After my undergraduate Physics studies
at the University of Paris-Sud XI in
Orsay, France, I was a postgraduate student at the University of Caen in Normandy, France.
I obtained my PhD in 1996 at the Grand Accélérateur National
d'Ions Lourds (GANIL) in Caen on high-precision
direct mass measurements of very exotic nuclei.
The
mass of doubly-magic 100Sn
An innovative experiment using the
CSS2 cyclotron at GANIL as a high-resolution spectrometer [1,2]
led to the production and identification of the very exotic nucleus 100Sn
with the 50Cr + 58Ni fusion-evaporation reaction at
255 MeV and to its mass-measurement for the first time [3]. The understanding
of this doubly-magic N = Z nucleus is one of the cornerstones on which nuclear
structure models depend. It was discovered in 1994 at GSI, Germany, and GANIL, France.
By analogy with electrons in the
atom, the nucleons (protons and neutrons) in the nucleus are organised into
energy levels or shells. These shells can only accept a certain number of
nucleons and, each time a shell is filled, the nucleus becomes more tightly
bound and more difficult to excite than others. These numbers (2, 8, 20, 28,
50, 82 and 126) discovered in 1949 are called the magic numbers of the nuclear
shell model. By analogy with atoms, magic nuclei are similar to the noble-gas
atoms of the Mendeleiev periodic table of the elements. 100Sn
with its 50 neutrons and 50 protons is called doubly-magic and is one of
a dozen nuclei to have both magic numbers for protons and neutrons,
which should greatly strengthen its stability. Of bound nuclei which have
the same numbers of neutrons as protons 100Sn is the heaviest
and most exotic. It is an extreme case where its magicity competes with its
exoticity.
The masses of neutron-deficient nuclei in the mass region A = 60
- 80
The direct time-of-flight technique
using the SPEG magnetic
spectrometer at GANIL was extended to
the mass measurement of neutron-deficient nuclei near the N = Z line such
as 66As, 68,70,71Se and 71Br [4,5] which
are in a region known to provide input for the modelling of the rp-process
(rapid proton capture) in nuclear astrophysics and information relevant to
nuclear structure in a region of high deformation. Radioactive secondary
beams were produced via the fragmentation of a high-energy high-intensity
78Kr beam on a natNi target, using the SISSI device.
After my PhD, I took a two-year
post-doctoral appointment jointly held between the National Superconducting
Cyclotron Laboratory (NSCL) at Michigan State University (MSU) and the Oak
Ridge National Laboratory (ORNL), USA,
to focus on the study of the structure of light exotic nuclei, in particular
nuclei showing a halo structure and unbound nuclei.
The ground-state of unbound 10Li
I studied the break-up of the one-neutron
halo nucleus 11Be in 10Li + p by measuring the 9Li
fragments in coincidence with 2.7 MeV gamma-rays (corresponding to the 9Li
first excited state) which were detected in anarray of 90 BaF2
detectors. These data provided information on the structure of the unbound-nucleus
10Li through the valence-neutron interaction with the 9Li
nucleus and showed evidence for a parity inversion in 10Li leading
to a dominant s-wave (l = 0) ground state [6]. The results of this experiment
are essential to a proper description of the three-body Borromean system
11Li, one of the most interesting of halo nuclei. Another similar
experiment showed evidence for an l = 0 ground state in unbound 9He
[7]. The secondary radioactive beam of 11Be was produced by fragmentation
of a 13C primary beam and purified in the A1200 spectrometer at
the NSCL.
Following my post-doctoral position
in the USA, I became in 1998 a Physics Lecturer at the University of Bordeaux
1 within the Centre d'Etudes Nucléaires de Bordeaux-Gradignan
(CENBG), France, where I have extended
my research activities to the spectroscopy of nuclei at the proton drip-line.
The two-proton radioactivity, that
is to say the emission of a 2He nucleus from the ground state
of a nucleus for which the emission of a single proton is energetically forbidden
has been predicted nearly forty years ago but is yet to be observed. From
mass predictions 45Fe and 48Ni are the best candidates
for this new radioactivity. With this aim, a projectile-fragmentation experiment
was recently performed at GANIL with the
LISE3 spectrometer that
led to the discovery of doubly-magic 48Ni [8]. Consequent
experimentswere
performed at GANIL and at GSI on the FRS fragment separator, to search for
two-proton radioactivity of 45Fe and 48Ni.
Odd-odd N = Z nuclei such as 62Ga
are good candidates to extend the test of the Conserved Vector Current hypothesis
and probe physics beyond the Standard Model of the weak interaction. These
nuclei have 0+ ground states and decay by super-allowed Fermi beta-decay.
The log ft values of these 0+ to 0+ transitions are
used to determine the dominant matrix element of the Cabbibo-Kobayashi-Maskawa
matrix which links the quark eigenstates to their mass eigenstates. To obtain
the log ft values, high precision beta-decay half-lives and Q-values are needed.
As these transitions are ground-state to ground-state transitions, the Q-values
can be determined by measuring the masses of parent and daughter nuclei.
I collaborate in experiments at the IGISOL facility
in Jyväskylä, Finland, and
at the on-line mass separator
at GSI which aim to perform detailed studies
of the decay
of 62Ga as well as the precise measurement of its half-life.
The discovery of two-proton radioacivity
At the limits of extremely proton-rich
nuclei, the direct emission of protons becomes the dominant decay mode and
ultimately defines one of the boundaries of observable nuclei in the N-Z plane.
In 2002 a new radioactive decay mode was discovered at GANIL and GSI: the
ground state two-proton emission from the nuclide 45Fe. Physicists also
plan to the search for this decay mode in another good candidate: the
doubly-magic nucleus 48Ni that was recently discovered at GANIL. These nuclei
can emit a di-proton, but are forbidden from expelling a single proton. An
interesting challenge for future research is to confirm whether or not the
protons are emitted as a 2He, which then breaks up. Theorists predicted this
new type of radioactivity forty years ago. Recent progress in the delivery
of secondary radioactive ion beams made these discoveries possible.
How to measure atomic masses
precisely? A direct mass measurement method using a cyclotron
The masses of heavy N =
Z nuclei
A new direct mass-measurement
method using the CIME cyclotron
The masses of neutron-deficient
argon isotopes
Mass measurements of very short-lived
exotic nuclei can be performed with the CSS2 cyclotron of GANIL and the new CIME
cyclotron of SPIRAL
which are complementary to those possible using the Penning trap of ISOLTRAP or the radio-frequency
spectrometer MISTRAL,
both at CERN/ISOLDE (Switzerland),
or the ESR storage
ring at GSI. An experimental proposal, of
which I am spokesperson, has recently been approved beam time in order to
develop and test the new CIME method, as well as to measure, with a precision
better than 10-6, the masses of 31,32Ar radioactive
isotopes delivered by SPIRAL.
1. G. Auger et al, Nucl. Instr.
Meth. A 350 (1994) 235.
2. M. Chartier et al, Nucl. Instr.
Meth. B 126 (1997) 334.
3. M. Chartier et al, Phys. Rev. Lett.
77 (1996) 2400.
4. M. Chartier et al, Nucl. Phys.
A 637 (1998) 3.
5. G.F. Lima et al, to appear in Phys.
Rev. C.
6. M. Chartier et al, Phys. Lett.
B 510 (2001) 24.
7. L. Chen et al, Phys. Lett.
B 505 (2001) 21.
8. B. Blank et al, Phys. Rev. Lett.
84 (2000) 1116.