A NNALES DE L ’I. H. P., SECTION A
J. C. L E G UILLOU J. L. B ASDEVANT
Crossing and experimental ππ S and P waves
Annales de l’I. H. P., section A, tome 17, n
o3 (1972), p. 221-226
<http://www.numdam.org/item?id=AIHPA_1972__17_3_221_0>
© Gauthier-Villars, 1972, tous droits réservés.
L’accès aux archives de la revue « Annales de l’I. H. P., section A » implique l’accord avec les conditions générales d’utilisation (http://www.numdam.
org/conditions). Toute utilisation commerciale ou impression systématique est constitutive d’une infraction pénale. Toute copie ou impression de ce fichier doit contenir la présente mention de copyright.
Article numérisé dans le cadre du programme Numérisation de documents anciens mathématiques
http://www.numdam.org/
221
Crossing and experimental 03C003C0 S and P
wavesJ. C. LE GUILLOU
J. L. BASDEVANT
Laboratoire de Physique atomique et moleculaire, College de France, Paris
C. E. R. N., Geneva
Vol. XVII, no 3, 1972, p. Physique théorique.
ABSTRACT. - We test the
crossing properties
of fits toexperimental
s-and p-wave 03C003C0
phases
of Baton et al.[1], using
theequations
ofRoy [2],
obtained from fixed t
dispersion
relations. A sum rule for thescattering lengths
ao and a2 is alsoused,
in which theasymptotic
contribution is animportant ingredient. Then,
our main conclusions are that :a. the method appears to be very
precise
and useful;b. if one believes
strictly
in the0 ~ o
of Baton thescattering lengths disagree
withWeinberg’s predictions
but ao agrees with the recent Ke~indications;
c. if
o~
is lower than Baton’svalues, acceptable agreement
withWeinberg’s predictions
can be achieved.RÉSUMÉ. - On teste les
proprietes
de croisement de fits a desdephasages experimentaux
de Baton et coll.[ 1]
pour les ondes s et p, en utilisant lesequations
deRoy [2]
obtenues par des relations dedispersion
a tfixe. Une
regle
de somme pour leslongueurs
de diffusion ao et a2 est aussiutilisee,
danslaquelle
la contributionasymptotique
est uningredient important.
Nos conclusionsprincipales
sont alors que :a. la methode s’avere tres
precise
et utile;b. si l’on croit strictement au
(~
de Baton leslongueurs
de diffusion sont en désaccord avec lespredictions
deWeinberg,
mais ao est enaccord avec les recentes indications de Ke’;
c. si
o~
estplus
bas que les valeurs de Baton, un accordacceptable.
avec les
predictions
deWeinberg peut
etre obtenu.222 J. C. LE GUILLOU AND J. L. BASDEVANT
Recently, Roy
has writtenequations
for 03C003C0partial
waveamplitudes [2J starting
from fixed momentum transferdispersion
relations. Theseequations
express thecrossing
andanalyticity properties
of the 1!1!amplitude directly
in terms ofphysical region amplitudes,
and this fact makes them veryinteresting
forperforming
low energy Tryrphenome- nology,
as we haveargued
elsewhere[3].
In this note we
report
the results of thefollowing investigation.
Wewant to know to what extent the
existing
data on 03C003C0scattering [ 1]
allow to determine the values of the s-waves
scattering lengths,
if oneuses
Roy’s equations
toperform
theanalytic
continuation down to threshold.Roy’s crossing equations
forphysical partial
waveamplitudes
areof the form
[3] :
The subtraction terms S. T. are
present
in s-waves and p-wave,they
arelinear
polynomials
in s whose coefficients are determinedby
the two scat-tering lengths
ao and Q2. Theexplicit
form ofEquation (1)
isgiven
in Reference
[3].
As shown in reference[3],
it is agood approximation
for s
L m’P
to retainonly
the contributions of s- and p-waveabsorptive parts
in theright
hand side ofEquation (1).
Also, the kernels G(s, s’)
are
highly convergent
in s’ and one may restrict theintegration
range 115. We concentrate on the s- and p-waveequations (I
= 0,1)
and
require consistency
between RHS and LHS ofEquation (1)
at lowenergies (s m~).
Good
experimental
Trrr s- and p-wavephase
shifts are available between 500 and 1000 MeV[1] (with
the well-knownup-down ambiguity
in I =0).
Our aim is to continue the
phases
down to thresholdby
some flexibleform and to fix the
parameters through
theconsistency
relations(1).
Here, the
imaginary part
of the 1=1 p-wave isparametrized
asin Reference
[4] (the
realpart being
determinedby
elasticunitarity).
This has the
advantage
ofproducing
an excellent fit toexperiment (with
m? = 767 MeV andr p
= 135MeV)
for alarge
range of value of thearbitrary parameter
ai - the p-wavescattering length
-.we choose for the I = 0,2 s-waves the
unitary
formand the K-matrix is
parametrized
as follows.(i)
In theexperimental
rangesI ~ s ~ 50 (81
>13)
we use the fitsto the
experimental
results of Baton el al.[ 1] (either
« up » or « down » solution for1=0) (see fig. 1);
Fig. 1. - S-wave ’r.7C phase-shifts (Experimental data are from [1]) :
I = 0 : Curve (a) [resp. (b)] : fit to experimental data for the « up »
[resp. « down »] 8g phase-shift;
Curve (c) : phase-shift corresponding to the curves of figure 2.
I = 2 : Curve (a’) : fit to experimental data;
Curve (b’) : phase-shift corresponding to the curves of figure 2.
(ii)
For s > 50 we use the continuation of theprevious expression-this
does not
play a
crucial role,owing
toquick
convergence of the s’ inte-gration ;
(iii)
In the low energyregion 4 L
s L§~
we use the flexible form224 J. C. LE GUILLOU AND J. L. BASDEVANT
The
joining
of thisexpression
to the fit toexperimental
data foris realized
by requiring continuity
of theexpression
and of its derivative at s = SI; this determines two of the threeparameters AI, BI,
CI ineach channel. We have noticed
that so, the joining point
in I =0,
isan
important parameter,
while the results are rather insensitive to S2 which was taken to be S2 = 16. Inletting
So vary, we allow ourselves toneglect
the first few I = 0experimental points
which may have small statisticalsignificance [1].
At thisstage,
we have fourparameters :
the three s- and p-wave
scattering lengths
ao, a2, ai, and theposition so
of
the joining point
in I = 0.For each set
(a2, so)
we first determine ao and aiby satisfying
thedispersion
sum rules(5) :
where FI - Fr
(s’,
t =0)
are the forward totalamplitudes.
InEquation (4)
the kernel decreases as S’-3 and it would be agood approxi-
mation to retain
only
s- and p-wave contributions. InEquation (5)
however, one has to take care ofhigher
waves( fo resonance)
and asymp- totic contributions(Reggeized p-exchange).
As in Reference[4],
weuse the
Reggeized p-parameters given by pole extrapolation
with ascale
parameter
of 0.8(Ge V)2,
and this leads to a total contribution of l ~ 2 andasymptotic
terms to the RHS ofEquation (5)
of[4]
~ 0. 23. We insist that this is an
important ingredient
in thepresent analysis :
it is clear that once a2 isfixed,
aodepends directly
on the value of the
asymptotic
contributions toEquation (5)
for whichwe have made a choice which seems reasonable but is
certainly
notcompulsory
atpresent.
We then vary the two
parameters
a2 and so,keeping
theexperimental
fits
o and 03B420
in as indicated in(i)
above, and retainonly
the values of a2 and So which lead toacceptable agreement
betweenRHS and LHS of
Equation (1)
in thelow-energy region
Owing
to the crudeness of ourparametrization,
we considersatisfactory
to
have
LHS -RHS 1/1 RHS ~ ~
10%
for smp.
We may remark that we are not concerned withsolving
the «up-down » ambiguity
fors >
mp (all
our conclusions hold in eithercase),
which wouldrequire
a local
investigation
of theequations
for s ~Also,
we noticethat subthreshold zeroes
(which
may become zeroes above threshold foro~
if a2 >0)
arealways present
in s-waveamplitudes;
this is relateddirectly
to the fact that in theexperimental region ~o
ando~
are ofopposite signs.
The results can be summarized as follows :
1. If we restrict ourselves to the fit of
o~
asgiven by
Baton et al.[1],
it appears that the
only acceptable
solutionsrequire
apositive
I = 2scattering length
0.04 -0.08).
Thecorresponding
I = 0 scat-tering length
is thenquite large (ao
~ 0. 5 or0.6)
and not well cons-Fig. 2. - Example of solution with a2 = - 0. 04 and ao = 0. 21. Solid curves : direct calculations; dashed curves : as computed through RHS of Equa-
tion (1).
trained. This result for ao would be in
good agreement
with the recentK e4 data
[7] (ao
rv0. 6 + 0. 25).
However we have a violentdisagree-
ment with the
generally
assumedpredictions
ofWeinberg [8]
or of theLovelace-Veneziano model
[6].
2. In
analysing
the reason for thiseffect,
we found that ifo~
couldbe somewhat
larger
in absolute value than the valuegiven by
Batonet al.
[1], things
could be restored. Sincethe on I
of Colton et al.[9]
is indeed somewhat
larger
thanBaton’s,
it ispossible
that somesystematic
error is
present
in the latterexperiment,
and we have allowed for valuesof o,
which would lie at the lower end of Baton’s error bars. It is thenpossible
to recoveragreement
with a2 0(see fig. 2)
and the ranges of the variousparameters
are[o~ being
fors > 13
curve(b’)
offig. 1] :
0.037~~~0.038, -0.05~~~-0.03,
(«
up »case) 0.040 ~ ~ ~ 0.041, -0.04 ~ ~ ~ - 0 . 03 ;
(cc
down »case)
226 J. C. LE GUILLOU AND J. L. BASDEVANT
3. To conclude : it appears that fixed-t
dispersion
relations, in the form ofRoy’s equations,
are a very sensitive and useful tool toinvestigate
the low energy Trrr
amplitude.
We beleive that the correct way to fit(smooth) experimental
data is not to fit each waveseparately,
butall the waves
simultaneously
with such adispersion
relationanalysis.
In
particular,
we think that otherwise anyattempt
to determine thescattering lengths by extrapolation
from theregion
above threshold iscompletely arbitrary.
Our
present simple
mindedinvestigation
isperhaps
not refinedenough
to
give
anunambiguous
answer, and a moregeneral global parametrization
is
certainly
necessary, which would have to take into account morecarefully
contributions from 12 2 waves and inelasticitiestogether
with a use of other
possible
values for theasymptotic
contribution to the sum rule(5) relating
the two s-wavescattering lengths.
Our last remark is that in view of our results, it seems that in order to determine
unambiguously
the low energy 03C003C0 S waves one needsmore information than the
parameters
of the p-meson and the absence of exotic resonances, asopposed
to what was found in other investi-gations [4] using crossing
sum rules inunphysical regions.
ACKNOWLEDGMENTS
We are
grateful
to Drs. J. P. Baton, G. Laurens and J.Reignier
foruseful
discussions,
and forcommunicating
their results.[1] J. P. BATON, G. LAURENS and J. REIGNIER, Phys. Lett., vol. 33 B, 1970, p. 528;
G. LAURENS, Thesis, C. E. A.-N-1497, 1971.
[2] S. M. ROY, Phys. Lett., vol. 36 B, 1971, p. 353.
[3] J. L. BASDEVANT, J. C. LE GUILLOU and H. NAVELET, Nuovo Cimento, vol. 7 A, 1972, p. 363.
[4] J. C. LE GUILLOU, A. MOREL and H. NAVELET, Nuovo Cimento vol. 5 A, 1971, p. 659.
[5] G. WANDERS, Nuovo Cimento, vol. 63 A, 1969, p. 108; M. G. OLSON, Phys. Rev.,
vol. 162, 1967, p. 1338.
[6] C. LOVELACE, Phys. Lett., vol. 28 B, 1968, p. 264; J. SHAPIRO, Phys. Rev., vol. 179, 1969, p. 1345.
[7] A. ZYLBERSZTEJN et al., Phys. Lett., vol. 38 B, 1972, p. 457.
[8] S. WEINBERG, Phys. Rev. Lett., vol. 17, 1966, p. 616.
[9] E. COLTON et al., Phys. Rev., vol. D 3, 1971, p. 2028.
(Manuscrit reçu le 11 juillet 1972.)