Chemistry of Atmospheres

By Michael E. Chang. 2003

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The global nitrogen cycle in the twenty-first century (2013, background): “The compounds generated are mainly NO and NO2, which arise from oxidation of atmospheric N2, and there is an additional contribution from nitrogen compounds in the fuel, derived from sequestration at the time the organic deposits were laid down [3].”
ABIOTIC OXYGEN-DOMINATED ATMOSPHERES ON TERRESTRIAL HABITABLE ZONE PLANETS (2014, background): “…interior by abiotic processes (Levi et al. 2013; Guzmán-Marmolejo et al. 2013), could have lifetimes similar to those on Earth today in an O2-rich atmosphere, although variations in O3 and NOx concentrations as a function of UV levels and atmospheric composition might alter this (Wayne 2000).”
Quantum dynamics of complex-forming bimolecular reactions (2012, background): “It plays an important role in atmospheric chemistry as a major mechanism for the production of the OH radical [167], and in combustion chemistry as a chain branching step [168].”