4:45 PM - 5:00 PM
[MIS12-11] Nucleation experiments of titanium and/or carbon from a vapor in gravity and microgravity conditions
Keywords:nucleation, dust, microgravity
To understand formation condition of core-mantle grains, we performed replicate experiments in both gravity and microgravity environments and determined two physical quantities of sticking probability and surface tension, which are crucial in a grain formation model using a nucleation theory. Since the physical quantities depend on temperature, grain size and so on, experimental determination in a similar environment, where grans form, is necessary. Especially, the ratio of collision frequency to cooling timescale is similar between grain formation in gas outflow from an evolved star and microgravity experiment. Therefore, we conducted a microgravity experiment using a MASER 14 sounding rocket and compared the results with that of gravity experiments.
Starting material was evaporated in a buffer argon gas and determined the temperature and concentration during gas cooling by in-situ imaging of a double-wavelength, Mach-Zehnder type laser interferometer. Produced particles were observed using transmission electron microscopes. Based on the nucleation conditions including timescale for gas cools and size of the produced particles, sticking probability and surface tension of nucleated particles are determined using the modified classical nucleation theory (MCNT).
Both of determined physical quantities of sticking probabilities (<0.5) and surface tensions (tend to larger than bulk values) of titan, carbon and titanium carbide suggest inefficient formation of presolar grains. We will discuss how presolar grains can be formed and grown based on the results of the further experiments and theoretical modeling.
Acknowledgements
Developments of the experimental system was supported by the Technical Division of Institute of Low Temperature Science, Hokkaido University, and the Advanced Machining Technology Group of JAXA. Onboard data saving was supported by Dr. S. Takeuchi of ISAS/JAXA. This work was supported by FY2016 ISAS Small-Scale Science Projects of JAXA and Grant-in-Aids for Scientific Research (S) from KAKENHI (15H05731 and 20H05657).