0000000000563612

AUTHOR

Heiko Hofmann

showing 2 related works from this author

Ice nucleation properties of the most abundant mineral dust phases

2008

[1] The ice nucleation properties of the nine most abundant minerals occurring in desert aerosols (quartz, albite, microcline, kaolinite, montmorillonite, illite, calcite, gypsum, and hematite) were investigated by environmental scanning electron microscopy (ESEM). In this instrument, the pure minerals are exposed to water vapor at variable pressures and temperatures. The crystallization of ice on the mineral particles is observed by secondary electron imaging, and the supersaturation for an activated particle fraction of 1–3% is determined as function of temperature. In all experiments, condensation of water prior to ice formation was not observed within detectable limits, even at water su…

Atmospheric ScienceSoil ScienceMineralogyAquatic ScienceMineral dustengineering.materialOceanographychemistry.chemical_compoundAlbiteGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)KaoliniteRelative humidityEarth-Surface ProcessesWater Science and TechnologyCalciteSupersaturationEcologyPaleontologyForestryGeophysicschemistrySpace and Planetary ScienceIlliteIce nucleusengineeringGeologyJournal of Geophysical Research
researchProduct

Size distribution, mass concentration, chemical and mineralogical composition and derived optical parameters of the boundary layer aerosol at Tinfou,…

2009

During the SAMUM 2006 field campaign in southern Morocco, physical and chemical properties of desert aerosols were measured. Mass concentrations ranging from 30 Ã�¼g m-3 for PM2.5 under desert background conditions up to 300,000 Ã�¼g m-3 for total suspended particles (TSP) during moderate dust storms were measured. TSP dust concentrations are correlated with the local wind speed, whereas PM10 and PM2.5 concentrations are determined by advection from distant sources. Size distributions were measured for particles between 20 nm and 500 Ã�¼m diameter (parameterizations are given). Two major regimes of the size spectrum can be distinguished. Smaller than 500 nm particle diameter, the distrib…

Atmospheric Sciencerefractive index010504 meteorology & atmospheric sciencesaerosolAtmosphärische SpurenstoffeMineralogySingle particle analysis010501 environmental sciencesMineral dust01 natural sciencesAerosolSAMUMParticle-size distributionUltrafine particlechemical compositionsingle-particle analysisParticleMass concentration (chemistry)Chemical compositionGeology0105 earth and related environmental sciencesTellus B: Chemical and Physical Meteorology
researchProduct