Chemistry in the First Hydrostatic Core Stage By Adopting Three-Dimensional Radiation Hydrodynamic Simulations
Kenji Furuya, Yuri Aikawa, Kengo Tomida, Tomoaki Matsumoto, Kazuya, Saigo, Kohji Tomisaka, Franck Hersant, and Valentine Wakelam

TL;DR
This study uses three-dimensional radiation hydrodynamic simulations to explore molecular evolution during the formation of the first hydrostatic core, revealing temperature-dependent chemical changes and potential tracers for early star formation stages.
Contribution
It introduces a detailed 3D simulation approach to track molecular evolution from molecular cloud cores to first hydrostatic cores, including chemical reactions and spatial distributions.
Findings
Molecular abundances remain stable until ~500 K.
Ice sublimation influences gas-phase chemistry in warm regions.
Large organic molecules are potential tracers of first cores.
Abstract
We investigate molecular evolution from a molecular cloud core to a first hydrostatic core in three spatial dimensions. We perform a radiation hydrodynamic simulation in order to trace fluid parcels, in which molecular evolution is investigated, using a gas-phase and grain-surface chemical reaction network. We derive spatial distributions of molecular abundances and column densities in the core harboring the first core. We find that the total of gas and ice abundances of many species in a cold era (10 K) remain unaltered until the temperature reaches ~500 K. The gas abundances in the warm envelope and the outer layer of the first core (T < 500 K) are mainly determined via the sublimation of ice-mantle species. Above 500 K, the abundant molecules, such as H2CO, start to be destroyed, and simple molecules, such as CO, H2O and N2 are reformed. On the other hand, some molecules are…
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