Search results for "MINERALOGY"

showing 10 items of 1516 documents

Sources, size distribution, and downwind grounding of aerosols from Mount Etna

2006

The number concentrations and size distributions of aerosol particles >0.3 mm diameter were measured at the summit of Mount Etna and up to 10 km downwind from the degassing vents during July and August 2004. Aerosol number concentrations reached in excess of 9 106 L1 at summit vents, compared to 4–8 104 L1 in background air. Number concentrations of intermediate size particles were higher in emissions from the Northeast crater compared to other summit crater vents, and chemical composition measurements showed that Northeast crater aerosols contained a higher mineral cation content compared to those from Voragine or Bocca Nuova, attributed to Strombolian or gas puffing activity within the ve…

Atmospheric Sciencegeographygeography.geographical_feature_categoryEcologyParticle numberPaleontologySoil ScienceMineralogyForestryAquatic ScienceOceanographyStrombolian eruptionPlumeAerosolGeophysicsImpact craterVolcanoSpace and Planetary ScienceGeochemistry and PetrologyParticle-size distributionEarth and Planetary Sciences (miscellaneous)PanacheEnvironmental scienceEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Atmospheres
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Application of aerosol optical properties to estimate aerosol type from ground-based remote sensing observation at urban area of northeastern China

2015

Abstract Aerosol optical properties were derived from ground-based sunphotometer observations between 2009-2013 at three urban sites of Shenyang, Anshan, Fushun in northeastern China. The annual means for extinction aerosol optical depths (EAOD) at 500 nm were 0.57±0.38, 0.52±0.35, and 0.41±0.31 at Shenyang, Anshan, Fushun, respectively. The corresponding annual means for the extinction Angstrom exponents (EAE) computed for the wavelengths of 440 and 870 nm were 0.86±0.32, 0.86±0.34 and 0.91±0.35, respectively, indicating that urban area of Northeast China were affected by both coarse and fine particles. Hygroscopic growth in summer and incursions of dust aerosols in spring were evidently r…

Atmospheric Sciencegeographygeography.geographical_feature_categoryMeteorologyCoal combustion productsMineral dustUrban areaAtmospheric sciencesAerosolGeophysicsSpace and Planetary ScienceExtinction (optical mineralogy)Environmental scienceAngstromBiomass burningAbsorption (electromagnetic radiation)Journal of Atmospheric and Solar-Terrestrial Physics
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The tropospheric processing of acidic gases and hydrogen sulphide in volcanic gas plumes as inferred from field and model investigations

2007

Abstract. Improving the constraints on the atmospheric fate and depletion rates of acidic compounds persistently emitted by non-erupting (quiescent) volcanoes is important for quantitatively predicting the environmental impact of volcanic gas plumes. Here, we present new experimental data coupled with modelling studies to investigate the chemical processing of acidic volcanogenic species during tropospheric dispersion. Diffusive tube samplers were deployed at Mount Etna, a very active open-conduit basaltic volcano in eastern Sicily, and Vulcano Island, a closed-conduit quiescent volcano in the Aeolian Islands (northern Sicily). Sulphur dioxide (SO2), hydrogen sulphide (H2S), hydrogen chlori…

Atmospheric Sciencegeographygeography.geographical_feature_categoryMineralogychemistry.chemical_elementAtmospheric sciencesSulfurPlumeDilutionAerosolTroposphereAtmospherechemistry.chemical_compoundchemistryVolcanoHydrogen chlorideAtmospheric Chemistry and Physics
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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
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Saharan dust absorption and refractive index from aircraft-based observations during SAMUM 2006

2009

During the Saharan Mineral Dust Experiment (SAMUM) conducted in summer 2006 in southeast Morocco, the complex refractive index of desert dust was determined from airborne measurements of particle size distributions and aerosol absorption coefficients at three different wavelengths in the blue (467 nm), green (530 nm) and red (660 nm) spectral regions. The vertical structure of the dust layers was analysed by an airborne high spectral resolution lidar (HSRL). The origin of the investigated dust layers was estimated from trajectory analyses, combined with Meteosat 2nd Generation (MSG) scenes and wind field data analyses. The real part n of the dust refractive index was found almost constant w…

Atmospheric Sciencerefractive indexMaterials science010504 meteorology & atmospheric sciencesaerosolAtmosphärische SpurenstoffeMineralogy010501 environmental sciencesMineral dust01 natural sciencesAerosolSAMUMTroposphereWavelengthLidarSpectral resolutionAbsorption (electromagnetic radiation)absorptionRefractive index0105 earth and related environmental sciencesRemote sensingTellus B: Chemical and Physical Meteorology
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Hydrothermal macroscopic Fe-sepiolite from Oujda Mounts (Middle Atlas, Eastern Morocco)

2008

The Triassic-Jurassic series in the Oujda Mounts (Middle Atlas, NE Morocco) includes two basaltic units. The whole sequence is crosscut by veins filled with Fe-sepiolite + chalcedony + calcite + smectite and mixed layer talc-saponite. Fe-sepiolite occurs as macroscopic fibres and is one of the latest mineral phases in the filling sequence of the veins. The compositional relationships and crystallographic parameters obtained on carefully selected samples of sepiolite are compared with previous data, and support the actual development of Mg-Fe substitution in this clay mineral, given the adequate hydrothermal conditions. Genesis of this uncommon variety of sepiolite in veins is interpreted as…

BasaltCalciteMineralChalcedonySepioliteGeochemistryMineralogyGeologyengineering.materialHydrothermal circulationchemistry.chemical_compoundSequence (geology)chemistryengineeringClay mineralsGeologyEarth-Surface ProcessesJournal of African Earth Sciences
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Occurrence of Fibrous Sepiolite in Alkaline Basalt in the Valley of Alfara (Baix Ebre, Tarragona, Spain)

1994

BasaltGeochemistry and PetrologySepioliteGeochemistryMineralogy020101 civil engineering02 engineering and technology010502 geochemistry & geophysics01 natural sciencesGeology0201 civil engineering0105 earth and related environmental sciencesClay Minerals
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Trace element partitioning in lamproitic magmas—the Gaussberg olivine leucitite

2004

Abstract Partition coefficients for compatible and incompatible trace elements for use in modelling the origin and evolution of lamproitic and other potassic rocks are reported. These are based on values obtained by in situ determination using laser ablation microprobe-inductively coupled plasma-mass spectrometry (LAM-ICP-MS) on mineral/glass pairs in examples of the Gaussberg olivine leucitite, a classic leucite lamproite. Leucite/melt partition coefficients for 32 elements show values above 1 only for Cs and Rb, whereas values for Ni, Ga and Co are 0.4–0.1. DLc/Lq for most other elements are in the range 0.07–0.0005, and delineate a gently sloping pattern to lower values for elements gene…

BasaltIncompatible elementMineralOlivineGeochemistryTrace elementMineralogyGeologyengineering.materialPeralkaline rockPartition coefficientGeochemistry and PetrologyengineeringLeuciteGeologyLithos
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Visible and near-infrared multispectral analysis of geochemically measured rock fragments at the Opportunity landing site in Meridiani Planum

2010

[1] We have used visible and near-infrared Panoramic Camera (Pancam) spectral data acquired by the Opportunity rover to analyze 15 rock fragments at the Meridiani Planum landing site. These spectral results were then compared to geochemistry measurements made by the in situ instruments Mossbauer (MB) and Alpha Particle X-ray Spectrometer (APXS) to determine the feasibility of mineralogic characterization from Pancam data. Our results suggest that dust and alteration rinds coat many rock fragments, which limits our ability to adequately measure the mineralogy of some rocks from Pancam spectra relative to the different field of view and penetration depths of MB and APXS. Viewing and lighting …

BasaltMeridiani PlanumAtmospheric ScienceEcologyOutcropNear-infrared spectroscopyMultispectral imagePaleontologySoil ScienceMineralogyForestryMars Exploration ProgramAquatic ScienceOceanographyGeophysicsMeteoriteRock fragmentSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Trace elements in natural metallic iron from Disko Island, Greenland

1986

The largest occurrence of natural metallic iron on Earth is on the island of Disko, Greenland. Metallic iron is found there in a variety of different types, from small metal particles in basalts to large meter-sized blocks. We have studied three different types of metallic iron: small metal spherules (< 300 μm) in basaltic magma; larger metal grains (300 μm-3 mm), often composed of aggregates of smaller particles, in similar host rocks; and massive iron lumps (up to several tons). Analytical data for 13 siderophile elements in samples from these three types are presented. All metals analysed have a distinctly crustal pattern of siderophile elements. High Co/Ni, Re/Ir or W/Ir ratios clearly …

BasaltMetalGeophysicsSettlingGeochemistry and PetrologyIron metalvisual_artvisual_art.visual_art_mediumGeochemistryMineralogyGeological evidenceGeologyMantle (geology)Contributions to Mineralogy and Petrology
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