Neutron capture rates of C18

M. Dan, G. Singh, R. Chatterjee, and Shubhchintak
Phys. Rev. C 99, 035801 – Published 6 March 2019

Abstract

Background: Small changes in reaction rates due to neutron capture, α capture, and β decay by exotic nuclei in the low and medium mass region can direct the r-process path in different ways, thereby affecting the abundance pattern. In this context, it is important to find the most abundant carbon isotope closer to the neutron drip line. It was postulated that the (n,γ) reaction network will be broken at the C18 isotope and follow the C18(α,n)O21 reaction path [Terasawa et al., Astrophys. J. 562, 470 (2001)].

Purpose: In this paper, we calculate the radiative capture cross section of C18(n,γ)C19, taking into consideration the halo character of C19. Eventually, we calculate the reaction rate for the same reaction and compare it with Hauser-Feshbach estimates of (n,γ) and (α,n) to determine the abundance pattern of carbon isotopes.

Method: We compute the relative energy spectrum for elastic Coulomb breakup of C19 on a Pb target at a beam energy of 67 MeV/u using the finite-range distorted-wave Born approximation (FRDWBA) theory. We use the principle of detailed balance to calculate the radiative capture cross section from the photo disintegration cross section, and subsequently we calculate the reaction rate.

Results: We report the C18(n,γ)C19 capture cross section as a function of relative energy. Estimation of the energy range contributing to the reaction rates is done by calculating the integrand of the reaction rate expression. A comparison of the C18(n,γ)C19 with C18(α,n)O21 (extracted from the Hauser-Feshbach estimates) shows the domination of the neutron radiative capture reaction in the relevant temperature range T9=0.14.

Conclusion: The radiative capture cross section of C18 calculated using FRDWBA theory agrees well with the experimental data, whereas the statistical model calculation lies orders of magnitude lower. We conclude that at equilibrium temperature of T9=0.62, the C18(n,γ)C19 reaction rate is orders of magnitude higher than that of the C18(α,n)O21 reaction, thereby pushing the carbon isotope abundance towards the neutron drip line.

  • Figure
  • Figure
  • Figure
  • Figure
  • Received 17 October 2018

DOI:https://doi.org/10.1103/PhysRevC.99.035801

©2019 American Physical Society

Physics Subject Headings (PhySH)

Nuclear Physics

Authors & Affiliations

M. Dan*, G. Singh, and R. Chatterjee

  • Department of Physics, Indian Institute of Technology - Roorkee, Roorkee 247667, India

Shubhchintak§

  • Physique Nucléaire Théorique et Physique Mathématique, C.P. 229, Université Libre de Bruxelles (ULB), B-1050 Brussels, Belgium

  • *mdan@ph.iitr.ac.in
  • Present address: Department of Physics, Indian Institute of Technology - Delhi, New Delhi 110016, India; gagandph@iitr.ac.in
  • rcfphfph@iitr.ac.in
  • §shubhchintak@ulb.ac.be

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 99, Iss. 3 — March 2019

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review C

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×