Water ice deuteration: a tracer of the chemical history of protostars
Vianney Taquet, Phillip Peters, Claudine Kahane, Cecilia, Ceccarelli, Ana L\`opez-Sepulcre, C\'eline Toubin, Denis Duflot and, Laurent Wiesenfeld

TL;DR
This study uses a detailed astrochemical model to explore how water deuteration in protostars depends on physical conditions, revealing its potential as a tracer of the chemical history of star-forming regions.
Contribution
We developed a multilayer astrochemical model including ortho-para states and surface reactions to analyze water deuteration, providing new insights into its dependence on environmental parameters.
Findings
Water deuteration is highly sensitive to H2 ortho-to-para ratio and density.
Deuteration levels suggest water forms in less dense, early-stage molecular clouds.
Comparison with observations indicates water and CO2 form together in specific conditions.
Abstract
Context. Millimetric observations have measured high degrees of molecular deuteration in several species seen around low-mass protostars. The Herschel Space Telescope, launched in 2009, is now providing new measures of the deuterium fractionation of water, the main constituent of interstellar ices. Aims. We aim at theoretically studying the formation and the deuteration of water, which is believed to be formed on interstellar grain surfaces in molecular clouds. Methods. We used our gas-grain astrochemical model GRAINOBLE, which considers the multilayer formation of interstellar ices. We varied several input parameters to study their impact on water deuteration. We included the treatment of ortho- and para-states of key species, including H2, which affects the deuterium fractionation of all molecules. The model also includes relevant laboratory and theoretical works on the water…
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