In this work, broad-band
soft X-ray (6–2000 eV) was employed
to irradiate frozen acetonitrile CH3CN, at the temperature
13 K, with different photon fluences up to 1.5 × 1018 photons cm–2. Here, acetonitrile is considered
as a representative complex organic molecule (COM) present in astrophysical
water-rich ices. The experiments were conduced at the Brazilian synchrotron
facility (LNLS/CNPEM) employing infrared spectroscopy (FTIR) to monitor
chemical changes induced by radiation. The effective destruction cross
section of acetonitrile and effective formation cross section for
daughter species formed inside the ice were obtained. The identified
radiation products were HCN, CH4, H2CCNH, and
CH3NC showing that fragmentation and rearrangement contribute
to acetonitrile destruction. Chemical equilibrium and molecular abundances
at this stage were determined, which also includes the abundance estimates
of unknown molecules, produced but not directly detected, in the ice.
The chemical equilibrium was reached at fluence around 1.5 ×
1018 photons cm–2. Time scales for ices,
at hypothetical snow line distances, to reach chemical equilibrium
around compact objects, young stellar objects, and O/B stars and inside
solar system were given. Among the obtained results are the time scales
for reaching chemical equilibrium around different astronomical strong
X-ray emitters, e.g., 14 days (for the Sun at 5 AU), 41 and 82 days
(for O/B stars at 5 AU), 109–1011 years
(for white dwarfs at 1 LY), 450 years (for Crab pulsar at 2.25 LY),
around 107 years (for Vela pulsar at 2.25 LY), and 7.5
× 106 years (for Sagittarius A* at 3 LY).