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Europhysics News (2002) Vol. 33 No. 1 Quest for superheavy nuclei P.H. Heenen1 and W. Nazarewicz2-4 The discovery of new superheavy nuclei has brought much excitement to the atomic and nuclear physics communities. Hopes of finding regions of long-lived superheavy nuclei, predicted in the early 1960s, have reemerged. Why is this search so important and what new knowledge can it bring? Not every combination of neutrons and protons makes a stable nucleus. Our Earth is home to 81 stable elements, including slightly fewer than 300 stable nuclei. Other nuclei found in nature, although bound to the emission of protons and neutrons, are radioactive. That is, they eventually capture or emit electrons and positrons, alpha particles, or undergo spontaneous fission. Each unstable isotope is characterized by its half-life (T1/2) - the time it takes for half of the sample to decay. Isotope half-lives range from less than a thousandth of a second to billions of years. Many radioactive nuclei may have half-lives comparable to or longer than the age of the Earth (4.5 billion years). Examples are the actinide nuclei 232Th (T1/2=1·1010 years), 235U (T1/2=7·108 years), or 239U (T1/2=4·108 years). Short-lived isotopes cannot be found naturally on Earth because they have long decayed since our planet was formed. Yet, thousands of short-lived isotopes are continually created in the cosmos. Their existence may be fleeting, but they play a crucial role in the ongoing formation of the elements in the Universe. The properties of most rare isotopes are unknown and can be only inferred, with considerable uncertainty, from theoretical calculations. Figure 1 shows bound nuclear systems as a function of their proton number Z (vertical axis) and their neutron number N (horizontal axis). The black squares represent the stable or very long-lived nuclei. They form the so-called "valley of stability". The yellow region indicates shorter-lived nuclei that have been produced and studied in laboratories. By adding either protons or neutrons, one moves away from the valley of stability, finally reaching the drip lines where nuclear binding ends because the forces between neutrons and protons are no longer strong enough to hold these particles together.
Historical Background Still heavier elements (transuraniums) were produced in heavy-ion accelerators by fusing heavy actinide targets (plutonium-californium) with light ions of carbon (nobelium, Z=102, 1958; ruthefordium, Z=104, 1969), boron (lawrencium, Z=103, 1961), neon (dubnium, Z=105, 1967), and oxygen (seaborgium, Z=106, 1974). In order to go heavier, to compensate the decrease of the proton-to-neutron ratio with mass, fusion of nuclei with the largest possible surplus of neutrons had to be used. In the 70s, "cold fusion" reactions involving medium-mass projectiles with Z ≥ 24 and lead or bismuth targets were introduced and replaced "hot fusion" reaction with actinide targets. This enabled the discovery of bohrium (Z=107, 1976), hassium (Z=108, 1984), meitnerium (Z=109, 1982), ununnilium (Z=110, 1994), unununium (Z=111, 1994), and ununbium (Z=112, 1996). The last three elements are still unnamed. So far, they carry temporary names derived directly from the atomic number according to the systematic nomenclature of the International Union of Pure and Applied Chemistry (IUPAC). Most of the heaviest elements were found in three "heavy element factories": Lawrence Berkeley Laboratory in Berkeley (USA), Joint Institute for Nuclear Research in Dubna (Russia), and Gesellschaft für Schwerionenforschung (GSI) near Darmstadt (Germany). After much discussion about the priority for their synthesis, IUPAC 1997 has accepted names up to Z=109. At that time, nuclei with Z=110, 111, and 112, discovered at GSI, were already known. The lifetimes of the heaviest elements were found to be very short. For instance, element Z=112, investigated using the reaction 70Zn + 208Pb -> 277Uub + 1n, turned out to have a half life of only about 280 µsec. The corresponding fusion cross section is extremely small, 1 pb. Since the production cross section was found to be rapidly decreasing with the atomic number, see Fig. 2, it was then concluded that it would be very difficult to reach still heavier elements. As far as theory is concerned, major advances were
made in 1966, when the first realistic theoretical calculations for
the superheavy nuclei were carried out. These early calculations were
based on the shell correction (or: macroscopic-microscopic) method in
which the total binding energy was decomposed into a smooth part (approximated
by a macroscopic liquid drop model) and a microscopic quantal shell
correction term strongly oscillating with the number of nucleons and
reflecting the energy stabilization due to the presence of nucleonic
shells. Such calculations predicted the nucleus with Z=114, N=184
(
Physics at the limit of cross sections is difficult and challenging. The synthesis of the new element Z=118 (293Uuo), announced in 1999 by the Berkeley group, has been retracted two years later. The history of heavy element research remembers other cases of elements discovered and gone, and sometimes discovered again. A team working in Stockholm at the Nobel Institute of Physics reported in 1957 an isotope with atomic number 102. The group proposed the name Nobelium in honor to Alfred Nobel. In 1958 a group at Berkeley reported that they were unable to reproduce this work, findings agreed by a Russian group at Dubna. But the name stuck... Structure of
the superheavy nuclei The stability of heavy and superheavy elements has been a longstanding fundamental question in nuclear science. Theoretically, it has been shown that the mere existence of nuclei with Z > 102 is entirely due to quantal shell effects. Indeed, in the classical liquid drop picture, the shape of a nucleus is governed by an interplay between surface tension (proportional to A2/3, trying to make the nucleus spherical) and Coulomb repulsion (proportional to Z2/A1/3, trying to make the nucleus deformed). At large values of Z2/A, the Coulomb force is so strong that the nuclear liquid drop becomes unstable to surface distortions and it fissions spontaneously. It is the stabilization brought by quantal shell effects that is responsible for the superheavies. In spite of an impressive agreement with experimental data for the heaviest elements, theoretical uncertainties are large when extrapolating to unknown regions of the nuclear chart. In particular, there is no consensus among theorists with regard to the center of the shell stability in the superheavy region. Since in these nuclei the single-particle level density is relatively large, small shifts in the position of single-particle levels (e.g., due to the Coulomb or spin-orbit interaction) can be crucial for determining the shell stability of a nucleus. While most macroscopic-microscopic (non-self-consistent) approaches predict Z=114 to be magic, most self-consistent calculations suggest that the center of the proton shell stability should be moved up to higher proton numbers, Z=120, 124, or 126. For the neutrons, most non- relativistic calculations predict magic gaps at N=184 while the relativistic mean-field theory yields N=172 - due to a slightly different spin-orbit interaction. The experimental determination of superheavy nuclei from this region will thus be of extreme importance for pinning down the fundamental question of the spin-orbit force. Does it actually make sense to talk about "magic superheavy nuclei"? A recent theoretical work [3] sheds a new light on this question. According to calculations, the patterns of single-particle levels are significantly modified in the superheavy elements. Firstly, the overall level density grows with mass number A, as a A1/3. Secondly, no pronounced and uniquely preferred energy gaps appear in the spectrum. This shows that shell closures which are to be associated with large gaps in the spectrum are not robust in superheavy nuclei. Indeed, the theory predicts that beyond Z= 82 and N= 126 the usual localization of shell effects at magic numbers is basically gone. Instead the theory predicts fairly wide areas of large shell stabilization without magic gaps. This is good news for experimentalists: there is a good chance to reach shell-stabilized superheavy nuclei using a range of beam-target combinations. Some of the observed a-decay chains attributed to elements 112 and 114 are believed to link odd-N nuclei. The presence of an odd neutron adds to a theoretical uncertainty. Since the single-particle level density of transactinides is large, there are many candidates for low- lying one-quasiparticle states in parent and daughter nuclei. Moreover, many alpha transitions are structurally forbidden since the properties of one-quasiparticle excitations in parent and daughter nuclei often differ dramatically. As an example, Fig. 4 shows the predicted a-chains for the nucleus 277112 found at GSI. The Hartree-Fock-Bogoliubov calculations explain two observed a branches, attributed experimentally to 273110, in terms of transitions between negative parity and positive parity single-neutron orbitals.
In 1993, chemical studies of dubnium demonstrated that it does not behave like tantalum, the element from the group to which dubnium was supposed to belong. On the contrary, the following chemical studies of Sg (year 1997), Bh (2000), and Hs (2001) confirmed relativistic calculations predicting their behavior to coincide with that expected on the basis of their positions in the periodic table. Hassium, for instance, forms a gaseous oxide similar to that of osmium, which places it in group 8. As of today, the periodic table has been experimentally established up to element 108. However, preparations are under way to carry out gas chemistry of element 112, which instead of behaving like its lighter transition metal homologs (Zn, Cd, Hg) is expected to have properties of a noble gas like Rn or Xe; a first attempt to chemically identify element Z=112 has recently been carried out in Dubna. Still heavier elements, predicted to be noble volatile metals, are also excellent candidates for gas chemical studies, provided that their half-lives are sufficiently long. In particular, there is hope of employing chemical methods for the firm identification of the alpha-chains of long- lived isotopes of Z=114 and 116 observed in Dubna. First predictions of the chemistry of superheavy elements were made in 1971, and the first relativistic molecular calculations for systems involving transactinide elements were published in 1977. Since then, calculations based on the relativistic quantum theory have been considerably improved and applied to many atoms and molecules [5]. Relativistic effects in transactinides are crucial and show up in several ways. Most importantly, s and p1/2 atomic orbitals contract relativistically. The shrinking of the inner shells results in an increased screening of the nuclear charge, and this gives rise to an expansion of the p3/2 and of higher angular momentum orbitals. Another relativistic effect is a change in the spin-orbit coupling. Both can produce drastic rearrangements of orbital levels. That is what is predicted to happen for element 112. Recent calculations indicate that the 7s orbital should be shifted below the 6d5/2 orbital due to relativistic effects. It is the large relativistic stabilization of its valence 7s orbital, combined with its closed shell electron configuration, that has led to the prediction that element 112 is chemically inert. Chemistry of the superheavy elements with Z > 118 is believed to show relativistic effects that are so large that comparison with lighter elements or nonrelativistic results is meaningless. Borders of the
superheavy region As a consequence of their saturation properties, nuclear forces favor values of the internal density close to the saturation density of nuclear matter. On the contrary, since the Coulomb interaction tends to increase the average distance between protons, the Coulomb energy is significantly lowered by either the creation of a central depression or by deformation, or by both. Based on this general argument, one expects the formation of voids in heavy nuclei. Recently, the subject of exotic (bubble, toroidal, band-like) configurations in nuclei with very large atomic numbers has been revisited by self-consistent calculations.
One of the most important and urgent tasks facing experimentalists will be to confirm the new elements found in Dubna. This will not be easy, since these nuclei form an isolated island, disconnected from the known region of the nuclear chart. In order to identify the elements beyond Z=112, new tools, such as direct mass measurements or chemical studies must be developed. How to reach even heavier nuclei? The new-generation high-current stable-beam accelerators will certainly be helpful in making new discoveries at a picobarn level. However, in order to explore new, more neutron-rich superheavy regions, accelerated beams of radioactive neutron-rich nuclei will have to be utilized. It is hoped that the new high-powered ISOL facilities will enable us to explore the theoretically crucial region of nuclei between the deformed N=162 shell and the spherical N=184 shell. There are also many challenges facing nuclear theory of superheavies. The currently highly phenomenological models used to describe heavy-ion fusion are not reliable when extrapolating outside the regions of known nuclei. The situation is not better for the description of static fission barriers and of dynamics of fission. Slightly better is the situation in the theoretical modeling of nuclear structure of transactinides, where the microscopic self- consistent models can make quantitative predictions. Here, the main problem is how to extrapolate density-dependent effective interactions to the superheavy "terra incognita" and how to describe exotic forms of nuclear existence created thanks to the huge Coulomb force and the borders of the superheavy region. The advances in computer technology and in numerical algorithms will certainly be crucial for the success of this task. This research was supported in part by the U.S. Department of Energy under Contract Nos. DE-FG02-96ER40963 (University of Tennessee), DE-AC05-00OR22725 with UT-Battelle, LLC (Oak Ridge National Laboratory), the Polish Committee for Scientific Research (KBN) under Contract No. 2 P03B 040 14, and NATO grant PST.CLG.977613. References [2] S. Cwiok et al., Nucl. Phys. A611 (1996) 211. [3] M. Bender, W. Nazarewicz, and P.G. Reinhard, Phys. Lett. B 515 (2001) 42. [4] J.V. Kratz, in Heavy Elements and Related New Phenomena, Eds. W. Greiner and R.K. Gupta (World Scientific, Singapore, 1999) p. 129. [5] P. Schwerdtfeger and M. Seth, Relativistic Effects of the Superheavy Elements, Encyclopedia of Computational Chemistry, Vol. 4 (Wiley, New York, 1998), p. 2480; V.Pershina et al. in Heavy Elements and Related New Phenomena, Eds. W. Greiner and R.K. Gupta (World Scientific, Singapore, 1999) p. 194. Copyright EPS and EDP Sciences, 2002 |
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