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The R-matrix method and 12 C( ) 16 O Pierre Descouvemont Université Libre de Bruxelles, Brussels, Belgium 1.Introduction 2.The R-matrix formulation: elastic scattering and capture 3.Application to 12 C( ) 16 O 4.Conclusions and outlook
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Introduction Many applications of the R-matrix theory in various fields “Common denominator” to all models and analyses Can mix theoretical and experimental information Two types of applications:data fitting variational calculations Application to 12 C( ) 16 O: nearly all recent papers References: A.M. Lane and R.G. Thomas, Rev. Mod. Phys. 30 (1958) 257 F.C. Barker, many papers
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R-matrix formulation Main idea: to divide the space into 2 regions (radius a) Internal: r ≤ a: Nuclear + coulomb interactions External: r > a: Coulomb only Internal region 16 O Entrance channel 12 C+ Exit channels 12 C(2 + )+ 15 N+p, 15 O+n 12 C+ Coulomb Nuclear+Coulomb: R-matrix parameters Coulomb In practice limited to low energies (each J must be considered individually). well adapted to nuclear astrophysics
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Example: 12 C+ Physical parameters = “observed” parameters Resonances: R-matrix parameters = “formal” parameters Poles: Similar but not equal 16 O 1 -, E R =2.42 MeV, =0.42 MeV Reduced width 2 : =2 2 P(E R ), with P = penetration factor 12 C+ R-matrix parameters = poles
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Background pole Isolated resonances: Treated individually High-energy states with the same J Simulated by a single pole = background Energies of interest Non resonant calculations possible: only a background pole
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a.Hamiltonian: H =E With, for r large: I l, O l = Coulomb functions U l = collision matrix (→ cross sections) = exp(2i l ) for single-channel calculations Total wave function b. Wave functions Set of N basis functions u (r) with Derivation of the R matrix (elastic scattering)
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c.Bloch-Schrödinger equation: With L = Bloch operator (restore the hermiticity of H over the internal region) Replacing int (r) and ext (r) by their definition:
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Solving the system, one has: R-matrix parameters R matrix =reduced width P=penetration factor S=shift factor Reduced width: proportional to the wave function in a ”measurement of clustering” Dimensionless reduced width “first guess”: 2 =0.1 Total width: Depend on a
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Penetration and shift factors P(E) and S(E)
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Two approaches: 1.Fit: The number of poles N is determined from the physics of the problem In general, N=1 but NOT in 12 C( ) 16 O : N=3 or 4 (or more) are fitted Phase shift: 2.Variational calculations (ex: microscopic calculations): N= number of basis functions are calculated (depend on a, but should not)
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Breit-Wigner approximation: peculiar case where N=1 One-pole approximation: N=1 Resonance energy: Thomas approximation: Then R-matrix parameters (calculated) Observed parameters (=data)
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Capture cross sections in the R-matrix formalism New parameters: = gamma width of the poles = interference sign between the poles is equivalent to the Breit-Wigner approximation if N=1 Relative phase between M int and M ext : ±1 M int and M ext are NOT independent of each other: a must be common U in M ext should be derived from R in M int Sometimes in the literature: exp(-Kr)
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Extension to 12 C( ) 16 O: N>1 Problem: many experimental constraints (energies, and widths) → how to include them in the R-matrix fit? Previous techniques: fit of the R-matrix parameters 2+ 11.52 3 poles + background → 12 R-matrix parameters to be fitted + constraints (experimental energies, widths) New technique: start from experimental parameters (most are known) and derive R matrix parameters strong reduction of the number of parameters!
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Generalization of the Breit-Wigner formalism: link between observed and formal parameters when N>1 C. Angulo, P.D., Phys. Rev. C 61, 064611 (2000) C. Brune, Phys. Rev. C 66, 044611 (2002) idea: Information for E2: 2 + phase shift E2 S-factor spectroscopy of 2 + states in 16 O: energy and widths
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2+ 11.52 Three 2 + states + background Energy (MeV) width (MeV) width (eV) -0.24?0.097 2.683.68 x 10 -4 0.0057 4.361.39 x 10 -2 0.61 Backg.10?? 3 parameters + interference signs in capture 2 steps:1) phase shifts: widths 2) S factor: width of the background the S-factor is fitted with a single free parameter From phase shift From S factor Application to 12 C( ) 16 O: E2 contribution Main goal: to reduce the number of free parameters
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First step: fit of the 2 + phase shift 2 parameters:
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Phase shift: Strong influence of the background! 2+ 11.52
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Second step: fit of the E2 S-factor 1 remaining parameter: 4 poles→4 signs 1, 2, 3, 4, 1 =+1 (global sign) 4 =+1 (very poor fits with 4 =-1) S E2 (300 keV)=190-220 keV-b
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Paper by Kunz et al., Astrophy. J. 567 (2002) 643 Similar analysis (with new data) S E2 (300 keV)=85 ± 30 keV-b very different result
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Origin: difference in the background treatment Here: background at 10 MeV Kunz et al.: background at 7.2 MeV R matrix: S factor at 300 keV“well” knownbackground Between 1~3 MeV, terms 1 and 4: have opposite signs are large and nearly constant Several equivalent possibilities -scattering does not provide without ambiguities! Consistent with a recent work by J.M. Sparenberg
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Recent work by J.-M. Sparenberg: Phys. Rev. C69 (2004) 034601 Based on supersymmetry (D. Baye, Phys. Rev. Lett. 58 (1987) 2738) acts on bound states of a given potential without changing the phase shifts VV Supersymmetric transformation Both potentials have exactly the same phase shifts (different wave functions) r r Original potential Transformed potential
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With this method: different potentials with Same phase shifts Different bound-state properties Example: V(r)=V 0 exp(-(r/r 0 ) 2 )/r 2, with V 0 =43.4 MeV, r 0 =5.09 fm No bound state V(r) Supersymmetric partners Identical phase shifts!
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Conclusion: It is possible to define different potentials giving the same phase shifts but different No direct link between the phase shifts and the bound-state properties Consistent with the disagreement obtained for R-matrix analyses using different background properties (~ potential) the background problem should be reconsidered!
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One indirect method: cascade transitions to the 2 + state F.C. Barker and T. Kajino, Aust. J. Phys. 44 (1991) 369 L. Buchmann, Phys. Rev. C64 (2001) 022801 Weakly bound: -0.24 MeV Capture to 2 + is essentially external M int negligible The cross section to the 2 + state is proportional to
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12 C( ) 16 O is probably the best example where the interplay between experimentalists, theoreticians and astrophysicists is the most important Required precision level too high for theory alone we essentially rely on experiment E1 probably better known than E2 ( 16 N -decay) Elastic scattering is a useful constraint, but not a precise way to derive Possible constraints from astrophysics? New project 16 O+ → 12 C (Triangle, North-Carolina) “Final” conclusions What do we know?
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What do we need? Theory: reconsider background effects Precise E1/E2 separation (improvement on E2) Capture to the 2+ state Data with lower error bars: precise data near 1.5 MeV are more useful than data near 1 MeV with a huge error Please avoid this!
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