Japan Geoscience Union Meeting 2021

Presentation information

[J] Poster

P (Space and Planetary Sciences ) » P-CG Complex & General

[P-CG19] Origin and evolution of materials in space

Fri. Jun 4, 2021 5:15 PM - 6:30 PM Ch.06

convener:Aki Takigawa(Department of Earth and Planetary Science, The University of Tokyo), Hitoshi Miura(Graduate School of Science, Department of Information and Basic Science, Nagoya City University), Takafumi Ootsubo(National Astronomical Observatory of Japan, National Institutes of Natural Sciences), Hideko Nomura(Division of Science, National Astronomical Observatory of Japan)

5:15 PM - 6:30 PM

[PCG19-P04] Modeling of Nitrogen Fractionation in the Protoplanetary Disk around TW Hya

*Seokho Lee1, Hideko Nomura1, Kenji Furuya1, Jeong-Eun Lee2 (1.National Astronomical Observatory of Japan, 2.Kyung Hee University)

Keywords:Astrochemistry, Numerical, protoplanetary disk, isotope, TW Hya

Observations conducted using the Atacama Large Millimeter/submillimeter Array on the protoplanetary disk around TW Hya show the nitrogen fractionation of HCN molecules in HC14N/HC15N ∼120 at a radius of ∼20 AU. In this study, we investigated the physical and chemical conditions that control this nitrogen fractionation process. To this end, a new disk model was developed, in which the isotope-selective photodissociation of molecular nitrogen and isotope-exchange chemical reactions have been incorporated. Our model can successfully reproduce the observed HCN column density when the elemental abundances of the gas-phase carbon and oxygen are depleted by two orders of magnitude relative to those in the interstellar medium and carbon is more abundant than oxygen ([C/O]elem> 1). The isotope-selective photodissociation of molecular nitrogen is the dominant nitrogen fractionation process in our models. The observed HC14N/HC15N ratio, which increases outwards, can also be reproduced by the model by assuming that the small dust grains in the atmosphere of the outer disk are depleted more than those in the inner disk. This is consistent with grain evolution models, according to which small dust grains are continuously replenished in the inner disk due to fragmentation of the large dust grains that radially drift from the outer disk.