Table B.2
Direct cosmic-ray desorption reactions.
Reaction | α (1) | Eads | ||||
---|---|---|---|---|---|---|
CH4* | +CRP | → | CH4 | GRAIN | 7.000e+01 | 1.120e+03 |
O2* | +CRP | → | O2 | GRAIN | 7.000e+01 | 1.210e+03 |
H2O* | +CRP | → | H2O | GRAIN | 8.000E–01 | 8.550e+02 |
CO* | +CRP | → | CO | GRAIN | 7.000e+01 | 8.550e+02 |
CO2* | +CRP | → | CO2 | GRAIN | 7.000e+01 | 2.690e+03 |
N* | +CRP | → | N | GRAIN | 7.000e+01 | 8.000e+02 |
NH3* | +CRP | → | NH3 | GRAIN | 2.360e+00 | 8.550e+02 |
N2* | +CRP | → | N2 | GRAIN | 7.000e+01 | 7.900e+02 |
CH3OH* | +CRP | → | CH3OH | GRAIN | 7.000e+01 | 4.240e+03 |
H2CO* | +CRP | → | H2CO | GRAIN | 7.000e+01 | 1.760e+03 |
HCO2H* | +CRP | → | HCO2H | GRAIN | 7.000e+01 | 1.500e+03 |
OCS* | +CRP | → | OCS | GRAIN | 7.000e+01 | 3.000e+03 |
H2S* | +CRP | → | H2S | GRAIN | 7.000e+01 | 1.800e+03 |
Fe* | +CRP | → | Fe | GRAIN | 7.000e+01 | 2.400e+03 |
HDO* | +CRP | → | HDO | GRAIN | 8.000E–01 | 8.550e+02 |
D2O* | +CRP | → | D2O | GRAIN | 8.000E–01 | 8.550e+02 |
NH2D* | +CRP | → | NH2D | GRAIN | 2.360e+00 | 8.550e+02 |
NHD2* | +CRP | → | NHD2 | GRAIN | 2.360e+00 | 8.550e+02 |
ND3* | +CRP | → | ND3 | GRAIN | 2.360e+00 | 8.550e+02 |
Notes. The 15N substitutions, which are identical to the 14N reactions, are not shown here. CRP stands for cosmic-ray particle. Mantle species are denoted by an asterisk.
(1) The rate is computed as in Flower et al. (2005; see their Sect. 3.3) and Faure et al. (2019) (Eq. (7)), where the yield (noted
γ in Flower et al. 2005) is given by , and the binding energy is Eads. The binding energies of the 14N and
15N variants of adsorbed species have equal values. The same desorption reactions, but by secondary photons (photodesorption), are also taken into accountin UGAN.
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