Restricted spin-range correction in the Oslo Method: The example of nuclear level density and $\gamma$-ray strength function from $^{239}\mathrm{Pu}(\mathrm{d,p}\gamma)^{240}\mathrm{Pu}$
F. Zeiser, G.M. Tveten, G. Potel, A.C. Larsen, M. Guttormsen, T.A., Laplace, S. Siem, D. L. Bleuel, B.L. Goldblum, L.A. Bernstein, F.L. Bello, Garrote, L. Crespo Campo, T.K. Eriksen, A. G\"orgen, K. Hadynska-Klek, V.W., Ingeberg, J.E. Midtb{\o}, E. Sahin, T. Tornyi, A. Voinov

TL;DR
This paper introduces an iterative correction method for the Oslo Method to accurately extract nuclear level density and gamma-ray strength functions from reactions with limited spin transfer, demonstrated on $^{240}$Pu.
Contribution
The study develops a novel iterative approach coupling Green's Function Transfer calculations with RAINIER to address spin-parity mismatch issues in the Oslo Method.
Findings
Identified a pronounced enhancement in the gamma-ray strength function between 2-4 MeV.
Validated the iterative correction method for cases with large spin-parity mismatch.
Observed the low-energy orbital M1 scissors mode in $^{240}$Pu.
Abstract
The Oslo Method has been applied to particle- coincidences following the (d,p) reaction to obtain the nuclear level density (NLD) and -ray strength function (SF) of . The experiment was conducted with a 12 MeV deuteron beam at the Oslo Cyclotron Laboratory. The low spin transfer of this reaction leads to a spin-parity mismatch between populated and intrinsic levels. This is a challenge for the Oslo Method as it can have a significant impact on the extracted NLD and SF. We have developed an iterative approach to ensure consistent results even for cases with a large spin-parity mismatch, in which we couple Green's Function Transfer calculations of the spin-parity dependent population cross-section to the nuclear decay code RAINIER. The resulting SF shows a pronounced enhancement between 2-4 MeV that isā¦
| 6.53420(23)a | 25.16(20)b | 0.12(8)b | 8.43(80)d | 2.20(9)c | 32.7(66) | 0.415(10) | 43(4)c |
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Restricted spin-range correction in the Oslo Method: The example of nuclear level density and -ray strength function from
F. Zeiser
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
G.M. Tveten
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
G. Potel
Facility for Rare Isotope Beams, Michigan State University, East Lansing, MI 48824, USA
āā
A.C. Larsen
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
M. Guttormsen
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
T.A. Laplace
Department of Nuclear Engineering, University of California, Berkeley, 94720, USA
āā
S. Siem
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
D.L. Bleuel
Lawrence Livermore National Laboratory, Livermore, CA 94551, USA
āā
B.L. Goldblum
Department of Nuclear Engineering, University of California, Berkeley, 94720, USA
āā
L.A. Bernstein
Department of Nuclear Engineering, University of California, Berkeley, 94720, USA
āā
F.L. Bello Garrote
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
L. Crespo Campo
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
T.K. Eriksen
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
A. Gƶrgen
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
K. Hadynska-Klek
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
V.W. Ingeberg
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
J.E. MidtbĆø
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
E. Sahin
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
T. Tornyi
Department of Physics, University of Oslo, N-0316 Oslo, Norway
āā
A.Ā Voinov
Department of Physics and Astronomy, Ohio University, Athens, Ohio 45701, USA
āā
M. Wiedeking
iThemba LABS, P.O. Box 722, Somerset West 7129, South Africa
āā
J. Wilson
Institut de Physique NuclĆ©aire dāOrsay, CNRS/ Univ. Paris-Sud, UniversitĆ© Paris Saclay, 91406 Orsay Cedex, France
(March 19, 2024)
Abstract
The Oslo Method has been applied to particle- coincidences following the (d,p) reaction to obtain the nuclear level density (NLD) and -ray strength function (SF) of . The experiment was conducted with a 12Ā MeV deuteron beam at the Oslo Cyclotron Laboratory. The low spin transfer of this reaction leads to a spin-parity mismatch between populated and intrinsic levels. This is a challenge for the Oslo Method as it can have a significant impact on the extracted NLD and SF. We have developed an iterative approach to ensure consistent results even for cases with a large spin-parity mismatch, in which we couple Greenās Function Transfer calculations of the spin-parity dependent population cross-section to the nuclear decay code RAINIER. The resulting SF shows a pronounced enhancement between 2-4Ā MeV that is consistent with the location of the low-energy orbital scissors mode.
I Introduction
Accurate knowledge of neutron induced cross-sections on actinides is important for many applications. From thermal energies up to several MeVs, there is a considerable competition between fission and neutron absorption. This competition, as well as several other factors like the lack of a mono-energetic neutron source in this energy range and the lifetime of short-lived isotopes, pose a challenge for direct cross-sections measurement.
Most designs for next generation nuclear reactors are based on fast-neutron induced fissionĀ Pioro (2016). Therefore, knowledge of the cross-sections for a wider range of incident neutron energies have become important. In particular, more precise measurements of the (n,) cross-section below Ā MeV are listed as a high priority request by the Nuclear Energy Agency (NEA)Ā NEA . Calculations for above the resonance region (i.e., above ākeV) can be obtained within the statistical Hauser-Feshbach frameworkĀ HauserĀ andĀ Feshbach (1952) and require knowledge of the nuclear level density (NLD) and -ray strength function (SF) of the residual nucleus . Furthermore, a better knowledge of NLDs and SFs in the actinide region has the potential to improve the nuclear-physics related uncertainties introduced to abundance calculations of heavy-element production in extreme astrophysical environmentsĀ ArnouldĀ etĀ al. (2007).
The Oslo methodĀ SchillerĀ etĀ al. (2000); LarsenĀ etĀ al. (2011) can be used on particle- coincidence spectra from transfer reactions to simultaneously extract the NLD and SF below the neutron separation energy . In a campaign to study actinide nuclei, the method has been applied to the compound nuclei , , , Ā GuttormsenĀ etĀ al. (2012, 2013, 2014); TornyiĀ etĀ al. (2014a) and Ā LaplaceĀ etĀ al. (2016) using different light-ion reactions. So far, all observed NLDs are consistent with a constant temperatureĀ Ericson (1960) level density formula. The SF of these heavy and well-deformed systems show a pronounced enhancement between about 2-4Ā MeV, which is in the energy rangeĀ HeydeĀ etĀ al. (2010) of a low-energy orbital M1 scissors resonance (SR).
The nuclear data community has recently started to take into account these strong M1 SRs, and in two recent studies by Ullmann et al.Ā UllmannĀ etĀ al. (2014, 2017), a significant impact of the SR on the cross-sections calculated for uranium isotopes has been shown. An extraction of the NLD and SF of will facilitate similar calculations for . They can be validated by comparison to updated direct measurement byĀ MosbyĀ etĀ al. (2018) between 10Ā eV and 1.3Ā MeV.
Larsen et al.Ā LarsenĀ etĀ al. (2011) have shown that the population of a limited spin range make it necessary to correct the slopes of SFs extracted with the Oslo Method. In the previous experimental studies on actinidesĀ GuttormsenĀ etĀ al. (2012, 2013, 2014); TornyiĀ etĀ al. (2014a); LaplaceĀ etĀ al. (2016), first indications of the impact of a low spin transfer using the (d,p) reaction mechanism were observed and an improvised procedure for the correction was developed. More recently, we have presented a systematic analysis of the effect of a realistic spin distribution on both the NLD and SF for the reaction ZeiserĀ etĀ al. (2018).
In this article, we will present the NLD and SF of analyzed with the Oslo Method. We develop an iterative procedure to correct for the bias introduced in the Oslo Method for (d,p) reactions on heavy nuclei due to a spin-parity population mismatch.
II Experimental methods and data analysis
The experiment was conducted using a 12Ā MeV deuteron beam extracted from the MC-35 Scanditronix Cyclotron at the Oslo Cyclotron Laboratory (OCL). The thick target was purified by an anion-exchange resin column procedureĀ HendersonĀ etĀ al. (2011) prior to electroplating it onto a beryllium backing. A -ray assay of the resulting target revealed the purity to be %.
Particle- coincidences were measured with the SiRi particle telescopesĀ GuttormsenĀ etĀ al. (2011) and CACTUS -ray detector arrayĀ GuttormsenĀ etĀ al. (1990). SiRi consists of 64 silicon particle telescopes with a thickness of 130 m for the front () and 1550 m for the back () detectors. In this experiment they were placed in a backward position with respect to the beam direction, covering azimuthal angles from to . Compared to the forward direction, this configuration reduces the contribution of elastically scattered deuterons and populates a broader and higher spin-range. The CACTUS array was composed of 26 lead collimated NaI(Tl) crystals with a total efficiency of 14.1(2) at (measured with a source) that surrounded the target chamber and the particle telescopes. Additionally, four Parallel Plate Avalanche Counters (PPAC)Ā TornyiĀ etĀ al. (2014b) were used to detect fission events. The back detectors of SiRi were used as master gates for a time-to-digital converter (TDC). The NaI(Tl) detectors were delayed by and individually served as stop signals. The signals were processed by a leading edge discriminator and the resulting time walk was corrected for by the procedure given in Ref.Ā GuttormsenĀ etĀ al. (2011). The prompt particle- coincidences were sorted event-by-event from a 28āns wide time-window and the background from random coincidences was subtracted. The amount of deposited energy depends on the outgoing particle type, which facilitated the selection of (d,p) events by setting proper gates in a - matrix. The spectra were calibrated using reaction kinematics, which also allowed translation of the deposited particle energy to the initial excitation energy of the residual nucleus . The -ray spectra for each excitation energy were unfolded following the procedure of Ref.Ā GuttormsenĀ etĀ al. (1996), however using new response functions measured in 2012Ā CampoĀ etĀ al. (2016). In this work we used the Oslo method software v1.1.2 GuttormsenĀ etĀ al. (2018).
To select the decay channel, only excitation energies below the neutron separation energy (Ā SinghĀ andĀ Browne (2008)) were considered. The energy range was further constrained by pile-up of -rays and the onset of fission events at Ā MeV. The latter was previously identified as sub-barrier fissionĀ BackĀ etĀ al. (1974); HunyadiĀ etĀ al. (2001). A more detailed analysis of the prompt fission -rays can be found in Ref.Ā RoseĀ etĀ al. (2017). The final extraction regions were , , .
We applied an iterative subtraction technique to obtain the energy spectrum of the primary (also called first generation) -rays from the initial spectrum, which includes all decay cascades. The principal assumption of the first-generation methodĀ GuttormsenĀ etĀ al. (1987) is that the decay from any excited state is independent of its formation. The branching ratio is an inherent property of a state. Thus, the assumption is automatically fulfilled if levels have the same probability to be populated by the decay of higher-lying states as directly by nuclear reactions (e.g. via the (d,p) reaction). As we consider the quasi-continuum, we can relax the strict conditions and apply statistical considerations so we only require that in a given excitation energy bin all levels with the same spin-parity are populated approximately equally (instead of specific states). In addition, the population probability of levels with a given spin-parities should be approximately constant as a function of the excitation energy. In Sec. V we will show that this condition is not satisfied and we propose a procedure to minimize the impact of the violation of this assumption. For a thorough discussion of other possible errors and uncertainties in this method, see Ref. LarsenĀ etĀ al. (2011). The coincidence matrices are displayed in Fig. 1.
III Extraction of NLD and SF
According to Fermiās golden rule, the decay rate from an initial state to a final state can be decomposed into the transition matrix element and the level density at the final state Dirac (1927); Fermi (1950). In the regime of statistical -rays, we consider ensembles of initial and final states, thus probing decay properties averaged over many levels. We assume that any decay mode can be build on the ground and excited state in the same way, i.e. there is no spin-parity or excitation energy dependence, which is a generalized version of the Brink-Axel hypothesisĀ Brink (1955); Axel (1962). Thus, the decay properties do not depend on the specific levels, but only on the energy difference between them. Consequently, the dependence on initial and final states is reduced to a single dependence on the energy difference given by the -ray energy . The decay probability corresponding to the first-generation matrix can therefore be factorized into the level density of the final excitation energy and the transmission coefficient Ā SchillerĀ etĀ al. (2000):
[TABLE]
The validity of the Brink-Axel hypothesis in the quasi-continuum has recently been shown for several nuclei LarsenĀ etĀ al. (2017); CampoĀ etĀ al. (2018), amongst them the actinide nucleus Ā GuttormsenĀ etĀ al. (2016). The level density and transmission coefficient were obtained by a fit to Ā SchillerĀ etĀ al. (2000). Note that this procedure does not require any initial assumptions on the functional form of and . However, any transformation and with the parameters , and gives identical fits to the matrix :Ā SchillerĀ etĀ al. (2000)
[TABLE]
The determination of the transformation parameters corresponding to the correct physical solution, i.e. the normalization of the NLD and SF, is discussed in the next section.
IV Initial extraction of the level density and transmission coefficient
For the normalization of the level density, , we need at least two reference points, such that we can determine the parameters and in Eq. (2). At low excitation energies, our data are matched to discrete levelsĀ NND up to the critical energy where we expect the low-lying level scheme to be complete. At the neutron separation energy , we calculate under the assumption of equal parity distribution from the average neutron resonance spacing for s-waves, , taken from RIPL-3Ā CapoteĀ etĀ al. (2009) following Ref.Ā SchillerĀ etĀ al. (2000):
[TABLE]
Here is the ground-state spin of the target nucleus .
We use the spin distribution proposed by Ericson (1960, Eq. (3.29))111The same spin distribution is often attributed to the subsequent work of GilbertĀ andĀ Cameron (1965). together with the rigid-body moment of inertia approach for the spin cut-off parameter from 2005 byĀ von EgidyĀ andĀ Bucurescu (2005):
[TABLE]
where is the mass number of the nucleus, is the level density parameter, is the intrinsic excitation energy, and is the back-shift parameter. All parameters are listed in Tab. 1
Since there is a gap of approximately 3.5Ā MeV between the highest excitation energy of the extracted level densities and the neutron separation energy , an interpolation is used to connect the datasets. In accordance with the findings for other actinidesĀ GuttormsenĀ etĀ al. (2013), we use the constant temperature (CT) level density formulaĀ Ericson (1960)
[TABLE]
with the shift in excitation energy given by
[TABLE]
The best fit is obtained for a constant temperature of . Only a limited number of data points are available for the fit which are well above . This makes a proper interpretation of the uncertainty on the fit parameters difficult. This is the main contribution to the systematic error, which is shown as an error band in the results in Fig. 2.
For the transmission coefficient , the remaining parameter is determined by normalization to the average total radiative width from (n,) experimentsĀ CapoteĀ etĀ al. (2009), under the assumption of equal parity usingĀ VoinovĀ etĀ al. (2001); KopeckyĀ andĀ Uhl (1990)
[TABLE]
where is the ground-state parity of the target nucleus . Note that the sum in Eq. (9) runs over all available final states of , where we consider only spins that can be reached by one primary dipole transition after neutron capture, i.e. . The -ray strength function is obtained under the same assumption of a dominance of dipole strength, =1, so , and
[TABLE]
To specify the integral in Eq. (9) completely, we use a log-linear extrapolation in the SF below and a log-linear extrapolation in between and .
V Corrections due to spin-parity mismatch
First indications that a limited spin-range of the levels populated in a given reaction has an impact on the Oslo method have been discussed in Ref.Ā LarsenĀ etĀ al. (2011). Due to the low angular momentum transfer expected for light-ion reactions, and in particular the (d,p) transfer reaction, the higher spin states that are already available at Ā MeV in heavy nuclei may not be populated. In Ref.Ā GuttormsenĀ etĀ al. (2012) an ad-hoc method was developed to correct for observations that were attributed to the limited angular momentum transfer. This correction has subsequently been applied to other heavy nucleiĀ GuttormsenĀ etĀ al. (2013, 2014); TornyiĀ etĀ al. (2014a); LaplaceĀ etĀ al. (2016); GiacoppoĀ etĀ al. (2015). In a recent analysis on systematic errors for (d,p) we have demonstrated that the application of the Oslo Method produces consistent results when the spin-parity dependent population probability equals the theoretically expected distribution of the intrinsic levels . However, when there is a large mismatch in the spin-parity distributions we have also shown that the aforementioned ad-hoc method lead to significant distortions in the NLD and SFĀ ZeiserĀ etĀ al. (2018). We will denote the extracted quantities as the apparent NLD and SF, and distinguish them from the true NLD and SF that would have been observed with an ideal, bias-free method. In absence of an ideal method, our goal is to find a consistent set of NLD and SF, where we define consistency as follows: if we provide this set as input to a nuclear decay code like RAINIERĀ L.E. KirschĀ andĀ F. Zeiser (2019), the generated synthetic data should match the experimentally obtained coincidences. This grantees at the same time that the analysis of the synthetic data yields the same apparent NLD and SF as those determined from the naive222In the sense that the experimental analysis does not inherently take into account a spin-parity mismatch. experimental analysis. In this section we extend the analysis of Ref.Ā ZeiserĀ etĀ al. (2018) in order to retrieve a consistent set of NLD and SF for for the same reaction. This approach is, however, easily generalizable to other target nuclei and in principle also applicable for other light-ion reactions.
We will start with a brief overview of the procedure and then discuss each step in more detail:
Calculate the spin-parity distribution of the population probability , and the distribution of the intrinsic levels for each excitation energy bin . 2. 2.
Generate a synthetic coincidence dataset for an artificial nucleus resembling , given the spin distributions, and the trial NLD and SF. 3. 3.
Analyze and compare the apparent NLD and SF from the synthetic dataset and experimental coincidences using the Oslo Method. 4. 4.
Adjust the trial NLD and SF and repeat step 2 and 3. Adopt the solution with the smallest difference between experimental and synthetic coincidence spectra.
To calculate the population probability for each in the residual nucleus following a (d,p) reaction, we have to distinguish between two reaction mechanisms. First, we consider direct processes, i.e. the breakup of a deuteron with emission of a proton, followed by the formation of a compound nucleus with the remaining neutron and the target. Spin-parity dependent cross section are calculated for the angles covered in the experiment within the Greenās Function Transfer formalism described in Ref.Ā PotelĀ etĀ al. (2015, 2017). The neutron-nucleus interactions are modeled by the dispersive optical model potential (OMP) of CapoteĀ etĀ al. (2008) implemented through potential no. 2408 listed in RIPL-3 CapoteĀ etĀ al. (2009). The usage of a dispersive OMP improves the predictive power for . Note that we did not use the OMP in the context of full coupled-channels calculations, which would have explicitly accounted for the coupling to rotational states. We expect that this will lead to an underestimation of the absorption cross-section of about 20%; however the relative population of the different spins and parities should essentially be unaffected. We normalize the population cross-sections to 1 for each bin, thus obtaining the probability distribution . Figure 3 shows the results for the population spin-parity distribution .
Compound reactions are the second mechanism leading to as a residual nucleus: proton evaporation after fusion of the deuteron and target nucleus and the inelastic excitation of the target to energies above the proton emission threshold. The spin-parity integrated cross-section for these processes has been estimated to be using the statistical framework of the TALYS nuclear reactions code v1.8Ā KoningĀ etĀ al. (2008). This is an order of magnitude smaller than for the direct process and therefore neglected. The low cross-sections are reasonable as the deuteron beam energy of 12Ā MeV is below the Coulomb barrier of about 14.46Ā MeV, where the latter is calculated with a radius parameter āfmĀ SoukhovitskiiĀ etĀ al. (2004).
To study the effect on the extracted NLD and SF, we generate a synthetic dataset with the statistical nuclear decay code RAINIER v1.4.1Ā KirschĀ andĀ Bernstein (2018); L.E. KirschĀ andĀ F. Zeiser (2019). This code uses a Monte Carlo approach to generate levels of an artificial nucleus and simulate -emission cascades via , , or transitions. The analysis library facilitates the extraction of the -ray spectra (first or all generations) emitted from each initial excitation energy bin . The matrix including the -ray spectra of all generations substitutes for the experimental particle- coincidence in the further analysis. The input parameters have been chosen to resemble the nucleus and the analysis in the previous section. The initial settings are summarized below, and a comprehensive list including the analysis code can be found online333https://github.com/fzeiser/240Pu_article_supplement:
- ā¢
Discrete levels up to 1.037 MeV (18 levels).
- ā¢
Above 1.037Ā MeV: Generated levels from the NLD extracted in Sec. IV with the nearest neighbor spacing according to the Wigner distribution Wigner (9567).
- ā¢
Intrinsic spin distribution following Eq. (5), with a spin-cut parameter of Eq. (6) (assumes equiparity).
- ā¢
Spin-parity dependent population probabilities from our calculations. 444Note that we did not include the excitation energy dependence of the population cross-section for this analysis, although it could in principle be included to give a more stringent test of the first generation method.
- ā¢
SF as extracted in Sec. IV, fitted by two constant temperature Generalized Lorentzians (GLO)Ā KopeckyĀ andĀ Uhl (1990), two Standard Lorentzians (SLO), and including Porter-Thomas fluctuationsĀ PorterĀ andĀ Thomas (1956). The component was assumed to be negligible.
- ā¢
Internal conversion model: BrIcc Frozen Orbital approximation Kibédi et al. (2008).
Due to the strong parity dependence of , the generated simulated coincidence spectra depend on the decomposition of the SF into its and components. We performed a fit of the centroid, the peak cross section and width of each resonance of the SF simultaneously using the differential evolution algorithm by StornĀ andĀ Price (1997). In addition to our data , which measures only the summed SF (+), we include the data of Kopecky et al. KopeckyĀ etĀ al. (2017); ChrienĀ etĀ al. (1985) around , which resolve the and components. There are no measurements for the Giant Dipole Resonance (GDR) of . However, as the GDR is expected to vary little between the plutonium isotopes, we also include measurements (again included in ) by DeĀ MoraesĀ andĀ Cesar (1993) and GurevichĀ etĀ al. (1976). A third dataset by BermanĀ etĀ al. (1986) is yield systematically lower cross-sections than the first two measurements, which where consistent within the error-bars. Therefore we did not include the data of BermanĀ etĀ al. (1986) in the fit. Each term is weighted by the experimental uncertainty of the datapoint. The total is then given as the sum over the s for the summing data () and data that resolve the and contributions:
[TABLE]
The generated coincidence data are analyzed with the Oslo Method and the results are displayed in Fig. 4. We can quantify how consistent the input NLD and SF are by construction of the ratio of the apparent NLD and SF analyzed from synthetic data to the experimental analysis (see Sec. IV). We extract this ratio for each iteration. For the NLD this means that below 3Ā MeV we compare to the data points, whereas above 3Ā MeV we use the CT extrapolation. In case of the SF, we compare to its fit, so the sum of the 2 GLOs and 2 SLOs. The inverse of the ratio is used as a bin-by-bin correction to the input NLD and SF of iteration , such that we generate the input for the next iteration, :
[TABLE]
where is the input NLD or SF, respectively. We introduced an additional factor of , which can be seen as reduction of the step-size of the correction . This increased the stability of the solution. As an example, looking at the first iteration, we find that the analyzed NLD from the synthetic data at 2.5Ā MeV is only 50% of the experimentally observed NLD. We would therefore increase the input NLD for the next iteration by 25% in this bin (and process all other bins of the NLD and SF in the same manner). For the first iterations we observe that the changes impact by about 25%. As is determined from independent measurements, we enforce a match by rescaling the predicted input SF.
After only 3 to 4 iterations, we observe that the SF and NLD have approximate converged, with the exception of the higher energy region of the SF. The reproduction of the SF above remains challenging. The corresponding fit region in the first-generation matrix is formed by non-statistical decays, thus it is not obvious that the Oslo Method should be applicable in this regime. In addition, the comparison in this regime is sensitive to the choice of the extrapolation of the initial SF.
In Fig. 5 we compare the experimental coincidence data with the synthetic data from different iterations. All spectra have been normalized to obtain the probability for the emission of a -ray with energy in the decay cascade from a level in the excitation energy bin . This removes any dependence on the simulated vs. measured number of -rays and of a potential mismatch of the population cross-section as a function of the excitation energy . The differences over whole extraction region (see Sec. II) are displayed for each iteration in Fig. 6. We find that iteration 3 improves the reproduction of the experimental coincidence spectra by about 50%, compared to the initial analysis, iteration 1. Higher iterations give a reasonable reproduction of the first generation spectra, but show an increased deviation of the (all generations) coincidence spectra. This might be explained by an overcompensation for MeV as discussed above. Additionally, a closer analysis of the first vs all generations spectra indicate a too high probability to decay through a specific state, or set of states, with MeV. This is already visible for iteration 3 in Fig. 5, but the mismatch increases for the higher iterations.
In the described procedure, we used a Monte-Carlo approach to simulate the nucleus and its behavior, therefore, the results may vary between different realizations from the same input parameters. However, we found that in the case of a heavy nucleus the level density was so high that the effects could be neglected for this analysis.
VI Discussion
As noted in Ref. ZeiserĀ etĀ al. (2018), the Oslo Method does not intrinsically account for differences in the spin-parity distributions and ; when there is a significant spin-parity mismatch the resulting apparent NLD and SF will be distorted compared to the a priori true NLD and SF. This effect can be observed in Fig. 4 by comparing the input for iteration 3 to RAINIER to the results after application of the Oslo Method. The presented method takes into account and and generates synthetic coincidence datasets. As the apparent NLD and SF extracted with the Oslo Method from synthetic and experimental coincidences data suffer the same distortions, we can identify a consistent set of NLD and SF from those simulations that lead to an apparent NLD and SF that match the results from the experimentally obtained coincidences (Sec. IV). In Fig. 4 it can be observed that this is the case for the input NLD and SF to the iteration. Future studies are recommended to establish the sensitivity of the current approach. It is for example possible to find other suitable decompositions and other empirical models to describe the SF in the fitting procedure in Sec. V. This would effect the SF and NLD derived from this method. Ideally, one could couple the RAINIER simulations with a Monte Carlo Markov chain code GelfandĀ andĀ Smith (1990); RobertĀ andĀ Casella (2011) directly (without iterating through the Oslo Method) and find the posterior probability of different NLD and SF combinations to match the experimental observations. However, for a heavy nucleus such as each iteration takes about 50 h on a single core Intel E5-2683v4 2.1 GHz, such that the computational costs quickly render a full-scale parameter search unfeasible.
In Fig. 7, we compare the input SF of the iteration to the result of the initial analysis (see Sec. IV) and the measurements of KopeckyĀ etĀ al. (2017), DeĀ MoraesĀ andĀ Cesar (1993) and GurevichĀ etĀ al. (1976). The absolute scale of the proposed SF is lower than in the initial analysis, which is attributed to the increased NLD (see Fig. 4, left panels), as can be seen from Eq. (9).
Around , the derived SF is significantly lower than the measurements by Kopecky et al. KopeckyĀ etĀ al. (2017); ChrienĀ etĀ al. (1985). However, there are two ways to resolve the apparent discrepancy: First, according to the original analysis ChrienĀ etĀ al. (1985), the data of Kopecky et al. KopeckyĀ etĀ al. (2017); ChrienĀ etĀ al. (1985) have a systematic normalization uncertainty of 30% (only the statistical errors are plotted). Second, our results have little sensitivity to the SF above approximately . Thus, we could add another resonance at without changing any other observables, like the shape of the extracted SF or .
The retrieved SF reveals an excess strength between on the hypothetically smooth tail of the GDR. This is consistent with the location of the low-energy orbital M1 SR HeydeĀ etĀ al. (2010). Several other studies in the actinide region using (d,p) reactions and the Oslo Method have observed a similar excessĀ GuttormsenĀ etĀ al. (2012, 2013, 2014); TornyiĀ etĀ al. (2014a); LaplaceĀ etĀ al. (2016). However, we expect that the spin-parity distributions may also have biased the NLD and SF obtained in those experiments, and therefore plan to reanalyze the extracted strength with the present method.
VII Conclusions
We have developed an iterative procedure to correct for the bias introduced in the Oslo Method when the spin-parity dependent population probability differs significantly from the spin-parity distribution of the intrinsic levels . We have calculated for the experiment performed at the OCL within the Greenās Function Transfer formalism. Using the nuclear decay code RAINIER, we have simultaneously retrieved a NLD and SF of which are consistent with the experimental analysis. The SF reveals excess strength between , which can be identified as the orbital M1 SR. The results have been compared to other measurements and the origin of the differences has been addressed.
Acknowledgements.
We would like to thank J. C. Müller, E. A. Olsen, A. Semchenkov, and J. C. Wikne at the Oslo Cyclotron Laboratory for providing the stable and high-quality deuteron beam during the experiment. We are indebted to R. Capote for discussions on the implementation of the OMP and L.E. Kirsch for his help explaining and extending the of capabilities of RAINIER. This work was supported by the Research Council of Norway under project Grants No. 263030 and 262952, and by the National Research Foundation of South Africa. A.C.L. gratefully acknowledges funding from the European Research Council, ERC-STG-2014 Grant Agreement No. 637686. We gratefully acknowledge support of the U.S. Department of Energy by Lawrence Livermore National Laboratory under Contract No. DE-AC52-07NA27344 and by the Lawrence Berkeley National Laboratory under Contract No. DE-AC02-05CH11231. This work was supported by the U.S. Department of Energy (DOE), National Nuclear Security Administration (NNSA) under Awards DE-NA0002905 and DE-NA0003180, the latter via the Office of Defense Nuclear Nonproliferation Research and Development (DNN R&D) through the Nuclear Science and Security Consortium. We acknowledge support by DOE Office of Science, Office of Nuclear Physics, under the FRIB Theory Alliance award DE-SC0013617. This work was supported by the National Research Foundation of South Africa Grant No. 118846.
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