The 9 MV FN Pelletron Tandem can provide beams from hydrogen to gold and can deliver currents up to μA. The 9 MV Tandem hosts different setups.
The ROmanian array for SPectroscopy in HEavy ion Reactions (ROSPHERE) [
98] is a multi-detection array. The "mixed" configuration, which combines fast LaBr
3(Ce) scintillators and large-volume HPGe detectors that have been Compton-suppressed, is the most common one used in the ROSPHERE array, which can hold up to 25 detectors. For cases requiring a high-resolution and high-efficiency detection system, ROSPHERE can alternatively be used as a full HPGe array. A variety of subjects have been addressed in the physics cases, including the role of the negative-parity neutron intruder orbitals in the structure of low-spin states configurations for nuclei near the “island of inversion” [
105], [
106], the study of the nuclear structure near shell and/or subshell closures (see for example [
107], [
108], [
109]), the study of neutron-rich nuclei using low energy transfer/incomplete fusion reactions induced by
7Li beams ( [
110], [
111]) as well as the interplay between collective and single-particle degrees of freedom (see Refs. [
107], [
108], [
109], [
110], [
111]). The main tool to investigate collective phenomena is that of lifetime measurements. Lifetime measurement observables are closely related to the determination of the reduced matrix elements of nuclear transitions. These quantities are in turn very sensitive to details of the nuclear structure and their knowledge is necessary for the testing of different theoretical models. A broad range of experimental techniques to cover the relevant interval for lifetimes of excited states in nuclear systems was employed: the fast timing technique, the RDDS method, and the DSAM method (see Refs. [
105], [
106], [
107], [
108], [
109], [
110], [
111] and references therein). Far from the valley of stability, deviations are observed from the conventional single-particle shell structure. Neutron-rich nuclei with Z ∼ 10 and N ∼ 20 have unexpectedly high binding energies due to the onset of deformation [
112]. The deformation occurs from the filling of the f
7/2 intruder orbital. In stable nuclei f
7/2 intruder orbital lies above the N = 20 shell closure ( [
113], [
114]). The size of the N = 20 shell gap is reduced for neutron-rich Z ∼ 10 nuclei, allowing excitations from the d
3/2 to the f
7/2 orbital to become favored, leading to the region of anomalous shell structure known as the “island of inversion.” The island of inversion is known to extend from neutron numbers N = 20–22 for the Ne, Na, and Mg isotopes (Z = 10–12) [
115]. The half-life of the I
π = 4
− , E=2305 keV intruder state in
34P has been measured as t
1/2 = 2.0 (1) ns. The result was obtained using γ-ray coincidence and fast timing techniques with the mixed LaBr
3-HPGe ROSPHERE detector array. The
18O(
18O,pn)
34P fusion-evaporation reaction at a beam energy of 36 MeV [
105] was used to populate states in
34P. For small values of the mixing ratio, the B(M2) value was found to be consistent with similar transitions associated with the occupation of neutron f
7/2 configurations in this mass region. In the medium-mass region of nuclei approaching the N = 40 subshell closure with Z ∼ 28, it is assumed from empirical observations and theoretical calculations that states with different structures such as single-particle, intruder, and collective states coexist at low and medium excitation energies ( [
116], [
117]). The half-lives of the 9/2
+, 13/2
+, and 15/2
+ yrast states in the neutron-rich
67Cu nucleus were determined by using the in-beam fast-timing technique [
101]. The
67Cu nuclei were produced in an α-induced reaction on a
64Ni target at an incident energy of 18 MeV. 9 MV tandem accelerator produced α-beams. Gamma rays were detected using a setup that consisted of five HPGe detectors, four planar HPGe detectors, and eight LaBr
3(Ce) scintillation detectors. The experimentally obtained E3 transition strength for the decay of the 9/2
+ level to the 3/2
− ground state suggests that the wave function of this level might contain a collective component arising from the coupling of the odd proton p
3/2 with the 3
− state in
66Ni. The measurement of electromagnetic transition rates in nuclei in transitional regions between shell closures and permanently axially deformed nuclei can shed light on the validity of corresponding models of nuclear structure. Excited states in
136Ce were populated via the
124Sn(
16O,4n) fusion-evaporation reaction. The gamma rays were detected using the mixed configuration of ROSPHERE array, which consisted of fourteen HPGe detectors and eleven LaBr
3(Ce) scintillator detectors. Each of the HPGe detectors was surrounded by active Compton suppression shields. The half-lives of the I
π = 5
− and I
π = 7
− yrast states with E
x = 1978 keV and E
x = 2307 keV in the N= 78 isotone
136Ce, have been measured to be 496(23) ps and 270(24) ps, respectively, using the coincident fast-timing spectroscopy technique [
109] The fusion-evaporation reaction
124Sn(
7Li,2n) was used to populate excited states in
129I [
110]. The array of eight HPGe detectors and five LaBr
3(Ce) scintillation detectors were used to measure in-beam γ-ray coincidences. A positive parity band structure built on the 7/2
+ ground state was established and the πg
7/2 configuration at oblate deformation was assigned to it based on the γγ coincidence data. The ground state collectivity of a nucleus can be accurately determined by measuring the reduced transition probability
, and half-life measurements are anticipated to shed light on the structure of nuclei in this transitional region. The ROSPHERE array has been also used to measure the half-life of the yrast I
π = 2
+ state in the neutron-rich nucleus
188W. Fast-timing technique has been used. The resulting value of t
1/2 = 0.87(12) ns is equivalent to a reduced transition probability of
for this transition. Even with a rather significant uncertainty, it seems to indicate a more abrupt decrease in collectivity compared to the trend of lighter tungsten isotopes. According to the estimates for this mass region, this predicted a possibly higher softness for
188W compared to stable tungsten isotopes.
The tape station for beta-decay experiments is also available at INFN-HH, using three clover detectors with 120 % relative efficiency and anti-Compton shields as well as fast LaBr3(Ce). The setup consists of multi-strip silicon detectors for particle detection that may move radially and longitudinally around the target. The setup is used for nuclear reaction and astrophysics studies.
Nuclear astrophysics research takes advantage of ion beams from a 3 MV Tandetron accelerator as well as of the ultra-low background laboratory in a salt mine at Slanic-Prahova [
119]. The ultra-low background radiation laboratory was built and became operational in 2006 in the former Unirea (Slanic-Prahova) salt mine at 208 m below the surface (estimated to a 560 m water equivalent (m.w.e)). In comparison to the identical spectrum recorded at the surface, in the open field, it was discovered that the overall gamma background spectrum between 40 keV and 3 MeV was 100 times smaller at the laboratory level. Given that proton and alpha-capture reactions serve as an important proxy in nucleosynthesis, two of the reactions that were studied at IFIN-HH are α +
64Zn and α +
58Ni [
120], [
121]. Both reactions are important for explosive nucleosynthesis, and in both cases, the measurements done at the IFIN-HH were able to investigate the Gamow window. However, up to now the most significant result was that obtained for the
12C +
12C fusion reaction [
122], [
123].
12C +
12C fusion reaction is a cornerstone case in nuclear astrophysics. There are few experimental data at energies below the Coulomb barrier, and theoretical model predictions on the fusion mechanisms often significantly disagree with the experimental results (see the references in Ref. [
120]). The adjacent reaction,
13C +
12C was studied to obtain information on the fusion interaction at such low energies. The extra neutron in
13C allowed for the production of the unstable
24Na (T
1/2 = 15.0 h) and the use of the activation method (see section 2.1.). The proton evaporation channel leads to an activity with a half-life of 15 h, suitable for samples’ transfer to the salt mine. The study was able to measure the cross-section of the proton evaporation channel down to E
cm =2.3 MeV.