TY - JOUR
T1 - Translational and rotational energy measurements of desorbed water molecules in their vibrational ground state following 157 nm irradiation of amorphous solid water
AU - Hama, Tetsuya
AU - Yokoyama, Masaaki
AU - Yabushita, Akihiro
AU - Kawasaki, Masahiro
AU - Watanabe, Naoki
N1 - Funding Information:
This work is supported by a grant-in-aid from JSPS ( 20245005 ).
PY - 2011/5/1
Y1 - 2011/5/1
N2 - Water ice is the major solid component in a variety of astrophysical environments, e.g., cold and dense molecular clouds. Photodesorption plays a dominant role in consuming ice in such cold regions. In this study, photodesorption of vibrationally ground-state H2O(v = 0) from amorphous solid water has been investigated at 157 nm. Using a resonance-enhanced multiphoton ionization technique, the translational and rotational energy distributions of photodesorbed H2O(v = 0) were measured, i.e., Boltzmann distributions at 1800 and 300 K, respectively. These energies are in good accordance with those predicted by classical molecular calculations for water photodesorption due to a kick-out mechanism following absorption of a single photon; hot H atom released by photodissociation of H2O in ice transfers enough momentum to another H2O molecule to kick it off the surface. Desorption of D2O(v = 0) following 193 nm photoirradiation of a D2O/H2S mixed ice was investigated to provide further direct evidence for the operation of a kick-out mechanism. The other desorption mechanisms were also discussed in the context of possible photodesorption of vibrationally excited H2O.
AB - Water ice is the major solid component in a variety of astrophysical environments, e.g., cold and dense molecular clouds. Photodesorption plays a dominant role in consuming ice in such cold regions. In this study, photodesorption of vibrationally ground-state H2O(v = 0) from amorphous solid water has been investigated at 157 nm. Using a resonance-enhanced multiphoton ionization technique, the translational and rotational energy distributions of photodesorbed H2O(v = 0) were measured, i.e., Boltzmann distributions at 1800 and 300 K, respectively. These energies are in good accordance with those predicted by classical molecular calculations for water photodesorption due to a kick-out mechanism following absorption of a single photon; hot H atom released by photodissociation of H2O in ice transfers enough momentum to another H2O molecule to kick it off the surface. Desorption of D2O(v = 0) following 193 nm photoirradiation of a D2O/H2S mixed ice was investigated to provide further direct evidence for the operation of a kick-out mechanism. The other desorption mechanisms were also discussed in the context of possible photodesorption of vibrationally excited H2O.
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U2 - 10.1016/j.nimb.2010.12.031
DO - 10.1016/j.nimb.2010.12.031
M3 - Article
AN - SCOPUS:79953745647
SN - 0168-583X
VL - 269
SP - 1011
EP - 1015
JO - Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms
JF - Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms
IS - 9
ER -