Uptake of Ammonia by Ice Surfaces at Atmospheric Temperatures
Abstract
We present an ambient pressure X-ray photoelectron spectroscopy investigation of the adsorption of ammonia on ice over the temperature range of −23 °C to −50 °C. Previous flow tube studies showed significant uptake of ammonia at these temperatures to ice, which was linked to the incorporation of ammonium into the ice crystal lattice. Our present investigation shows a significant uptake of ammonia to the ice interface, with ammonia concentrations that exceed those measured in past studies for the case of bulk snow ice and samples. We also have indication that some of the ammonia is protonated at the ice surface and thus adsorbed there as ammonium ions. The impact of high ammonia concentrations at the air-ice interface on the surface chemistry of ice clouds is discussed. The present study lays the groundwork for investigating the reaction of adsorbed ammonia with other trace gases in the atmosphere, which is demonstrated on the example of a proof-of-principle experiment of its interaction with acetic acid.
- This article is part of the themed collection: Atmospheric chemistry in cold environments