title: Water uptake of clay and desert dust aerosol particles at sub- and supersaturated water vapor conditions.
abstract: Airborne mineral dust particles serve as cloud condensation nuclei (CCN), thereby influencing the formation and properties of warm clouds. It is therefore of atmospheric interest how dust aerosols with different mineralogy behave when exposed to high relative humidity (RH) or supersaturation (SS) with respect to liquid water. In this study the subsaturated hygroscopic growth and the supersaturated cloud condensation nucleus activity of pure clays and real desert dust aerosols were determined using a hygroscopicity tandem differential mobility analyzer (HTDMA) and a cloud condensation nuclei counter (CCNC), respectively. Five different illite, montmorillonite and kaolinite clay samples as well as three desert dust samples (Saharan dust (SD), Chinese dust (CD) and Arizona test dust (ATD)) were investigated. Aerosols were generated both with a wet and a dry disperser. The water uptake was parameterized via the hygroscopicity parameter kappa. The hygroscopicity of dry generated dust aerosols was found to be negligible when compared to processed atmospheric aerosols, with CCNC derived kappa values between 0.00 and 0.02 (the latter corresponds to a particle consisting of 96.7% by volume insoluble material and approximately 3.3% ammonium sulfate). Pure clay aerosols were generally found to be less hygroscopic than natural desert dust particles. The illite and montmorillonite samples had kappa approximately 0.003. The kaolinite samples were less hygroscopic and had kappa=0.001. SD (kappa=0.023) was found to be the most hygroscopic dry-generated desert dust followed by CD (kappa=0.007) and ATD (kappa=0.003). Wet-generated dust showed an increased water uptake when compared to dry-generated samples. This is considered to be an artifact introduced by redistribution of soluble material between the particles. Thus, the generation method is critically important when presenting such data. These results indicate any atmospheric processing of a fresh mineral dust particle which leads to the addition of more than approximately 3% soluble material will significantly enhance its hygroscopicity and CCN activity.
authors.affiliation: Institute for Atmospheric and Climate Science, ETH Zurich, CH-8092, Zurich, Switzerland.
authors.forename: Hanna
authors.initials: H
authors.lastname: Herich
authors.forename: Torsten
authors.initials: T
authors.lastname: Tritscher
authors.forename: Aldona
authors.initials: A
authors.lastname: Wiacek
authors.forename: Martin
authors.initials: M
authors.lastname: Gysel
authors.forename: Ernest
authors.initials: E
authors.lastname: Weingartner
authors.forename: Ulrike
authors.initials: U
authors.lastname: Lohmann
authors.forename: Urs
authors.initials: U
authors.lastname: Baltensperger
authors.forename: Daniel J
authors.initials: DJ
authors.lastname: Cziczo
mesh_terms: D000042:Absorption; D000336:Aerosols / Q000737:chemistry*; D000538:Aluminum Silicates / Q000737:chemistry*; D001272:Atmosphere / Q000032:analysis* / Q000737:chemistry*; D000077215:Clay; D003198:Computer Simulation; D003889:Desert Climate; D004391:Dust / Q000032:analysis*; D005740:Gases / Q000737:chemistry; D010316:Particle Size; D052638:Particulate Matter / Q000737:chemistry*; D044367:Phase Transition; D014867:Water / Q000737:chemistry*
chemical_list: D000336:Aerosols; D000538:Aluminum Silicates; D004391:Dust; D005740:Gases; D052638:Particulate Matter; D014867:Water; D000077215:Clay