Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors

Ice chemistry in the dense, cold interstellar medium (ISM) is probably responsible for the formation of interstellar complex organic molecules (COMs). Recent laboratory experiments performed at T ∼ 4 K have shown that irradiation of CO:N _2 ice samples analog to the CO-rich interstellar ice layer ca...

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Main Authors: Rafael Martín-Doménech, Alexander DelFranco, Karin I. Öberg, Mahesh Rajappan
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
Series:The Astrophysical Journal
Subjects:
Online Access:https://doi.org/10.3847/1538-4357/ad187e
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author Rafael Martín-Doménech
Alexander DelFranco
Karin I. Öberg
Mahesh Rajappan
author_facet Rafael Martín-Doménech
Alexander DelFranco
Karin I. Öberg
Mahesh Rajappan
author_sort Rafael Martín-Doménech
collection DOAJ
description Ice chemistry in the dense, cold interstellar medium (ISM) is probably responsible for the formation of interstellar complex organic molecules (COMs). Recent laboratory experiments performed at T ∼ 4 K have shown that irradiation of CO:N _2 ice samples analog to the CO-rich interstellar ice layer can contribute to the formation of COMs when H _2 molecules are present. We have tested this organic chemistry under a broader range of conditions relevant to the interior of dense clouds by irradiating CO: ^15 N _2 :H _2 ice samples with 2 keV electrons in the 4–15 K temperature range. The H _2 ice abundance depended on both, the ice formation temperature and the thermal evolution of the samples. Formation of H-bearing organics such as formaldehyde (H _2 CO), ketene (C _2 H _2 O), and isocyanic acid (H ^15 NCO) was observed upon irradiation of ice samples formed at temperatures up to 10 K, and also in ices formed at 6 K and subsequently warmed up and irradiated at temperatures up to 15 K. These results suggest that a fraction of the H _2 molecules in dense cloud interiors might be entrapped in the CO-rich layer of interstellar ice mantles, and that energetic processing of this layer could entail an additional contribution to the formation of COMs in the coldest regions of the ISM.
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spelling doaj.art-6cff480f9ce34b1d84f9c407b8d01e622024-02-12T11:49:32ZengIOP PublishingThe Astrophysical Journal1538-43572024-01-01962210710.3847/1538-4357/ad187eOrganic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud InteriorsRafael Martín-Doménech0https://orcid.org/0000-0001-6496-9791Alexander DelFranco1https://orcid.org/0000-0003-2322-7526Karin I. Öberg2https://orcid.org/0000-0001-8798-1347Mahesh Rajappan3https://orcid.org/0000-0003-2761-4312Centro de Astrobiología (CSIC-INTA) Carretera de Ajalvir , km. 4, Torrejón de Ardoz, E-28850, Madrid, Spain ; rmartin@cab.inta-csic.esCenter for Astrophysics ∣ Harvard & Smithsonian 60 Garden St., Cambridge, MA 02138, USA; Physics and Astronomy Department, Amherst College , 21 Merrill Science Drive, Amherst, MA 01002, USACenter for Astrophysics ∣ Harvard & Smithsonian 60 Garden St., Cambridge, MA 02138, USACenter for Astrophysics ∣ Harvard & Smithsonian 60 Garden St., Cambridge, MA 02138, USAIce chemistry in the dense, cold interstellar medium (ISM) is probably responsible for the formation of interstellar complex organic molecules (COMs). Recent laboratory experiments performed at T ∼ 4 K have shown that irradiation of CO:N _2 ice samples analog to the CO-rich interstellar ice layer can contribute to the formation of COMs when H _2 molecules are present. We have tested this organic chemistry under a broader range of conditions relevant to the interior of dense clouds by irradiating CO: ^15 N _2 :H _2 ice samples with 2 keV electrons in the 4–15 K temperature range. The H _2 ice abundance depended on both, the ice formation temperature and the thermal evolution of the samples. Formation of H-bearing organics such as formaldehyde (H _2 CO), ketene (C _2 H _2 O), and isocyanic acid (H ^15 NCO) was observed upon irradiation of ice samples formed at temperatures up to 10 K, and also in ices formed at 6 K and subsequently warmed up and irradiated at temperatures up to 15 K. These results suggest that a fraction of the H _2 molecules in dense cloud interiors might be entrapped in the CO-rich layer of interstellar ice mantles, and that energetic processing of this layer could entail an additional contribution to the formation of COMs in the coldest regions of the ISM.https://doi.org/10.3847/1538-4357/ad187eInterstellar mediumInterstellar cloudsInterstellar moleculesDense interstellar cloudsIce compositionComplex organic molecules
spellingShingle Rafael Martín-Doménech
Alexander DelFranco
Karin I. Öberg
Mahesh Rajappan
Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors
The Astrophysical Journal
Interstellar medium
Interstellar clouds
Interstellar molecules
Dense interstellar clouds
Ice composition
Complex organic molecules
title Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors
title_full Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors
title_fullStr Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors
title_full_unstemmed Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors
title_short Organic Chemistry in the H2-bearing, CO-rich Interstellar Ice Layer at Temperatures Relevant to Dense Cloud Interiors
title_sort organic chemistry in the h2 bearing co rich interstellar ice layer at temperatures relevant to dense cloud interiors
topic Interstellar medium
Interstellar clouds
Interstellar molecules
Dense interstellar clouds
Ice composition
Complex organic molecules
url https://doi.org/10.3847/1538-4357/ad187e
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