s-Processing from MHD-Induced Mixing and Isotopic Abundances in Presolar SiC Grains

S. Palmerini, , O. Trippella, M. Busso, D. Vescovi, M. Petrelli, A. Zucchini, F. Frondini
Geochimica et Cosmochimica Acta (in Press) Link to Article [https://doi.org/10.1016/j.gca.2017.05.030]
Dipartimento di Fisica e Geologia, Università degli Studi di Perugia, Italia, INFN, Sezione di Perugia, Italia
Copyright Elsevier

In the past years the observational evidence that s-process elements from Sr to Pb are produced by stars ascending the so-called Asymptotic Giant Branch (or “ AGB”) could not be explained by self-consistent models, forcing researchers to extensive parameterizations. The crucial point is to understand how protons can be injected from the envelope into the He-rich layers, yielding the formation of presup13C and then the activation of the presup13C(α  ,n)presup16O reaction. Only recently, attempts to solve this problem started to consider quantitatively physically-based mixing mechanisms. Among them, MHD processes in the plasma were suggested to yield mass transport through magnetic buoyancy. In this framework, we compare results of nucleosynthesis models for Low Mass AGB Stars (M≲3M), developed from the MHD scenario, with the record of isotopic abundance ratios of s-elements in presolar SiC grains, which were shown to offer precise constraints on the presup13C reservoir. We find that n-captures driven by magnetically-induced mixing can indeed account for the SiC data quite well and that this is due to the fact that our presup13C distribution fulfils the above constraints rather accurately. We suggest that similar tests should be now performed using different physical models for mixing. Such comparisons would indeed improve decisively our understanding of the formation of the neutron source.

Iron and nickel isotope compositions of presolar silicon carbide grains from supernovae

János Kodolányia, Thomas Stephanb,c, Reto Trappitschb,c,d, Peter Hoppea, Marco Pignatarid,e, Andrew M. Davisb,c,f, Michael J. Pellinb,c,f,g
Geochimica et Cosmochimica Acta (in Press) Link to Article [https://doi.org/10.1016/j.gca.2017.05.029]
aMax Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany
bChicago Center for Cosmochemistry
cDepartment of the Geophysical Sciences, The University of Chicago, 5734 S Ellis Ave, Chicago, IL 60637, USA
dThe NuGrid Collaboration1
eE. A. Milne Centre for Astrophysics, University of Hull, Hull, HU6 7RX, UK
fEnrico Fermi Institute, The University of Chicago, Chicago, IL 60637, USA
gMaterials Science Division, Argonne National Laboratory, Argonne, IL 60439, USA
Copyright Elsevier

We report the carbon, silicon, iron, and nickel isotope compositions of twenty-five presolar SiC grains of mostly supernova (SN) origin. The iron and nickel isotope compositions were measured with the new Chicago Instrument for Laser Ionization, CHILI, which allows the analysis of all iron and nickel isotopes without the isobaric interferences that plagued previous measurements with the NanoSIMS. Despite terrestrial iron and nickel contamination, significant isotopic anomalies in 54Fe/56Fe, 57Fe/56Fe, 60Ni/58Ni, 61Ni/58Ni, 62Ni/58Ni, and 64Ni/58Ni were detected in nine SN grains (of type X). Combined multi-isotope data of three grains with the largest nickel isotope anomalies (>100 ‰ or <−100 ‰ in at least one isotope ratio, when expressed as deviation from the solar value) are compared with the predictions of two SN models, one with and one without hydrogen ingestion in the He shell prior to SN explosion. One grain’s carbon-silicon-iron-nickel isotope composition is consistent with the prediction of the model without hydrogen ingestion, whereas the other two grains’ isotope anomalies could not be reproduced using either SN models. The discrepancies between the measured isotope compositions and model predictions may indicate element fractionation in the SN ejecta prior to or during grain condensation, and reiterate the need for three-dimensional SN models.

Rare Earth Element abundances in presolar SiC

T.R. Irelanda,b, J.N. Ávilaa,b, M. Lugaroc, S. Cristallod, P. Holdena, P. Lanca, L. Nittlere, C.M.O’D. Alexandere, F. Gyngardf, S. Amarif
Geochimica et Cosmochimica Acta (in Press) Link to Article [https://doi.org/10.1016/j.gca.2017.05.027]
aResearch School of Earth Sciences, The Australian National University, Canberra ACT 2601, Australia
bPlanetary Science Institute, The Australian National University, Canberra ACT 2601, Australia
cKonkoly Observatory, Hungarian Academy of Sciences, Budapest, Hungary
dINAF – Osservatorio Astronomico di Teramo, 64100, Italy
eDepartment of Terrestrial Magnetism, Carnegie Institution of Washington, Washington DC 20015, USA
fLaboratory for Space Sciences, Physics Dept., Washington University, St. Louis, MO 63130, USA
Copyright Elsevier

Individual isotope abundances of Ba, lanthanides of the rare earth element (REE) group, and Hf have been determined in bulk samples of fine-grained silicon carbide (SiC) from the Murchison CM2 chondrite. The analytical protocol involved secondary ion mass spectrometry with combined high mass resolution and energy filtering to exclude REE oxide isobars and Si-C-O clusters from the peaks of interest. Relative sensitivity factors were determined through analysis of NIST SRM reference glasses (610 and 612) as well as a trace-element enriched SiC ceramic. When normalised to chondrite abundances, the presolar SiC REE pattern shows significant deficits at Eu and Yb, which are the most volatile of the REE. The pattern is very similar to that observed for Group III refractory inclusions. The SiC abundances were also normalised to s-process model predictions for the envelope compositions of low-mass (1.5 to 3 fx1) AGB stars with close-to-solar metallicities (Z=0.014 and 0.02). The overall trace element abundances (excluding Eu and Yb) appear consistent with the predicted s-process patterns. The depletions of Eu and Yb suggest that these elements remained in the gas phase during the condensation of SiC. The lack of depletion in some other moderately refractory elements (like Ba), and the presence of volatile elements (e.g. Xe) indicates that these elements were incorporated in to SiC by other mechanisms, most likely ion implantation.