A New Determination of the Binding Energy of Atomic Oxygen on Dust Grain Surfaces: Experimental Results and Simulations
Jiao He, Jianming Shi, Tyler Hopkins, Gianfranco Vidali, Michael J., Kaufman

TL;DR
This study provides the first direct measurements of atomic oxygen desorption energy from dust grain analogs, revealing values about twice those previously assumed, which significantly impacts models of interstellar chemistry.
Contribution
It introduces the first experimental determination of O desorption energy from dust analogs and explores its effects on molecular cloud chemistry.
Findings
Desorption energies are approximately 1660 K for water ice and 1850 K for silicate surfaces.
Higher binding energies lead to increased water formation on grains at lower extinction levels.
The new values alter predictions of molecular abundances like H2O and O2 in interstellar clouds.
Abstract
The energy to desorb atomic oxygen from an interstellar dust grain surface, , is an important controlling parameter in gas-grain models; its value impacts the temperature range over which oxygen resides on a dust grain. However, no prior measurement has been done of the desorption energy. We report the first direct measurement of for atomic oxygen from dust grain analogs. The values of are ~K and ~K for porous amorphous water ice and for a bare amorphous silicate film, respectively, or about twice the value previously adopted in simulations of the chemical evolution of a cloud. We use the new values to study oxygen chemistry as a function of depth in a molecular cloud. For cm and =10 (=1 is the average local interstellar radiation field), the main result of the adoption of the higher oxygen…
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