Vacuum ultraviolet photodesorption and photofragmentation of formaldehyde-containing ices
arXiv:1905.08223 · doi:10.1021/acsearthspacechem.9b00057
Abstract
Non-thermal desorption from icy grains containing HCO has been invoked to explain the observed HCO gas phase abundances in ProtoPlanetary Disks (PPDs) and Photon Dominated Regions (PDRs). Photodesorption is thought to play a key role, however no absolute measurement of the photodesorption from HCO ices were performed up to now, so that a default value is used in the current astrophysical models. As photodesorption yields differ from one molecule to the other, it is crucial to experimentally investigate photodesorption from HCO ices. We measured absolute wavelength-resolved photodesorption yields from pure HCO ices, HCO on top of a CO ice (HCO/CO), and HCO mixed with CO ice (HCO:CO) irradiated in the Vacuum UltraViolet (VUV) range (7-13.6~eV). Photodesorption from a pure HCO ice releases HCO in the gas phase, but also fragments, such as CO and H. Energy-resolved photodesorption spectra, coupled with InfraRed (IR) and Temperature Programmed Desorption (TPD) diagnostics, showed the important role played by photodissociation and allowed to discuss photodesorption mechanisms. For the release of HCO in the gas phase, they include Desorption Induced by Electronic Transitions (DIET), indirect DIET through CO-induced desorption of HCO and photochemical desorption. We found that HCO photodesorbs with an average efficiency of molecule/photon, in various astrophysical environments. HCO and CO photodesorption yields and photodesorption mechanisms, involving photofragmentation of HCO, can be implemented in astrochemical codes. The effects of photodesorption on gas/solid abundances of HCO and all linked species from CO to Complex Organic Molecules (COMs), and on the HCO snowline location, are now on the verge of being unravelled.
ACS Earth and Space Chemistry; Complex Organic Molecules (COMs) in Star-Forming Regions special issue
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