Efficiency of immersion mode ice nucleation on surrogates of mineral dust
Open Access
- 4 October 2007
- journal article
- Published by Copernicus GmbH in Atmospheric Chemistry and Physics
- Vol. 7 (19), 5081-5091
- https://doi.org/10.5194/acp-7-5081-2007
Abstract
A differential scanning calorimeter (DSC) was used to explore heterogeneous ice nucleation of emulsified aqueous suspensions of two Arizona test dust (ATD) samples with particle diameters of nominally 0–3 and 0–7 μm, respectively. Aqueous suspensions with ATD concentrations of 0.01–20 wt% have been investigated. The DSC thermograms exhibit a homogeneous and a heterogeneous freezing peak whose intensity ratios vary with the ATD concentration in the aqueous suspensions. Homogeneous freezing temperatures are in good agreement with recent measurements by other techniques. Depending on ATD concentration, heterogeneous ice nucleation occurred at temperatures as high as 256 K or down to the onset of homogeneous ice nucleation (237 K). For ATD-induced ice formation Classical Nucleation Theory (CNT) offers a suitable framework to parameterize nucleation rates as a function of temperature, experimentally determined ATD size, and emulsion droplet volume distributions. The latter two quantities serve to estimate the total heterogeneous surface area present in a droplet, whereas the suitability of an individual heterogeneous site to trigger nucleation is described by the compatibility function (or contact angle) in CNT. The intensity ratio of homogeneous to heterogeneous freezing peaks is in good agreement with the assumption that the ATD particles are randomly distributed amongst the emulsion droplets. The observed dependence of the heterogeneous freezing temperatures on ATD concentrations cannot be described by assuming a constant contact angle for all ATD particles, but requires the ice nucleation efficiency of ATD particles to be (log)normally distributed amongst the particles. Best quantitative agreement is reached when explicitly assuming that high-compatibility sites are rare and that therefore larger particles have on average more and better active sites than smaller ones. This analysis suggests that a particle has to have a diameter of at least 0.1 μm to exhibit on average one active site.Keywords
All Related Versions
This publication has 37 references indexed in Scilit:
- Morphology characterization of emulsions by differential scanning calorimetryAdvances in Colloid and Interface Science, 2005
- Ice nucleation by surrogates for atmospheric mineral dust and mineral dust/sulfate particles at cirrus temperaturesAtmospheric Chemistry and Physics, 2005
- T-dependent rate measurements of homogeneous ice nucleation in cloud droplets using a large atmospheric simulation chamberJournal of Photochemistry and Photobiology A: Chemistry, 2005
- Measurements of the concentration and composition of nuclei for cirrus formationProceedings of the National Academy of Sciences, 2003
- African dust aerosols as atmospheric ice nucleiGeophysical Research Letters, 2003
- Ice Formation in (NH4)2SO4−H2O ParticlesThe Journal of Physical Chemistry A, 1999
- Cloud Microphysics and ClimateScience, 1997
- Ice crystallization induced by silver iodide and bacteria in microsize droplets dispersed within emulsionsPublished by Walter de Gruyter GmbH ,1991
- Numerical Simulation of the Effects of Varying Ice Crystal Nucleation Rates and Aggregation Processes on Orographic SnowfallJournal of Climate and Applied Meteorology, 1986
- A study of the freezing of supercooled water dispersed within emulsions by differential scanning calorimetryJournal of Physics C: Solid State Physics, 1976