAcnica, project
number PB93/l125,
andNATO,
Collaborative Research Grant OUTR.CRG951228,
for financialsupport.
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