期刊
PLANETARY SCIENCE JOURNAL
卷 3, 期 7, 页码 -出版社
IOP Publishing Ltd
DOI: 10.3847/PSJ/ac75b5
关键词
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资金
- National Science Foundation Graduate Research Fellowship Program [DGE-1746045]
- Australian Research Council through its Future Fellowships scheme [FT180100375]
- Research Corporation for Science Advancement through a Cottrell Scholar Award
- NASA through NASA Hubble Fellowship grant - Space Telescope Science Institute [HST-HF2-51485.001-A]
- NASA through Rosetta Data Analysis Program (RDAP) grant [80NSSC19K1306]
Based on the discoveries of interstellar objects like 'Oumuamua and Borisov, the Rubin Observatory Legacy Survey is expected to detect at least one interstellar object annually. Future measurements of H2O, CO2, and CO production rates in these objects will help estimate their carbon-to-oxygen ratios. Studies on solar system comets suggest they formed interior to the CO snow line, while the preferential desorption of CO and CO2 relative to H2O in the interstellar medium indicates that measured C/O ratios represent lower limits on the primordial ratios.
Based on the occurrence rates implied by the discoveries of 1I/'Oumuamua and 2I/Borisov, the forthcoming Rubin Observatory Legacy Survey of Space and Time (LSST) should detect >= one interstellar object every year. We advocate for future measurements of the production rates of H2O, CO2, and CO in these objects to estimate their carbon-to-oxygen ratios, which trace formation locations within their original protoplanetary disks. We review similar measurements for solar system comets, which indicate formation interior to the CO snow line. By quantifying the relative processing in the interstellar medium and solar system, we estimate that production rates will not be representative of primordial compositions for the majority of interstellar comets. Preferential desorption of CO and CO2 relative to H2O in the interstellar medium implies that measured C/O ratios represent lower limits on the primordial ratios. Specifically, production rate ratios of Q(CO)/Q(H2O) < 0.2 and Q(CO)/Q(H2O) > 1 likely indicate formation interior and exterior to the CO snow line, respectively. The high C/O ratio of 2I/Borisov implies that it formed exterior to the CO snow line. We provide an overview of the currently operational facilities capable of obtaining these measurements that will constrain the fraction of ejected comets that formed exterior to the CO snow line. This fraction will provide key insights into the efficiency of and mechanisms for cometary ejection in exoplanetary systems.
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