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Formation of H2+ by ultra-low-energy collisions of protons with water ice surfaces
Published in
2011
Volume: 115
   
Issue: 28
Pages: 13813 - 13819
Abstract
The molecular ion of dihydrogen (H2+) is produced by 1 eV collisions of protons (H+) on amorphous water ice surfaces. The reaction is also observed on crystalline ice surfaces, but with lower efficiency. Collisions of D+ on amorphous H2O and D 2O ices yield D2+ on the former, subsequent to isotope exchange on the H2O surface. Ultra-low-energy collision-induced dihydrogen ion production is also observed from alkanol surfaces, with decreasing efficiency as the alkyl chain length increases. There is no corresponding reaction on solid hexane. This endothermic reaction, with implications for interstellar chemistry and plasma etching processes, is proposed to occur as a result of stabilization of the other reaction product, a hydroxyl radical (OH•), on water surfaces through hydrogen-bonding interactions with the surface. These results point to an interesting chemistry involving ultra-low-energy ions on molecular solids. © 2011 American Chemical Society.
About the journal
JournalJournal of Physical Chemistry C
ISSN19327447
Open AccessNo
Concepts (25)
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    ALKANOLS
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    Alkyl chain lengths
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    AMORPHOUS WATER
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    CRYSTALLINE ICE
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    Dihydrogen
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    ENDOTHERMIC REACTIONS
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    Hydrogen bonding interactions
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    HYDROXYL RADICALS
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    INTERSTELLAR CHEMISTRY
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    ION PRODUCTION
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    ISOTOPE EXCHANGE
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    Molecular ions
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    MOLECULAR SOLID
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    PLASMA ETCHING PROCESS
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    WATER ICE SURFACES
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    WATER SURFACE
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    Energy efficiency
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    Hexane
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    Hydrogen bonds
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    Ice
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    Ions
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    Isotopes
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    Plasma etching
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    Protons
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    Surface reactions