Oxidation mechanism of ammonia in water clusters

Abstract

Oxidation of ammonia is an important atmospheric process, but detailed mechanisms are for the most part yet unknown. Here the later steps in a mechanism forming nitric oxide and water from NH₂ and O₂ are studied. The transition states for isomerisation of NH₂OO to HNOOH and for dissociation of HNOOH to HNO and OH are identified and the subsequent formation of nitric oxide and water is discussed. This process is studied in small water clusters to model the effect of the nearest neighbouring water molecules in larger clusters or at extended surfaces, demonstrating the effect of solvation in lowering the barrier height for NH₂OO to HNOOH isomerisation. Proton transfer through the surrounding water provides a feasible reaction path in this system. As a result, it is shown that the high barrier for isomerisation between intermediates in the gas phase is not likely to prevent ammonia oxidation in small water clusters or aerosols.

GRAPHICAL ABSTRACT

KEYWORDS:

• Ammonia oxidation
• amidogen radical
• solvation

Acknowledgement

MEV and RBG gratefully appreciate insights learned from John F.Stanton on open-shell interactions.

Disclosure statement

No potential conflict of interest was reported by the author(s).

Additional information

Funding

YA acknowledges support from the National Science Foundation (DUE-1643737). RBG was supported by the Israel Science Foundation (593/20). YA and mev acknowledge computational resources from Iona College, and additional resources provided by the MERCURY consortium (http://mercuryconsortium.org/) through the NSF (CHE-1662030 and CHE-2018427).