Abstract

Abstract. Experiments on the title compounds have been performed using a multidiagnostic stirred-flow reactor (SFR) in which the gas phase as well as the condensed phase has been simultaneously investigated under stratospheric temperatures in the range 175–200 K. Wall interactions of the title compounds have been taken into account using Langmuir adsorption isotherms in order to close the mass balance between deposited and desorbed (recovered) compounds. Thin solid films at 1 µm typical thickness have been used as a proxy for atmospheric ice particles and have been deposited on a Si window of the cryostat, with the optical element being the only cold point in the deposition chamber. Fourier transform infrared (FTIR) absorption spectroscopy in transmission as well as partial and total pressure measurement using residual gas mass spectrometry (MS) and sensitive pressure gauges have been employed in order to monitor growth and evaporation processes as a function of temperature using both pulsed and continuous gas admission and monitoring under SFR conditions. Thin solid H2O ice films were used as the starting point throughout, with the initial spontaneous formation of α-NAT (nitric acid trihydrate) followed by the gradual transformation of α- to β-NAT at T > 185 K. Nitric acid dihydrate (NAD) was spontaneously formed at somewhat larger partial pressures of HNO3 deposited on pure H2O ice. In contrast to published reports, the formation of α-NAT proceeded without prior formation of an amorphous HNO3 ∕ H2O layer and always resulted in β-NAT. For α- and β-NAT, the temperature-dependent accommodation coefficient α(H2O) and α(HNO3), the evaporation flux Jev(H2O) and Jev(HNO3) and the resulting saturation vapor pressure Peq(H2O) and Peq(HNO3) were measured and compared to binary phase diagrams of HNO3 ∕ H2O in order to afford a thermochemical check of the kinetic parameters. The resulting kinetic and thermodynamic parameters of activation energies for evaporation (Eev) and standard heats of evaporation ΔHev0 of H2O and HNO3 for α- and β-NAT, respectively, led to an estimate for the relative standard enthalpy difference between α- and β-NAT of −6.0 ± 20 kJ mol−1 in favor of β-NAT, as expected, despite a significantly larger value of Eev for HNO3 in α-NAT. This in turn implies a substantial activation energy for HNO3 accommodation in α- compared to β-NAT where Eacc(HNO3) is essentially zero. The kinetic (α(HCl), Jev(HCl)) and thermodynamic (Peq(HCl)) parameters of HCl-doped α- and β-NAT have been determined under the assumption that HCl adsorption did not significantly affect α(H2O) and α(HNO3) as well as the evaporation flux Jev(H2O). Jev(HCl) and Peq(HCl) on both α- and β-NAT are larger than the corresponding values for HNO3 across the investigated temperature range but significantly smaller than the values for pure H2O ice at T < 200 K.

Highlights

  • Heterogeneous processes taking place on ice clouds in the upper troposphere (UT) or on polar stratospheric clouds (PSCs) in the lower stratosphere (LS) have, for a long time, been recognized as one of the major ozone-depleting mechanisms (Solomon et al, 1986)

  • We refrain at this point from showing raw data (FTIR absorption spectra and mass spectrometry (MS) data as a function of time) because representative samples have been shown by Iannarelli and Rossi (2015) for α- and β-nitric acid trihydrate (NAT)

  • As in the case of α-NAT, this result is very different compared to the case of HCl hydrates studied before using the same apparatus (Iannarelli and Rossi, 2013) where the evaporation of H2O is not influenced by the presence of adsorbed HCl on the ice and takes place at a rate characteristic of pure ice for all HCl concentrations used

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Summary

Introduction

Heterogeneous processes taking place on ice clouds in the upper troposphere (UT) or on polar stratospheric clouds (PSCs) in the lower stratosphere (LS) have, for a long time, been recognized as one of the major ozone-depleting mechanisms (Solomon et al, 1986). PSCs consist of either particles of crystalline nitric acid trihydrate (NAT) (type Ia), ternary H2SO4 / HNO3 / H2O supercooled solutions (type Ib) or pure H2O ice (type II) (Zondlo et al, 2000), and are Published by Copernicus Publications on behalf of the European Geosciences Union. J. Rossi: Trace gases on α- and β-NAT formed during the polar winter season when temperatures are sufficiently low in order to allow H2O supersaturation that leads to cloud formation in the dry stratosphere subsequent to ice nucleation (Peter, 1997)

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