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Impacts of chemical reactivity on ice nucleation of kaolinite particles: A case study of levoglucosan and sulfuric acid
Author(s) -
Tobo Yutaka,
DeMott Paul J.,
Raddatz Michael,
Niedermeier Dennis,
Hartmann Susan,
Kreidenweis Sonia M.,
Stratmann Frank,
Wex Heike
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2012gl053007
Subject(s) - kaolinite , ice nucleus , levoglucosan , nucleation , sulfuric acid , saturation (graph theory) , chemical engineering , mineral , mineralogy , materials science , aerosol , chemistry , inorganic chemistry , organic chemistry , metallurgy , mathematics , combinatorics , biomass burning , engineering
Changes in the ice nucleation properties of mineral dust particles due to soluble coatings are still not well understood. Here we show that the reactivity with soluble materials deposited on the surfaces of kaolinite particles is an important factor affecting the ice nucleation properties of the particles. Using kaolinite particles treated with levoglucosan or H 2 SO 4 (i.e., non‐reactive and reactive materials, respectively), we investigated the fraction of particles capable of nucleating ice at temperatures ranging from −34°C to −26°C. Below water saturation, both the levoglucosan and H 2 SO 4 coatings similarly reduced the ice nucleating ability of kaolinite particles. Above water saturation, however, only the H 2 SO 4 coatings reduced the ice nucleating ability of the particles, particularly at warmer temperatures. We suggest that the absence or presence of surface chemical reactions plays an important role in determining the number concentrations of ice crystals formed from mineral dust ice nuclei under mixed‐phase cloud conditions.