Spectroscopic study on \textsuperscript{39}Ca for classical nova endpoint nucleosynthesis

ORAL

Abstract


 In classical nova nucleosythesis repeated proton capture reactions and beta-decays produce proton-rich isotopes and the endpoint of this nucleosynthesis typically occurs in nuclei close to A $\sim$ 40. There is currently a discrepancy between the observed and predicted isotopic abundances in this mass region. One particular reaction, $^{38}$K(p,$\gamma$)$^{39}$Ca is important in this regard. Nova simulations show that this reaction can affect isotopic abundances of $^{38}$Ar, $^{39}$Ar, and $^{40}$Ca significantly when the reaction rate is varied by its maximum uncertainty. Thus, it is important to constrain uncertainties of this reaction rate to accurately predict isotopic abundances.\\
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Although a recent direct measurement has reduced the reaction rate uncertainty, further work is needed to constrain this reaction rate. Specifically, additional measurements to precisely probe the low energy resonances within the Gamow window. To that end, I will present the results of measuring these astrophysically important levels in $^{39}$Ca using the reaction $^{40}$Ca(d,t)$^{39}$Ca. The experiment was carried out at the Maier-Leibnitz-Laboratory (MLL) using the 14 MV MP-Tandem accelerator and Quadrupole 3-Dipole (Q3D) magnetic spectrograph.

Presenters

  • Johnson Liang

    McMaster Univ

Authors

  • Johnson Liang

    McMaster Univ

  • A. A. Chen

    McMaster University, McMaster Univ

  • Marius Anger

    Technical University Munich

  • Shawn Bishop

    Technical University Munich

  • Thomas Faestermann

    Technical University Munich

  • Cathleen E E Fry

    Michigan State Univ

  • Ralf Hertenberger

    Ludwing-Maximilians-University Munich

  • Athanasios Psaltis

    McMaster University, McMaster Univ

  • Dominik Seiler

    Technical University Munich

  • Pranjal Tiwari

    Michigan State Univ

  • Hans-Friedrich Wirth

    Ludwing-Maximilians-University Munich

  • Christopher Lars Henrik Lars Henrik Wrede

    Michigan State Univ