$s$-wave scattering lengths for the $^7$Be+p system from an $\textit{R}$-matrix analysis
S. N. Paneru (1), C. R. Brune (1), R. Giri (1), R. J. Livesay (2), U., Greife (2), J. C. Blackmon (3), D. W. Bardayan (4), K. A. Chipps (5), B., Davids (6, 7), D. S. Connolly (6), K. Y. Chae (8), A. E. Champagne (9), C., Deibel (10), K. L. Jones (11, 12), M. S. Johnson (12)

TL;DR
This study measures the $s$-wave scattering lengths for the $^7$Be+p system using an R-matrix analysis, providing more precise values that can improve understanding of the astrophysical $S$-factor and the structure of $^8$B.
Contribution
The paper presents the first precise determination of $s$-wave scattering lengths for $^7$Be+p, reducing uncertainties significantly and exploring the level structure of $^8$B.
Findings
$s$-wave scattering lengths for channels 1 and 2 are 17.34 and -3.18 fm.
Uncertainty in scattering lengths reduced by a factor of 5-8.
Evidence for 0$^+$ and 2$^+$ levels in $^8$B at 1.9 and 2.21 MeV.
Abstract
The astrophysical -factor for the radiative proton capture reaction on Be () at low energies is affected by the -wave scattering lengths. We report the measurement of elastic and inelastic scattering cross sections for the Be+p system in the center-of-mass energy range 0.474 - 2.740 MeV and center-of-mass angular range of 70- 150. A radioactive Be beam produced at Oak Ridge National Laboratory's (ORNL) Holifield Radioactive Ion Beam Facility was accelerated and bombarded a thin polypropylene (CH) target. Scattered ions were detected in the segmented Silicon Detector Array. Using an -matrix analysis of ORNL and Louvain-la-Neuve cross section data, the -wave scattering lengths for channel spins 1 and 2 were determined to be 17.34 and -3.18 fm, respectively. The uncertainty in the…
| Reaction () | Norm | N | |
|---|---|---|---|
| (A) 7Be(p,p)7Be | |||
| 0.474 MeV | 1.012 | 37.750 | 16 |
| 0.537 MeV | 1.283 | 53.301 | 16 |
| 0.626 MeV | 1.039 | 17.119 | 16 |
| 0.854 MeV | 1.274 | 24.176 | 16 |
| 0.981 MeV | 1.375 | 3.333 | 4 |
| 1.106 MeV | 1.300 | 18.982 | 16 |
| 1.232 MeV | 1.177 | 12.599 | 16 |
| 1.358 MeV | 1.144 | 8.223 | 16 |
| 1.484 MeV | 1.039 | 29.985 | 16 |
| 1.610 MeV | 1.032 | 14.725 | 16 |
| 1.861 MeV | 0.893 | 10.891 | 12 |
| 1.987 MeV | 0.781 | 15.205 | 16 |
| 2.175 MeV | 0.964 | 5.815 | 13 |
| 2.389 MeV | 0.987 | 6.270 | 16 |
| 2.489 MeV | 0.933 | 2.706 | 13 |
| 2.740 MeV | 0.908 | 3.351 | 16 |
| (B) 7Be(p,p’)7Be(1/2-) | |||
| 1.106 MeV | 1.060 | 27.143 | 11 |
| 1.232 MeV | 1.177 | 34.612 | 14 |
| 1.358 MeV | 1.022 | 6.982 | 12 |
| 1.484 MeV | 0.871 | 13.540 | 15 |
| 1.610 MeV | 0.858 | 21.685 | 12 |
| 1.861 MeV | 1.398 | 20.647 | 16 |
| 1.987 MeV | 0.939 | 5.095 | 16 |
| 2.175 MeV | 0.980 | 2.020 | 6 |
| 2.389 MeV | 1.120 | 12.803 | 16 |
| 2.489 MeV | 0.930 | 13.521 | 10 |
| 2.740 MeV | 0.713 | 46.574 | 16 |
| (C) 7Be(p,p)7Be | |||
| 120.24∘-131.13∘ | 0.987 | 98.966 | 87 |
| 156.62∘-170.21∘ | 0.978 | 236.707 | 343 |
| Jπ | S=1 | S=2 | S=0 | S=1 | |
|---|---|---|---|---|---|
| (MeV) | (MeV) | (MeV) | (MeV) | (MeV) | |
| 2+ | 0.000 | -0.456 | -0.959 | 0.000 | 0.510 |
| 1+ | 0.774 | 1.484 | -0.268 | -0.004 | 2.904 |
| 0+ | 1.900 | 0.501 | 0.000 | 0.000 | 1.201 |
| 2+ | 2.210 | -0.274 | 0.323 | 0.000 | 0.632 |
| 3+ | 2.320 | 0.000 | 0.607 | 0.000 | 0.000 |
| 2- | 3.520 | 0.000 | 1.700 | 0.000 | 0.000 |
| 1- | (9.000) | 1.433 | 0.000 | 0.000 | -1.822 |
| 2+ | (9.000) | -77.322 | -332.657 | 0.000 | 66.565 |
| 3+ | (14.000) | 0.000 | 1.514 | 0.000 | 0.000 |
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
-wave scattering lengths for the 7Be+p system from an R-matrix analysis
S. N. Paneru
Department of Physics and Astronomy, Ohio University, Athens, Ohio 45701, USA
C. R. Brune
Department of Physics and Astronomy, Ohio University, Athens, Ohio 45701, USA
R. Giri
Department of Physics and Astronomy, Ohio University, Athens, Ohio 45701, USA
R. J. Livesay
Department of Physics, Colorado School of Mines, Golden, Colorado 80401, USA
U. Greife
Department of Physics, Colorado School of Mines, Golden, Colorado 80401, USA
J. C. Blackmon
Department of Physics and Astronomy, Louisiana State University, Baton Rouge, Louisiana 70803, USA
D. W. Bardayan
Department of Physics, University of Notre Dame, Notre Dame, Indiana 46556, USA
K. A. Chipps
Physics Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA
B. Davids
TRIUMF, Vancouver, British Columbia V6T 2A3, Canada
Physics Department, Simon Fraser University, Burnaby, British Columbia V5A1S6, Canada
D. S. Connolly
TRIUMF, Vancouver, British Columbia V6T 2A3, Canada
K. Y. Chae
Department of Physics, Sungkyunkwan University, Suwon 16419, Korea
A. E. Champagne
Department of Physics and Astronomy, University of North Carolina, Chapel Hill, North Carolina, 27599, USA
C. Deibel
Wright Nuclear Structure Laboratory, Yale University, New Haven, Connecticut 06520, USA
K. L. Jones
Department of Physics and Astronomy, University of Tennessee, Knoxville, Tennessee 37996, USA
Department of Physics and Astronomy, Rutgers University, Piscataway, New Jersey 08854, USA
M. S. Johnson
Department of Physics and Astronomy, Rutgers University, Piscataway, New Jersey 08854, USA
R. L. Kozub
Physics Department, Tennessee Technological University, Cookeville, Tennessee 38505, USA
Z. Ma
Department of Physics and Astronomy, University of Tennessee, Knoxville, Tennessee 37996, USA
C. D. Nesaraja
Department of Physics and Astronomy, University of Tennessee, Knoxville, Tennessee 37996, USA
Physics Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA
S. D. Pain
Department of Physics and Astronomy, Rutgers University, Piscataway, New Jersey 08854, USA
F. Sarazin
Department of Physics, Colorado School of Mines, Golden, Colorado 80401, USA
J. F. Shriner Jr
Physics Department, Tennessee Technological University, Cookeville, Tennessee 38505, USA
D. W. Stracener
Physics Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA
M. S. Smith
Physics Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA
J. S. Thomas
Department of Physics and Astronomy, Rutgers University, Piscataway, New Jersey 08854, USA
D. W. Visser
Department of Physics and Astronomy, University of North Carolina, Chapel Hill, North Carolina, 27599, USA
C. Wrede
Wright Nuclear Structure Laboratory, Yale University, New Haven, Connecticut 06520, USA
Abstract
The astrophysical -factor for the radiative proton capture reaction on 7Be () at low energies is affected by the -wave scattering lengths. We report the measurement of elastic and inelastic scattering cross sections for the 7Be+p system in the center-of-mass energy range 0.474- 2.740 MeV and center-of-mass angular range 70∘- 150∘. A radioactive 7Be beam produced at Oak Ridge National Laboratory’s (ORNL) Holifield Radioactive Ion Beam Facility was accelerated and bombarded a thin polypropylene (CH2) target. Scattered ions were detected in the segmented Silicon Detector Array. Using an R-matrix analysis of ORNL and Louvain-la-Neuve cross-section data, the -wave scattering lengths for channel spins 1 and 2 were determined to be 17.34 and -3.18 fm, respectively. The uncertainty in the -wave scattering lengths reported in this work is smaller by a factor of 5-8 compared to the previous measurement, which may reduce the overall uncertainty in at zero energy. The level structure of 8B is discussed based upon the results from this work. Evidence for the existence of 0+ and 2+ levels in 8B at 1.9 and 2.21 MeV, respectively, is observed.
pacs:
I INTRODUCTION
The total terrestrial flux of high-energy neutrinos resulting from the decay of 8B in the Sun has been measured with a precision of 4 Aharmim et al. (2013); Abe et al. (2016). Comparisons of the measured and predicted 8B solar neutrino fluxes are therefore limited primarily by the theoretical uncertainty of approximately 14 associated with standard solar model predictions Haxton et al. (2013). The low-energy astrophysical factor for the 7Be(p,)8B radiative capture reaction, , is the most uncertain nuclear input needed to predict the 8B solar neutrino flux Bahcall et al. (1969); Adelberger et al. (2011) in the standard solar model. It must be known at or near the Gamow peak of 18 keV, which is experimentally inaccessible due to the Coulomb barrier Brune and Davids (2015). The cross sections are unmeasurably small at these energies, so available data starting around 100 keV above the Gamow peak must be extrapolated to solar energies with the aid of theoretical models.
Descouvemont Descouvemont (2004) used a microscopic three-cluster model and a potential model to study the theoretical uncertainty in extrapolating to zero energy and found that below 1 MeV it is dominated by the uncertainties in the -wave scattering lengths for the 7Be + p system. A leading-order calculation of 7Be(p,)8B in a low-energy effective field theory Zhang et al. (2014) found that the experimental uncertainties in the scattering lengths strongly affected the calculation at energies as low as 400 keV. A simple potential model Baye (2000) shows the importance of the -wave scattering lengths in extrapolating to zero energy, although it is not clear how the results in this paper can be translated into uncertainties in the (0) value deduced from capture data. Although one recent effective field theory calculation Zhang et al. (2015) suggests that the contribution of scattering length uncertainties to the extrapolation uncertainty of below 500 keV may not be large, this sensitivity depends on the range of scattering lengths considered in the calculation.
Owing to the required use of radioactive 7Be (half-life = 53.2 days), the scattering lengths have only been measured once, by Angulo et al. Angulo et al. (2003), who found = 259 fm and = -73 fm, where is the -wave scattering length for channel spin . The -wave scattering lengths deduced from the ab-initio no-core shell model/resonating group method Navratil et al. (2011) are = -5.2 fm and = -15.3 fm. Discrepancies in the predicted and measured -wave scattering lengths, particularly for channel spin 2, demand caution when using theoretical models in the extrapolation of to zero energy. Reference Navratil et al. (2011) also calculates the astrophysical factor for 7Be(p,)8B radiative capture reaction at zero energy, but the relationship between the -wave scattering lengths and (0) is not highlighted. Better constraints on the scattering lengths may lead to a significant reduction in the uncertainty of (0), thereby reducing the overall uncertainty in the 8B neutrino flux prediction.
The evaluation of in the energy range below 100 keV depends on complete knowledge of the low-lying energy levels of 8B, which remains elusive Tilley et al. (2004). There have been several 7Be+p elastic scattering measurements aimed at elucidating the level structure of 8B. Gol’dberg et al. Gol’dberg et al. (1998) measured the elastic scattering excitation function with a thick target at relative kinetic energies from 1 to 3.6 MeV at 0∘ in inverse kinematics and proposed the existence of a level at 2.83 MeV with a width of 780 keV. Rogachev et al. Rogachev et al. (2001) measured elastic scattering using a thick target over a relative kinetic energy range from 1 to 3.3 MeV and found evidence for the existence of a level at 3.50.5 MeV with a width of 4 MeV. Angulo et al. Angulo et al. (2003) measured the 7Be+p elastic cross section with a thin polyethylene target from = 0.3 MeV to = 0.75 MeV. From an R-matrix analysis, the scattering lengths were inferred and the width of the resonance at 6345 keV was determined to be 314 keV. Yamaguchi et al. Yamaguchi et al. (2009) measured resonant elastic and inelastic scattering from 1.3 to 6.7 MeV, adducing evidence for and states. Based on an R-matrix analysis of a recent thick-target elastic and inelastic scattering measurement, Mitchell et al. Mitchell et al. (2013) proposed new low-lying , , and states at 1.9, 2.54, and 3.3 MeV, respectively, in 8B. These levels have not yet been confirmed by further experiments. Thus far there has been only a single measurement of elastic scattering below 1 MeV and the available data at higher energies are inconsistent. Based on these experiments there are only two well-known excited states of 8B, the and states at 0.77 and 2.32 MeV, respectively. All other states inferred on the basis of previous 7Be+p elastic scattering measurements require further experimental verification.
This paper describes a new measurement of the elastic and inelastic scattering cross sections of 7Be+p and a determination of the -wave scattering lengths using an R-matrix analysis. It also presents evidence for the existence of various excited states in 8B that must be properly described in theoretical models of its structure. The measurement of elastic and inelastic scattering was performed in inverse kinematics from = 0.474 MeV to 2.740 MeV covering a center-of-mass angular range of 70∘ to 150∘. We used the R-matrix method Lane and Thomas (1958) to analyze elastic and inelastic scattering data. In this work, we confirm the existence of some of the levels reported in the literature and re-assess that of others. In particular, we find no evidence in our data set for the 1+ level at 3.3 MeV that has been reported in Ref. Mitchell et al. (2013).
The experimental method used to measure the elastic and inelastic scattering is explained in Sec. II. We used a multichannel, multilevel R-matrix approach to analyze elastic and inelastic scattering data simultaneously. The best-fit parameters from the R-matrix analysis were used to determine the -wave scattering lengths using the method described in Sec. III. Section IV contains the findings of this work and a comparison with available data from the literature. We conclude in Sec. V.
II EXPERIMENT
The elastic and inelastic 7Be+p scattering cross sections were measured in inverse kinematics between 0.474 and 2.740 MeV in the center-of-mass system at the Holifield Radioactive Ion Beam Facility (HRIBF) Beene et al. (2011) of Oak Ridge National Laboratory (ORNL). 7Be was produced at the Triangle University Nuclear Laboratory using the 7Li(p,n)7Be reaction Fitzgerald (2005). The lithium targets (disks of 2-cm diameter and 3-mm thickness) were bombarded with 8- to 11-MeV protons, typically producing 240 mCi of 7Be. The activity was transported to ORNL in the form of an ingot for chemical extraction and concentration using the method described in Ref. Gialanella et al. (2002). 7Be ions were injected into the HRIBF’s tandem accelerator via a cesium sputter source. The beam was stripped to the 4+ charge state before the analyzing magnet, removing any 7Li whose maximum charge state is 3+. The fully-stripped 7Be beam was then directed into the target chamber hosting the Silicon Detector Array (SIDAR) Bardayan et al. (2000). Additional details of the experimental setup are provided in Ref. Livesay (2006).
The SIDAR consists of an array of Micron YY1 detectors with 40-keV energy resolution, which can be arranged in either a lamp-shade (with six wedges) or a flat configuration (with eight wedges). We utilized the SIDAR in the flat configuration for this experiment. The array was composed of detectors of either 300- or 500-m nominal thickness. A schematic diagram of the target station is shown in Fig. 1. Self-supporting thin foils of polypropylene (CH2) and gold (Au) were used as the targets. The thickness of the (CH2) target was determined via -particle energy loss measurements to be 100 g/cm2, with an uncertainty of 10 resulting from the stopping power calculations. The target foils were mounted on a retractable target ladder placed in the scattering chamber. There were two diagnostic tools on the ladder, namely, an aperture and a phosphor screen, which provide information about the location and size of the beam in the scattering chamber. The scattered protons were detected in the SIDAR located downstream of the target. The ionization chamber was separated from the target chamber by a 0.9-m-thick mylar window and filled with 40 T of isobutane gas. The ionization chamber was used for tuning and beam diagnostics. The unscattered beam was blocked by a 1.5-cm aluminum disk that was small enough to let the scattered 7Be ions enter into the ionization chamber.
The experiment was performed in two campaigns, for which the experimental configurations were similar. The measurements were taken using two different distances of the SIDAR from the target, providing overlapping angular ranges of 26*∘-50∘* and 14*∘-31∘*. The 7Be bombarding energies were chosen in 16 energy steps between 4 and 27 MeV with intensities of 106-107 pps at the target station. The 7Be+p scattering cross sections were measured relative to the 7Be+Au and 7Be+12C scattering cross sections, which were used for normalization of the data. The energy loss in the target was taken into account by calculating the effective beam energy as , where is the incident beam energy and is the energy loss in the target calculated using SRIM Ziegler and Biersack . This procedure is valid as long as there is no strong energy dependence of the cross section over the energy range covered in the target. Since there is a resonance at 0.634 MeV, the correction factors for the low energy experimental data points were calculated using Eqs. (6) and (7) from Ref. Brune and Sayre (2013). The correction factor calculated for the 5.2-MeV measurement in the laboratory system was 0.90, while for all other experimental data points, the correction factor was within 2 of unity. This correction factor has been included in the analysis of the =5.2 MeV measurement.
For each beam energy, there were two runs, for the purpose of separately collecting 7Be+p and 7Be+Au events. The two runs were performed with a (CH2) target and a combined target [i.e., a (CH2) foil with a Au foil in the back], respectively. The proton scattering events could be distinguished from the 7Be+12C scattering events based upon their energies as shown in Fig. 2 (a). Proton inelastic scattering events were only observed at high 7Be beam energies. The proton inelastic scattering events were well separated from the proton elastic scattering events as shown in Fig. 2 (b).
The 7Be+p scattering data were normalized to simultaneous scattering reactions. The low energy scattering data (for 7Be beam energies of = 4, 4.5, and 5.2 MeV) were normalized to the 7Be+12C scattering data, as the carbon scattering at these energies is well described by Rutherford scattering. At higher energies, the 7Be+12C scattering starts deviating from Rutherford scattering as shown in Fig 3. For 7Be beam energies of = 7, 8, 9, 10, 11, 12, 13, and 16 MeV, the 7Be+p scattering data were normalized to 7Be+12C scattering cross sections, which were themselves normalized by 7Be+Au scattering data. To utilize this normalization procedure, we need to know the carbon-to-gold ratio rather than the absolute target thickness assuming H/C=2. The carbon-to-gold ratio was determined using the ratio of differential cross sections of 7Be+12C and 7Be+Au scattering, both of which are described by Rutherford scattering at small angles. The carbon-to-gold ratio was determined to be C/Au=10.20.7, where the quoted uncertainty is statistical in nature. For 7Be beam energies of = 19.2 and 22 MeV, the proton scattering data were normalized directly to the 7Be+Au scattering data, as 7Be+Au scattering at all angles and energies covered in this experiment is well described by Rutherford scattering. For three beam energies ( = 15, 17.5, and 20 MeV), 7Be+Au scattering was not measured and 7Be+12C cross sections were not experimentally determined. For these energies the 7Be+p scattering was normalized to the 7Be+12C elastic scattering cross section calculated via the optical model using the DWUCK5 code Kunz . The 7Li+12C optical model parameters from Ref. Poling et al. (1972) were used to describe 7Be+12C elastic scattering by changing the charge and the incident energy. This parametrization was found to give a good agreement, to within 10 of the 7Be+12C elastic scattering data at energies where the normalization was determined independently.
The normalization procedures explained before depend on the ratio of the target atoms. The hydrogen-to-carbon ratio in the target was determined from the 4-MeV 7Be measurement using the ratio of 7Be+p and 7Be+12C scattering, both of which were assumed to be Rutherford scattering. The systematic uncertainty for 7Be measurements of = 4, 4.5, 5.2, 15, 17.5, and 20 MeV, which depends on the hydrogen-to-carbon ratio, was estimated to be 6. For 7Be beam energies of = 7, 8, 9, 10, 11, 12, 13, and 16 MeV, the normalization procedure depends on the carbon-to-gold ratio, and the systematic uncertainty was estimated to be 6. For measurements at = 19.2 and 22 MeV, the normalization procedure depends on the hydrogen-to-gold ratio, and the systematic uncertainty was estimated to be 7. The optical model analysis used for three beam energies ( = 15, 17.5, and 20 MeV) has an additional systematic uncertainty of 7, thus the overall systematic uncertainty for these energies was estimated to be 10.
Figure 4 shows the excitation function for elastic scattering of 7Be+p measured in this work. Circles and squares correspond to the data from the first and second experimental campaigns, respectively.
III R-MATRIX ANALYSIS
The differential scattering cross section for 7Be(p,p)7Be is described using R-matrix theory Lane and Thomas (1958). The elastic and inelastic cross-section data from this experiment and low-energy elastic scattering data from Angulo et al. Angulo et al. (2003) have been analyzed using the multilevel multichannel code AZURE2 Azuma et al. (2010). The alternative parametrization of the R-matrix theory presented in Ref. Brune (2002) is used. So, the -matrix can be expressed in terms of alternative parameters namely the observed resonance energy and the observed reduced width amplitude . A channel radius of 4.3 fm is assumed and the background poles have been fixed at particular excitation energies.
The spins of the ground and first excited states of 7Be are 3/2- and 1/2-, respectively. If we restrict our calculations up to p waves, then the allowed levels in 8B following the coupling scheme would be 0-, 0+, 1-, 1+, 2-, 2+, and 3+. The R-matrix analysis was started with the states of 8B identified in previous experiments Angulo et al. (2003); Gol’dberg et al. (1998); Rogachev et al. (2001); Yamaguchi et al. (2009); Mitchell et al. (2013), namely the 2+, 1+, 3+ and 2- levels at excitation energies of 0, 0.77, 2.32, and 3.52 MeV, respectively. The separation energies for the levels introduced in the -matrix analysis were taken from Ref. ENS . The values of the asymptotic normalization constants (ANC) used for the ground state in this analysis are =0.0990(57) fm*-1*, =0.438(23) fm*-1*, and =0.1215(36) fm*-1* Zhang et al. (2018), where the third value refers to the 7Be excited state component and the ANC’s were obtained using ab initio methods Nollett and Wiringa (2011). The fits to the scattering data is not highly sensitive to the choice of ANC values in this analysis. These states reproduce the fits to the elastic scattering data reasonably well, as shown in Fig. 5, but could not explain the inelastic scattering data. In Fig. 5(b), data points correspond to the inelastic scattering cross section for a center-of-mass angle 1194*∘*. The conversion from laboratory angle to center-of-mass angle was done taking into account the correct kinematics for inelastic scattering. Under the assumption of just the known literature values the inelastic channel was not well reproduced, so alternative level schemes were used for the -matrix parameters in order to improve the fit. Additional 0+, 1-, and 2+ states at excitation energies of 1.9, 9.0, and 2.21 MeV were introduced to improve the fits to the inelastic scattering data with no significant changes in the fits to the elastic scattering data. The 0+ level at an excitation energy of 1.9 MeV in 8B was previously suggested in Ref. Mitchell et al. (2013). The 1- level is introduced as a background level in our fits. In the phenomenological R-matrix theory, levels introduced at energies higher than the highest energy data points and with large widths are termed background levels. The solid red line in Fig. 5 represents the fit with all these levels. These levels are defined as preferred levels hereafter. It can be infered from Fig. 5 that the 2+ level at 2.21 MeV is required to fit the inelastic scattering data well. The introduction of an additional 2- level at 9.0 MeV as a background level does not change significantly the fits to the data, so it was not included in our final fit. The sensitivity of the fit to the excitation energy of the 2+ level was studied and we differ in the extracted excitation energy for such a level from Ref. Mitchell et al. (2013).
The existence of a 1+ level around 2 to 3 MeV in 8B has often been questioned. Gol’dberg et al. Gol’dberg et al. (1998) suggested a 1+ level at 2.830.150 MeV with a width of 780200 keV. Mitchell et al. Mitchell et al. (2013) introduced a 1+ level at 3.3 MeV with a width of 2.8 MeV. The recoil corrected continuum shell-model calculations in Ref. Halderson (2006) also suggested the presence of a 1+ level in 8B requiring verification by inelastic scattering measurements. The dashed blue curve in Fig. 5 shows the effect of a 1+ level at an excitation energy of 3.3 MeV along with the preferred levels. The fits to the data with and without this 1+ level can be compared in Fig. 5. There is no significant change in the elastic excitation function but the inelastic scattering cross section is underestimated. Therefore, based on the scattering data available for 7Be+p, there is no conclusive evidence for a 1+ level at an excitation energy of 3.3 MeV. Based on the analysis of these data, the level structure of the 8B is shown in Fig. 6.
III.1 Scattering length from R-matrix analysis
In this section, we relate the -wave scattering lengths to the best-fit R-matrix parameters. The collision matrix can be expressed as
[TABLE]
where . is the level matrix as defined in Ref. Brune (2002), is the penetration factor, and is the channel index. For single-channel elastic scattering Eq. (1) reduces to
[TABLE]
where
[TABLE]
The quantities and are the hard sphere phase shift and Coulomb phase shift respectively. For -wave scattering (=0), . For diagonal collision matrix elements, , where is the total phase shift. In this case, the phase shift can be related to -matrix parameters via
[TABLE]
In the low-energy limit, Eq. (4) can be written as
[TABLE]
with ; is the channel radius, is the wave number, and is the irregular Coulomb function for =0. In the limit , the effective range expansion from Bethe (1949) can be reduced to
[TABLE]
where , with the Sommerfeld parameter. From Eq. (5) and Eq. (6), the expression for the -wave scattering length ( in terms of -matrix parameters is obtained as
[TABLE]
where and are modified Bessel functions and , and are the nuclear charges, is the reduced Planck’s constant, is the reduced mass, and is the -matrix channel radius. The Coulomb functions have been expressed in terms of modified Bessel functions using Ref. Humblet (1985).
IV RESULTS
The elastic and inelastic angular distribution data from the ORNL measurement and the elastic scattering data from Ref. Angulo et al. (2003) have been fitted simultaneously. The low-energy data from Ref. Angulo et al. (2003) were introduced to constrain the fits below 1 MeV center-of-mass energy. The systematic uncertainties of both data sets were introduced in the simultaneous fitting. In AZURE2, the systematic uncertainty for the data is introduced in the normalization of the data. A systematic uncertainty of 5.5 has been assumed for the data from Ref. Angulo et al. (2003) as quoted in the paper, while the systematic uncertainties for different angular distributions from the ORNL measurement are included as explained in Sec. II. The absolute normalization of the data is allowed to vary during the fits. The output of the fit along with the chi-square values for each data segment are presented in Table 1. The best-fit parameters from the simultaneous fitting are presented in Table 2.
The fits to the elastic angular distributions are presented in Figs. 7, 8, and 9 and the fits to the inelastic angular distributions are presented in Fig. 10 and Fig. 11. The fits to data from Ref. Angulo et al. (2003) are shown in Fig. 12.
Using the best-fit parameters from Table 2 and Eq. (7), the -wave scattering lengths for channel spins 1 and 2 were calculated to be 17.34 and -3.18 fm, respectively. To illustrate the sensitivity of the fit to the reduced width amplitudes of the 1- and 2- levels, the reduced width amplitudes for these levels were varied and the changes in the total were compared. A change of =1 is used to define the acceptable range of the reduced width amplitudes for these levels, which gives the error bars in the scattering length values for channel spins 1 and 2, respectively. Using the same approach, the 1- error bar was estimated for the parameters of the 0+ and 2+ levels. The widths of the 0+ level are =0.1200.028 MeV and =0.4280.130 MeV, where and refer to the elastic and inelastic channel widths, respectively. Similarly, the widths of the 2+ level are =0.0240.009 MeV and =0.2300.001 MeV. The excitation energies of the 0+ and 2+ levels are 1.90.1 and 2.210.04 MeV, respectively. Our excitation energy for the 2+ level differs from the value presented in Ref. Mitchell et al. (2013). The elastic proton partial width for the 1+ state (0.77 MeV) from our analysis is in agreement with the value reported in Ref. Angulo et al. (2003).
Table 1 lists the values of the fit to each data set. The fits to the first two data segments in both the elastic and the inelastic scattering from this work have a large . There are no obvious reasons for this, but point-to-point uncertainty is one possible explanation. Sensitivity tests were performed by excluding segments with large values (i.e., /N >2) and segments with normalization factors above or below 20 (i.e, Norm <0.80 and Norm >1.20). Excluding segments with /N >2 does not affect the normalizations of the included segments considerably. Similar conclusions were obtained by excluding the segments following the normalization criterion. Also, the data from Ref. Angulo et al. (2003) were fitted alone, starting with the parameters in Table 2, to evaluate the effects on the scattering length values. If the well-known states [2+ (ground state), 1+ (0.77 MeV), and 3+ (3.52 MeV)] alone are included to fit the data from Ref. Angulo et al. (2003) along with the 2- and 1- background levels, we obtain -wave scattering lengths consistent with the results in Ref. Angulo et al. (2003). But with the introdution of the inelastic channel along with the inclusion of the 0+ (1.9-MeV), and 2+ (2.21-MeV) states, the results for the -wave scattering lengths differ significantly from the results in Ref. Angulo et al. (2003). The scattering lengths obtained from this analysis along with the values published in the literature are presented in Table 3. Angulo et al. made the only previous determination of -wave scattering lengths for the 7Be+p system, where the cross-section data have been analyzed in an -matrix framework and the -wave scattering lengths have been deduced. Navratil et al. Navratil et al. (2011) used the ab initio no-core shell model/resonating group method to calculate the 7Be(p,)8B radiative capture cross section and deduce the -wave scattering lengths for 7Be+p. The -wave scattering lengths from Ref. Navratil et al. (2011) do not agree with the results of this analysis.
In the context of the potential model Baye (2000), the extrapolation of down to solar energies depends on the value of the average scattering length (), defined as
[TABLE]
The value deduced from this work is 0.60 fm using the ANC values from Ref. Zhang et al. (2018) neglecting their uncertainties. This shows that the average scattering length can be better constrained than the individual scattering lengths for channel spins 1 and 2, respectively.
V CONCLUSIONS
The angular distributions for 7Be+p elastic and inelastic scattering were measured in the center-of-mass energy range 0.474-2.740 MeV and center-of-mass angular range 70∘-150∘. Simultaneous fits of the angular distributions from this measurement and the excitation functions from Ref. Angulo et al. (2003) indicate the existence of a 0+ state at 1.9 MeV and a 2+ state at 2.21 MeV in 8B. These states are required to explain the inelastic scattering excitation function, which shows a clear peak at 2.2 MeV. The results of this analysis do not provide conclusive evidence for the existence of a 1+ level at 3.3 MeV in 8B.
The experimental determination of -wave scattering lengths for the 7Be+p system from an R-matrix analysis of elastic and inelastic scattering data has been presented. The scattering length for channel spin 1 is in agreement with the previously reported scattering length in Ref. Angulo et al. (2003). Our result for channel spin 2 lies just outside the 1- lower limit of the scattering length reported in Ref. Angulo et al. (2003). The general agreement between our results and those in Ref. Angulo et al. (2003) is not surprising, as the low-energy scattering data in Ref. Angulo et al. (2003) play a very significant role in both analyses. It can be inferred from Table 3 that the uncertainties in the -wave scattering lengths have been reduced by a factor of 5-8 compared to the previous experimental measurement Angulo et al. (2003). This lower uncertainty may reduce the overall uncertainty in (0), as discussed by Descouvemont Descouvemont (2004) and Baye Baye (2000). Using the potential model of Baye, the uncertainty in (0) due to the average scattering length can be calculated using Eq. (20) from Ref. Baye (2000). Using this approach, the uncertainty in the average scattering length deduced in this work using Eq. (8) contributes the very small uncertainty of 0.03 to (0), although it is not clear how this uncertainty impacts the extrapolation error on the (0) value deduced from capture data.
Besides this measurement, there is only one 7Be+p elastic scattering measurement below 1 MeV. The measurements above this energy are not in agreement with each other. To better constrain the fits and the R-matrix parameters, more precise measurements are needed. Measurements below the 634-keV resonance are most important for constraining the scattering lengths. However, the data at higher energies are also important. Ideally, new scattering measurements would span a wide range of energy, from below the 634-keV resonance to well above 1 MeV. Transfer reactions could shed more light onto the structure of 8B.
Acknowledgements.
We are grateful to R. J. deBoer for his assistance with AZURE2. We thank D. R. Phillips for taking part in constructive discussions. This work was supported in part by the U.S. Department of Energy under Grants No. DE-NA0002905, No. DE-NA0003883, No. DE-FG02-88ER40387, and DE-FG02-93ER40789 and Contract No. DE-AC05-00OR22725 (ORNL). D. W. B. acknowledges support from NSF under Grant No. PHY-1713857. B. D. acknowledges support from NSERC, Canada. The work of K. Y. C. was supported in part by a National Research Foundation of Korea (NRF) Grants No. NRF-2016R1A5A1013277 and No. NRF-2013M7A1A1075764 funded by the Korean government (MEST). This research used resources of the Holifield Radioactive Ion Beam Facility, which was a DOE Office of Science User Facility operated by the Oak Ridge National Laboratory. The authors are grateful to the staff of the HRIBF whose hard work made the experiment possible.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1Aharmim et al. (2013) B. Aharmim et al. (SNO Collaboration), Phys. Rev. C 88 , 025501 (2013) . · doi ↗
- 2Abe et al. (2016) K. Abe et al. (Super-Kamiokande Collaboration), Phys. Rev. D 94 , 052010 (2016) . · doi ↗
- 3Haxton et al. (2013) W. C. Haxton, R. G. Hamish Robertson, and A. M. Serenelli, Annual Review of Astronomy and Astrophysics 51 , 21 (2013) , https://doi.org/10.1146/annurev-astro-081811-125539 . · doi ↗
- 4Bahcall et al. (1969) J. N. Bahcall, N. A. Bahcall, and R. K. Ulrich, Astrophys. J. 156 , 559 (1969) . · doi ↗
- 5Adelberger et al. (2011) E. G. Adelberger, A. García, R. G. H. Robertson, K. A. Snover, A. B. Balantekin, K. Heeger, M. J. Ramsey-Musolf, D. Bemmerer, A. Junghans, C. A. Bertulani, J.-W. Chen, H. Costantini, P. Prati, M. Couder, E. Uberseder, M. Wiescher, R. Cyburt, B. Davids, S. J. Freedman, M. Gai, D. Gazit, L. Gialanella, G. Imbriani, U. Greife, M. Hass, W. C. Haxton, T. Itahashi, K. Kubodera, K. Langanke, D. Leitner, M. Leitner, P. Vetter, L. Winslow, L. E. Marcucci, T. Motobayashi, A. M · doi ↗
- 6Brune and Davids (2015) C. R. Brune and B. Davids, Annual Review of Nuclear and Particle Science 65 , 87 (2015) . · doi ↗
- 7Descouvemont (2004) P. Descouvemont, Phys. Rev. C 70 , 065802 (2004) . · doi ↗
- 8Zhang et al. (2014) X. Zhang, K. M. Nollett, and D. R. Phillips, Phys. Rev. C 89 , 051602 (2014) . · doi ↗
