Atmospheric Chemistry Lab Work
This practical course offers the opportunity to get to know lab work on a topic of atmospheric importance.
Content
Cirrus clouds play an important role in the radiative budget of the Earth. Due to scattering and absorption of the solar as well as terrestrial radiation the cirrus cloud cover may influence significantly the Earth climate. How the cirrus clouds exactly form, is still unknown. Ice particles in cirrus clouds may form by homogeneous ice nucleation from liquid aerosols or via heterogeneous ice nucleation on solid ice nuclei (IN). The dihydrate of oxalic acid (OAD) acts as a heterogeneous ice nucleus, with an increase in freezing temperature between 2 and 5K depending on solution composition. In several field campaigns, oxalic acid enriched particles have been detected in the upper troposphere with single particle aerosol mass spectrometry. Simulations with a microphysical box model indicate that the presence of OAD may reduce the ice particle number density in cirrus clouds by up to ~50% when compared to exclusively homogeneous cirrus formation without OAD.
The goal of this atmospheric chemistry lab work is to expand the knowledge about the influence of oxalic acid in different aqueous solution systems for the heterogeneous ice nucleation process. Experiments of emulsified aqueous solutions containing oxalic acid will be performed with a differential scanning calorimeter (DSC, TA Instruments Q10). Water-in-oil emulsions contain a high number of micrometer-sized water droplets. Each droplet freezes independently which allows the measurement of homogeneous freezing for droplets without heterogeneous IN and heterogeneous freezing in the presence of an IN. OAD is formed in-situ in a first freezing cycle and will act as an IN in a second freezing cycle. This experiment will be performed in the presence of different solutes. In general, the presence of a solute leads to a decrease of the freezing temperature. However, also more specific interactions with oxalic acid are possible so that e.g. the formation of OAD is inhibited.
In the atmospheric chemistry lab work experiments, emulsified aqueous oxalic acid solutions are prepared and investigated in the DSC during several freezing cycles. The onset of freezing is evaluated. Freezing onsets in the presence and absence of OAD are compared. This is done for pure oxalic acid solutions and oxalic acid solutions containing a second solute (e.g. another dicarboxylic acid). The quality of the emulsions is checked in an optical microscope.
The practical course is divided into three parts
- Self-dependent reading of recommended literature (2 days).
- Laboratory work on ice nucleation using a Differential Scanning Calorimeter (CHN D59, 2 days). The work will be performed in groups of 2-3 students. The dates will be scheduled on the first meeting. The literature reading has to be done before the laboratory work can be started.
- All groups together write one report, which includes the results of all individual groups. The results will further be presented in a short talk (15-20 min). The date for the talk will be scheduled on the first meeting. The report has to be handed in on the same day as the talk is given.
- B. Zobrist, C. Marcolli, T. Koop, B. P. Luo, D. M. Murphy, U. Lohmann, A. A. Zardini, U. K. Krieger, T. Corti, D. J. Cziczo, S. Fueglistaler, P. K. Hudson, D. S. Thomson, and T. Peter; Oxalic acid as a heterogeneous ice nucleus in the upper troposphere and its indirect aerosol effect, Atmos. Chem. Phys., 6, 3115–3129, 2006. Download pdf of the article (PDF, 1.9 MB)
- B. Zobrist; Untersuchungen zum Gefrierverhalten von wässrigen Polyethylenglykol-Lösungen mit einem selbstentwickelten Kalorimeter; Diplomarbeit, ETH Zürich, 2001. Pages 5-7 and 9-11, pdf of the article
- Koop, T.; Luo, B.P.; Tsias, A. and T. Peter; Water activity as the determinant for homogeneous ice nucleation in aqueous solutions, Nature, 406, 611-614, 2000. external page article online
- Murphy, D.M and T. Koop, T; Review of the vapour pressures of ice and supercooled water for atmospheric applications, Q. J. R. Meteorol. Soc., 131, 1539-1565, 2005. Equations 7 and 10 to parameterize the vapor pressures of water and ice. external page article online
