Hydrogen burning of $^{29}$Si and its impact on presolar stardust grains from classical novae
Lori Downen, Christian Iliadis, Art Champagne, Thomas Clegg, Alain, Coc, Jordi Jose

TL;DR
This study provides new experimental data on the $^{29}$Si(p,$$)$^{30}$P reaction, significantly refining the predicted silicon isotopic signatures in classical novae, which helps identify presolar grains of nova origin.
Contribution
The paper presents the first direct measurement of the $^{29}$Si(p,$$)$^{30}$P reaction rate, reducing uncertainties and improving models of silicon isotopic ratios in nova-formed presolar grains.
Findings
New $^{29}$Si(p,$$)$^{30}$P reaction rate differs by up to 50% from previous results.
Uncertainty in $$Si predictions reduced by up to a factor of 3.
$$Si isotopic ratios in presolar grains can be used to identify nova origins.
Abstract
Presolar stardust grains found in primitive meteorites are believed to retain the isotopic composition of stellar outflows at the time of grain condensation. Therefore, laboratory measurements of their isotopic ratios represent sensitive probes for investigating open questions related to stellar evolution, stellar explosions, nucleosynthesis, mixing mechanisms, dust formation, and galactic chemical evolution. For a few selected presolar grains, classical novae have been discussed as a potential source. For SiC, silicate, and graphite presolar grains, the association is based on the observation of small C)/C) and N)/N) number abundance ratios compared to solar values, and abundance excesses in Si relative to Si, as previously predicted by models of classical novae. We report on a direct measurement of the Si(p,)P…
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