Quantifying the temperature-dependent yields of N and NH formation in vacuum-ultraviolet-irradiated NH ice
arXiv:2609.17878 · doi:10.1051/0004-6361/202658992
Abstract
Gas--grain astrochemical models predict that a substantial fraction of elemental nitrogen in dense cores and protoplanetary disks is locked in molecular nitrogen (N), in the gas or ice phase, although interstellar N ice has not been directly identified. Rosetta measurements at comet 67P/Churyumov--Gerasimenko showed strong N depletion relative to CO, while NH was the dominant detected nitrogen-bearing ice. We experimentally quantify the conversion of NH ice into N and NH under astronomically relevant conditions by studying its temperature- and fluence-dependent VUV photochemistry. Experiments were performed under ultra-high vacuum using 40-monolayer NH ice at 15, 25, and 70 K irradiated at 115--170 nm to a total fluence of photons cm. Laser desorption with post-ionization reflection time-of-flight mass spectrometry (ReTOF-MS) was used to monitor N and NH simultaneously. VUV photolysis efficiently forms both products, with formation kinetics and product ratios depending on temperature and photon fluence. Initial-growth fits gave the highest apparent ice-retained N formation yield at 15 K, approximately an order of magnitude above those at 25 and 70 K. The N/NH column-density ratio was determined as a function of fluence and compared with astronomical constraints. These results suggest that NH ice photochemistry may provide an additional pathway to N ice in cold outer planetary environments.
22 pages, 7 figures
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