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Title: The Link Between Rare-Earth Peak Formation and the Astrophysical Site of the R Process

Abstract

The primary astrophysical source of the rare-earth elements is the rapid neutron capture process (r process). The rare-earth peak that is seen in the solar r-process residuals has been proposed to originate as a pile-up of nuclei during the end of the r process. We introduce a new method utilizing Monte Carlo studies of nuclear masses in the rare-earth region, that includes self-consistently adjusting β-decay rates and neutron capture rates, to find the mass surfaces necessary for the formation of the rare-earth peak. We demonstrate our method with two types of astrophysical scenario, one corresponding to conditions typical of hot winds from core-collapse supernovae and stellar-mass accretion disks, and one corresponding to conditions typical of the ejection of the material from the tidal tails of neutron star mergers. In each type of astrophysical condition, this method successfully locates a region of enhanced stability in the mass surface that is responsible for the rare-earth peak. For each scenario, we find that the change in the mass surface has qualitatively different features, thus future measurements can shed light on the type of environment in which the r process occurred.

Authors:
ORCiD logo [1]; ORCiD logo [2];  [3]; ORCiD logo [4]
  1. Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Univ. of Notre Dame, IN (United States). Dept. of Physics
  2. North Carolina State Univ., Raleigh, NC (United States). Dept. of Physics
  3. Univ. of Notre Dame, IN (United States). Dept. of Physics
  4. Univ. of Tennessee, Knoxville, TN (United States). Dept. of Physics and Astronomy; Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Physics Division
Publication Date:
Research Org.:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States); Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Nuclear Physics (NP); USDOE National Nuclear Security Administration (NNSA); National Science Foundation (NSF)
OSTI Identifier:
1419745
Alternate Identifier(s):
OSTI ID: 1460246
Report Number(s):
LA-UR-16-21461
Journal ID: ISSN 1538-4357; TRN: US1801381
Grant/Contract Number:  
AC52-06NA25396; PHY1554876; PHY0822648; PHY1419765; SC0013039; FG02-02ER41216; AC05-00OR22725
Resource Type:
Accepted Manuscript
Journal Name:
The Astrophysical Journal (Online)
Additional Journal Information:
Journal Name: The Astrophysical Journal (Online); Journal Volume: 833; Journal Issue: 2; Journal ID: ISSN 1538-4357
Publisher:
Institute of Physics (IOP)
Country of Publication:
United States
Language:
English
Subject:
79 ASTRONOMY AND ASTROPHYSICS; Atomic and Nuclear Physics; Astronomy and Astrophysics; r-process, nuclear masses; nuclear reactions; nucleosynthesis; abundances

Citation Formats

Mumpower, Matthew R., McLaughlin, Gail C., Surman, Rebecca, and Steiner, Andrew W. The Link Between Rare-Earth Peak Formation and the Astrophysical Site of the R Process. United States: N. p., 2016. Web. doi:10.3847/1538-4357/833/2/282.
Mumpower, Matthew R., McLaughlin, Gail C., Surman, Rebecca, & Steiner, Andrew W. The Link Between Rare-Earth Peak Formation and the Astrophysical Site of the R Process. United States. https://doi.org/10.3847/1538-4357/833/2/282
Mumpower, Matthew R., McLaughlin, Gail C., Surman, Rebecca, and Steiner, Andrew W. Tue . "The Link Between Rare-Earth Peak Formation and the Astrophysical Site of the R Process". United States. https://doi.org/10.3847/1538-4357/833/2/282. https://www.osti.gov/servlets/purl/1419745.
@article{osti_1419745,
title = {The Link Between Rare-Earth Peak Formation and the Astrophysical Site of the R Process},
author = {Mumpower, Matthew R. and McLaughlin, Gail C. and Surman, Rebecca and Steiner, Andrew W.},
abstractNote = {The primary astrophysical source of the rare-earth elements is the rapid neutron capture process (r process). The rare-earth peak that is seen in the solar r-process residuals has been proposed to originate as a pile-up of nuclei during the end of the r process. We introduce a new method utilizing Monte Carlo studies of nuclear masses in the rare-earth region, that includes self-consistently adjusting β-decay rates and neutron capture rates, to find the mass surfaces necessary for the formation of the rare-earth peak. We demonstrate our method with two types of astrophysical scenario, one corresponding to conditions typical of hot winds from core-collapse supernovae and stellar-mass accretion disks, and one corresponding to conditions typical of the ejection of the material from the tidal tails of neutron star mergers. In each type of astrophysical condition, this method successfully locates a region of enhanced stability in the mass surface that is responsible for the rare-earth peak. For each scenario, we find that the change in the mass surface has qualitatively different features, thus future measurements can shed light on the type of environment in which the r process occurred.},
doi = {10.3847/1538-4357/833/2/282},
journal = {The Astrophysical Journal (Online)},
number = 2,
volume = 833,
place = {United States},
year = {Tue Dec 20 00:00:00 EST 2016},
month = {Tue Dec 20 00:00:00 EST 2016}
}

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Cited by: 14 works
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Works referencing / citing this record:

Reverse engineering nuclear properties from rare earth abundances in the r process
journal, February 2017

  • Mumpower, M. R.; McLaughlin, G. C.; Surman, R.
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Reverse engineering nuclear properties from rare earth abundances in the $r$ process
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