Search results for "Mineral"

showing 10 items of 2711 documents

The size distribution of primary biological aerosol particles in cloud water on the mountain Kleiner Feldberg/Taunus (FRG)

2000

During the field campaign, FELDEX 95 cloud water samples were collected and the insoluble particles were analysed by single particle analysis in order to determine the content of primary biological aerosol particles (PBAP). It is found that 25% of the total insoluble particles are biological ones. During cloud events with increasing wind velocity, the concentration of biological particles also increases. Anthropogenic influence leads to a higher amount of both total and biological particles. Within the size distribution, the percentage of biological particles decreases with increasing radius.

Atmospheric ScienceParticle-size distributionBiological particlesMineralogySingle particle analysisEnvironmental scienceCloud waterRadiusAtmospheric sciencescomplex mixturesField campaignWind speedAerosolAtmospheric Research
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Soil sedimentology at Gusev Crater from Columbia Memorial Station to Winter Haven

2008

[1] A total of 3140 individual particles were examined in 31 soils along Spirit's traverse. Their size, shape, and texture were quantified and classified. They represent a unique record of 3 years of sedimentologic exploration from landing to sol 1085 covering the Plains Unit to Winter Haven where Spirit spent the Martian winter of 2006. Samples in the Plains Unit and Columbia Hills appear as reflecting contrasting textural domains. One is heterogeneous, with a continuum of angular-to-round particles of fine sand to pebble sizes that are generally dust covered and locally cemented in place. The second shows the effect of a dominant and ongoing dynamic aeolian process that redistributes a un…

Atmospheric SciencePopulationGeochemistrySoil ScienceMineralogyAquatic ScienceOceanographyTexture (geology)Impact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)SedimentologyPebbleeducationEarth-Surface ProcessesWater Science and TechnologyMartiangeographyeducation.field_of_studygeography.geographical_feature_categoryEcologyPaleontologyForestryGeophysicsVolcanoSpace and Planetary ScienceAeolian processesGeologyJournal of Geophysical Research
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Composition-resolved size distributions of volcanic aerosols in the Mt. Etna plumes

2008

Particle size distributions for soluble and insoluble species in Mt. Etna's summit plumes were measured across an extended size range (10 nm < d < 100 μm) using a combination of techniques. Automated scanning electron microscopy (QEMSCAN) was used to chemically analyze many thousands of insoluble particles (collected on pumped filters) allowing the relationships between particle size, shape, and composition to be investigated. The size distribution of fine silicate particles (d < 10 μm) was found to be lognormal, consistent with formation by bursting of gas bubbles at the surface of the magma. The compositions of fine silicate particles were found to vary between magmatic and nearl…

Atmospheric ScienceQEMSCANSoil ScienceMineralogyNanoparticleAquatic ScienceOceanographychemistry.chemical_compoundGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryvolcanic aerosolsSilicateAerosolPlumeSettore GEO/08 - Geochimica E VulcanologiaEarth sciencesGeophysicsVolcanochemistrySpace and Planetary ScienceParticle-size distributionParticle sizeGeologyJOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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Characterization of the atmosphere during SEN2FLEX 2005 field campaign

2008

The European Space Agency carried out the Sentinel-2 and Fluorescence Experiment (SEN2FLEX) campaign in Barrax (Spain) during the summer of 2005, with the main objective of observe solar induced fluorescence signal using the AirFLEX airborne instrument over different vegetation targets in order to verify signal suitability for observations from space as proposed in the FLEX mission. A highly precise atmospheric correction is mandatory for adequate measurements of the AirFLEX instrument; thus a complete characterization of the atmosphere was programmed in SEN2FLEX in order to document the presence of atmospheric aerosols above the experimental area, as their effects represent the major sourc…

Atmospheric ScienceRadiació solarMeteorologySoil Science550 - Earth sciencesAquatic ScienceMineral dustOceanographyAtmosphereGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Satellite imageryEarth-Surface ProcessesWater Science and TechnologyRemote sensingAerosolsEcologyAtmospheric correctionPaleontologyForestryGeofísicaAerosolGeophysicsLidarSpace and Planetary ScienceEnvironmental scienceSatelliteWater vaporJOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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Column-integrated aerosol optical properties in Sodankylä (Finland) during the Solar Induced Fluorescence Experiment (SIFLEX-2002).

2006

[1] A study has been made of the column aerosols using solar irradiance extinction measurements at ground level in a boreal region (Sodankyla, Finland) during spring 2002. The aerosol properties have been related to air mass origin. In general, the aerosol levels were observed to be very low, independent of the air mass origin, with an aerosol optical depth (AOD) value at 500 nm of less than 0.09 ± 0.03. Two characteristic patterns were observed depending on whether the air masses originated in the north and west or from the south and east. In the first case (north and west origins) the aerosol load was very small, with very low optical depths in the range 0.03 ± 0.02 to 0.09 ± 0.03 for 500…

Atmospheric ScienceRadiació solarMeteorologySoil ScienceAquatic ScienceOceanographySolar irradianceAtmospheric sciencesGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Air massEarth-Surface ProcessesWater Science and TechnologyAerosolsEcologySpring seasonPaleontologyForestryGeofísicaAerosolGround levelWavelengthGeophysicsBorealSpace and Planetary ScienceExtinction (optical mineralogy)Environmental science
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One year of measurements with a POM02 radiometer at an Alpine EuroSkyRad statio

2014

Atmospheric ScienceRadiometerMeteorologySkymedia_common.quotation_subjectEnvironmental scienceMineral dustmedia_commonRemote sensing
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Individual-particle analysis of airborne dust samples collected over Morocco in 2006 during SAMUM 1

2011

During the course of SAMUM 1 in May and June 2006, airborne samples were collected in southern Morocco at altitudes between 830 and 3340 m above ground. We analysed approximately 22 500 particles of 1–30 μm by automated individual-particle analysis with a scanning electron microscope (SEM) and an energy-dispersive X-ray (EDX) analyser. The major difference between samples is due to the presence and amount of chlorine- and sulphur-bearing particles, pointing to a varying maritime influence and to different degrees of aging. In contrast, the desert dust component is very homogeneous independent of altitude, activated local source area, and dust storm intensity, implying very fast mixing of th…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesScanning electron microscopePalygorskiteMineralogy010501 environmental sciencesMineral dust01 natural sciencesAerosolAltitudeDust stormmedicineParticleEnvironmental science0105 earth and related environmental sciencesmedicine.drugTellus B: Chemical and Physical Meteorology
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Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006

2009

The Saharan Mineral Dust Experiment (SAMUM) was conducted in May/June 2006 in southern Morocco. As part of SAMUM, airborne in situ measurements of the particle size distribution in the diameter range 4 nm < Dp < 100 μm were conducted. The aerosol mixing state was determined below Dp < 2.5 μm. Furthermore, the vertical structure of the dust layers was investigated with a nadir-looking high spectral resolution lidar (HSRL). The desert dust aerosol exhibited two size regimes of different mixing states: below 0.5 μm, the particles had a non-volatile core and a volatile coating; larger particles above 0.5 μm consisted of non-volatile components and contained light absorbing material. In…

Atmospheric ScienceRange (particle radiation)Materials science010504 meteorology & atmospheric sciencesgiant particlesAnalytical chemistryAtmosphärische Spurenstoffemixing state010501 environmental sciencesMineral dust01 natural sciencesAerosoldust layer structureTroposphereSAMUMdesert dustParticle-size distributionUltrafine particleParticle sizeparticle size distributionSpectral resolutionairborne measurements0105 earth and related environmental sciencesRemote sensingTellus B
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Hygroscopic properties and water-soluble volume fraction of atmospheric particles in the diameter range from 50 nm to 3.8 μm during LACE 98

2002

[1] Hygroscopic properties of atmospheric aerosol particles in the Aitken, large, and giant particle range were studied during the Lindenberg Aerosol Characterization Experiment (LACE 98) in a rural area 80 km southeast of Berlin. The hygroscopic behavior of Aitken particles were determined in situ in four size classes (50, 100, 150, 250 nm) with a Hygroscopic Tandem Differential Mobility Analyzer for relative humidities (RH) of 60% and 90%. Measurements at 60% RH served as reference data used by other LACE 98 investigators for mass closure and radiative transfer calculations. In most cases, at 90% RH, the atmospheric particles could be classified into two groups (“more” and “less” hygrosco…

Atmospheric ScienceRange (particle radiation)Materials scienceEcologyAnalytical chemistryPaleontologySoil ScienceMineralogyForestryFraction (chemistry)Aquatic ScienceOceanographyAerosolGeophysicsVolume (thermodynamics)Space and Planetary ScienceGeochemistry and PetrologyDifferential mobility analyzerVolume fractionEarth and Planetary Sciences (miscellaneous)ParticleParticle sizeEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Atmospheres
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Rainwater composition over a rural area with special emphasis on the size distribution of insoluble particulate matter

1987

The rainwater composition in the vicinity of Mainz, FRG, has been investigated with special emphasis on insoluble constituents. The number size distribution was determined in the range from 0.1 μm up to 100 μm radius. For particles with r>0.5 μm radius the shape of the size distribution of insoluble particles in rain follows the shape of the average urban and rural aerosol. In this particular size range no major size selective removal processes could be seen. For r<0.5 μm the number size distribution tends to flatten compared to the average aerosol. This might be the indication of a size selective removal process (Greenfield Gap).

Atmospheric ScienceRange (particle radiation)Materials scienceEnvironmental ChemistryMineralogyComposition (visual arts)RadiusParticulatesSize selectiveChemical compositionRainwater harvestingAerosolJournal of Atmospheric Chemistry
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