Abstract

Abstract. Glyoxal (CHOCHO) and methylglyoxal (CH3C(O)CHO) are well-known components of atmospheric particles and their properties can impact atmospheric chemistry and cloud formation. To get information on their hydration states in aqueous solutions and how they are affected by the addition of inorganic salts (sodium chloride (NaCl) and sodium sulfate (Na2SO4)), we applied carbon and oxygen K-edge X-ray absorption spectroscopy (XAS) in transmission mode. The recorded C K-edge spectra show that glyoxal is completely hydrated in the dilute aqueous solutions, in line with previous studies. For methylglyoxal, supported by quantum chemical calculations we identified not only C–H, C=O and C–OH bonds, but also fingerprints of C–OH(CH2) and C=C bonds. The relatively low intensity of C=O transitions implies that the monohydrated form of methylglyoxal is not favored in the solutions. Instead, the spectral intensity is stronger in regions where products of aldol condensation and enol tautomers of the monohydrates contribute. The addition of salts was found to introduce only very minor changes to absorption energies and relative intensities of the observed absorption features, indicating that XAS in the near-edge region is not very sensitive to these intermolecular organic–inorganic interactions at the studied concentrations. The identified structures of glyoxal and methylglyoxal in an aqueous environment support the uptake of these compounds to the aerosol phase in the presence of water and their contribution to secondary organic aerosol formation.

Highlights

  • Aerosol particles in the atmosphere have several important effects on atmospheric chemistry and climate

  • We present oxygen K-edge spectra of aqueous solutions with glycerol and their ternary solutions containing inorganic salts

  • We recorded absorption spectra for the carbon and oxygen K edges and we measured as a reference the oxygen Kedge spectrum of aqueous glycerol

Read more

Summary

Introduction

Aerosol particles in the atmosphere have several important effects on atmospheric chemistry and climate They interact with solar radiation and participate in cloud formation. Previous work has revealed a large potential impact of interactions between organic and inorganic compounds on their gas–particle partitioning and water uptake properties (Kurtén et al, 2014; Hansen et al, 2015). Such interactions, including salting in and out effects, i.e., non-ideal solute–solute interactions in solution phase, are currently poorly described on the molecular level and have been characterized theoretically or experimentally only for a limited number of atmospherically relevant systems. Salting in and out effects refer here to the increase or decrease in the solubility of the organic solute (glyoxal and methylglyoxal) in water due to the presence of a co-solute, in this case an inorganic salt (NaCl, Na2SO4), in the solution

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call