摘要

The mass uptake of ambient oxygen in nanoporous ice is enhanced by irradiation with 193 nm photons, due to conversion of O-2 into H2O2 and O-3, with an efficiency that increases with decreasing temperature. These findings show a new way to form H2O2 and O-3 on icy surfaces in the outer solar system at depths much larger than are accessible by typical ionizing radiation, with possible astrobiological implications.

  • 出版日期2011-9-1