Barium Isotopic Composition of Mainstream Silicon Carbides from Murchison: Constraints for s-process Nucleosynthesis in Asymptotic Giant Branch Stars

Nan Liu1 et al. (>10)*
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1Department of the Geophysical Sciences, The University of Chicago, Chicago, IL 60637, USA

We present barium, carbon, and silicon isotopic compositions of 38 acid-cleaned presolar SiC grains from Murchison. Comparison with previous data shows that acid washing is highly effective in removing barium contamination. Strong depletions in δ(138Ba/136Ba) values are found, down to –400‰, which can only be modeled with a flatter 13C profile within the 13C pocket than is normally used. The dependence of δ(138Ba/136Ba) predictions on the distribution of 13C within the pocket in asymptotic giant branch (AGB) models allows us to probe the 13C profile within the 13C pocket and the pocket mass in AGB stars. In addition, we provide constraints on the 22Ne (αn) 25Mg rate in the stellar temperature regime relevant to AGB stars, based on δ(134Ba/136Ba) values of mainstream grains. We found two nominally mainstream grains with strongly negative δ(134Ba/136Ba) values that cannot be explained by any of the current AGB model calculations. Instead, such negative values are consistent with the intermediate neutron capture process (i process), which is activated by the very late thermal pulse during the post-AGB phase and characterized by a neutron density much higher than the s process. These two grains may have condensed around post-AGB stars. Finally, we report abundances of two p-process isotopes, 130Ba and 132Ba, in single SiC grains. These isotopes are destroyed in the s process in AGB stars. By comparing their abundances with respect to that of 135Ba, we conclude that there is no measurable decay of 135Cs (t 1/2 = 2.3 Ma) to 135Ba in individual SiC grains, indicating condensation of barium, but not cesium into SiC grains before 135Cs decayed.

Reference
Liu et al. (2014) Barium Isotopic Composition of Mainstream Silicon Carbides from Murchison: Constraints for s-process Nucleosynthesis in Asymptotic Giant Branch Stars. The Astrophysical Journal 786:66.
[doi:10.1088/0004-637X/786/1/48]

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The Evolving Activity of the Dynamically Young Comet C/2009 P1 (Garradd)

D. Bodewits1, T. L. Farnham1, M. F. A’Hearn1, L. M. Feaga1, A. McKay2,3, D. G. Schleicher4 and J. M. Sunshine1

1Department of Astronomy, University of Maryland, College Park, MD 20742-2421, USA
2Astronomy Department, New Mexico State University, Las Cruces, NM 88003, USA
3University of Texas Austin/McDonald Observatory, 1 University Station, Austin, TX 78712, USA
4Lowell Observatory, 1400 West Mars Hill Road, Flagstaff, AZ 86001, USA

We used the Ultraviolet-Optical Telescope on board Swift to observe the dynamically young comet C/2009 P1 (Garradd) from a heliocentric distance of 3.5 AU pre-perihelion until 4.0 AU outbound. At 3.5 AU pre-perihelion, comet Garradd had one of the highest dust-to-gas ratios ever observed, matched only by comet Hale-Bopp. The evolving morphology of the dust in its coma suggests an outburst that ended around 2.2 AU pre-perihelion. Comparing slit-based measurements and observations acquired with larger fields of view indicated that between 3 AU and 2 AU pre-perihelion a significant extended source started producing water in the coma. We demonstrate that this source, which could be due to icy grains, disappeared quickly around perihelion. Water production by the nucleus may be attributed to a constantly active source of at least 75 km2, estimated to be >20% of the surface. Based on our measurements, the comet lost 4 × 1011 kg of ice and dust during this apparition, corresponding to at most a few meters of its surface. Even though this was likely not the comet’s first passage through the inner solar system, the activity of Garradd was complex and changed significantly during the time it was observed.

Reference
Bodewits D, Farnham TL, A’Hearn MF, Feaga LM, McKay A, Schleicher DG and Sunshine JM (2014) The Evolving Activity of the Dynamically Young Comet C/2009 P1 (Garradd). The Astrophysical Journal 786:48.
[doi:10.1088/0004-637X/786/1/48]

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