1 / 23

Extending the Bertini Cascade Model to Kaons

Dennis H. Wright (SLAC) Monte Carlo 2005 17-21 April 2005. Extending the Bertini Cascade Model to Kaons. Outline. The Bertini cascade vs. LEP model Extending the Bertini model to kaons cross sections final state generation

layne
Download Presentation

Extending the Bertini Cascade Model to Kaons

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Dennis H. Wright (SLAC) Monte Carlo 2005 17-21 April 2005 Extending the Bertini Cascade Model to Kaons

  2. Outline • The Bertini cascade vs. LEP model • Extending the Bertini model to kaons • cross sections • final state generation • intra-nuclear propagation • Validation • quasi-elastic scattering • strangeness exchange • Conclusions and Plans

  3. Motivation • Propagation of low and medium energy particles (0 – 5 GeV) is important for: • validating medium energy experiments now in progress • calorimetry in planned high energy experiments • Traditionally, p, n and p have received most of the attention at these energies: • comprisemostofthehadronicshower • treatedby 3 Geant4 models • Kaons, hyperons and anti-particles are of interest too • onlyoneGeant4 model handles them • more accurate alternative required

  4. Bertini Cascade vs. Low Energy Parameterized Model • LowEnergyParameterizedModel (LEP) • handles p, n, p, K, hyperons, anti-particles • derived from GHEISHA and not especially suited for low energies • no intra-nuclear physics included • quantum numbers conserved on average over events • BertiniCascadeModel • currentlyhandlesonly p, n, p, butstraightforwardtoextendtokaons,hyperons • appropriate for E < 10 GeV, validated at ~1 GeV and below • intra-nuclear cascade included • quantum numbers conserved event-by-event

  5. Extending the Bertini Cascade: Cross Sections (1) • Model uses free-space cross sections for projectiles and cascade particles interacting within nucleus => parameterize existing data • Large amount of (K+,p) (K+,n) (K-,p) (K-,n) data • But what about K0 and anti-K0 ? • nodata • useisospintogetcrosssectionsfromchargedkaondata=>sK0p=sK+n , sK0barn=sK-p • For interaction of cascade-generated particles, also need (L,p) (L,n) (S,p) ...... • alittle data forthese • useisospin,strangeness,chargeconservationtofillin

  6. Extending the Bertini Cascade: Cross Sections (2) • All data taken from CERN particle reaction catalogs • Data for all kaon and hyperon-induced reactions thin out at about 15 GeV => inherent limit of the model • At the higher energies (>5 GeV) use total inelastic cross section data to partition cross section strength among various channels where it is not known

  7. Extending the Bertini Cascade: Final State Generation (1) • Foreachinteractiontype(K+,p),(S+,n),...,themodelkeepsalistoffinalstatechannels: • store multiplicity and particle type • angular distibution parameters • all functions of incident energy • Un-modifiedmodelhandlesupto6-bodyfinalstates • validupto10GeV • Extendedmodelhandlesupto7-bodyfinalstates • validupto ~15GeV • includeskaonsandlowestmasshyperons • doesnotincluderesonances

  8. Extending the Bertini Cascade: Final State Generation (2) • Angular distributions • lots of data for two-body final states below 3 GeV => parameterize as function of incident energy • for > 2-body, use phase space calculation • above 3 GeV, everything is forward peaked, parameterize using exponential decay • luckily, more than one interaction occurs in cascade => distributions are smeared and precise data are not required • Momentum distributions • some data for 3-body final states • otherwise use phase space calculation

  9. Extending the Bertini Cascade: Intra-nuclear Propagation • Model propagates particles from the final state of the elementary interaction to the site of the next interaction • requires a knowledge of the nuclear potential for each particle type • current model uses a detailed 3D model of the nucleus • p, n potentials well-known, pion potential less well-known • potentials for strange particles almost unknown • Model includes other propagation features: • Pauli blocking for nucleons • nucleon-nucleon correlations (pion absorption) • kaon absorption not yet included

  10. Validation • Quasi-elasticK+scattering • Kormanyos et al., 1995 • Targets: D, C, Ca, Pb • 0.7 GeV/c incident K+ , detect K+ at 24o and 430 • Sensitive to Fermi motion, depth of potential for kaons • Strangeness exchange (K- , p-) • Bruckner et al., 1975, 1976 • Targets: Be, C, O, S, Ca • 0.9 GeV/c incident K- , detect 0o pions • Sensitive to nuclear potential seen by kaons, hyperons

  11. Qausi-elastic: 705 MeV/c K+ on Pb

  12. Quasi-elastic: 705 MeV/c K+ on Ca

  13. Qausi-elastic: 705 MeV/c K+ on C

  14. Quasi-elastic: 705 MeV/c K+ on D

  15. Note on previous 4 slides: • ComparisonstoLEPmodelarenotshownbecause: • no final state K+ produced at these energies • none seen until incident momentum exceeds 2 GeV/c • model converts K+ to K0L , K0S and pions

  16. Strangeness Exchange: 0.9 GeV/c (K-, p-) on Ca

  17. Strangeness Exchange: 0.9 GeV/c (K- , p-) on S

  18. Strangeness Exchange: 0.9 GeV/c (K- , p-) on O

  19. Strangeness Exchange: 0.9 GeV/c (K- , p-) on C

  20. Strangeness Exchange: 0.9 GeV/c (K-, p-) on Be

  21. Conclusions: K+ Quasi-elastic Scattering • For all nuclei tested, Bertini cascade is clearly better than LEP at < 2 GeV/c • LEP removes kaons, Bertini conserves them • Bertini reproduces energy of quasi-elastic peak • Some drawbacks: • Bertini under-estimates the width of the QE peak • better kaon-nuclear potentials might fix this • overall normalization is about 30% low for all targets • this could be due to uncertainties in the total inelastic cross section, which itself is parameterized

  22. Conclusions: Strangeness Exchange • For all nuclei tested at 0.9 GeV/c Bertini cascade is again better than LEP • LEP is not so bad for heavy nuclei, but Bertini is better • for light nuclei, only Bertini reproduces the quasi-elastic peak • for all targets, Bertini reproduces the normalization fairly well => total inelastic cross section at 0.9 GeV/c is OK • Some drawbacks: • for light nuclei Bertini does not reproduce the energy of the QE peak • better kaon-nuclear potentials might fix this

  23. Plans for Future Development • Nearterm • complete theparameterizationofmomentumandangulardistributionsforstrangeparticlefinalstates • tunekaon-andhyperon-nuclearpotentialdepthstobetterreproducedata • testtheextendedmodelfor incident K0L and L • Longer term • add strange pair production to p-, n- and pion-induced reactions • extend validity of p-, n- and pion-induced reactions to 15 GeV • add anti-proton and anti-neutron induced reactions

More Related