Search results for "MINERALOGY"

showing 10 items of 1516 documents

The Flux Density of Radiation Energy Originating from the Circumsolar Sky Measured at Groundbased Stations

1983

The aim of this project was the measurement of the radiant energy flux provided by the diffuse radiation of the ring shaped area of the sky around the unmasked sun disk. More than 200 measurements of the irradiance of this circumsolar cloudy or cloudfree sky up to an angular radius of 10° had been taken at Mainz (FRG), Deuselbach (FRG) and Adrano (Sicily). The measurements show that the irradiance of the circumsolar sky radiation may reach an amount of more then 30 % of the direct solar irradiance at the observation site. This means, optical systems combining the direct solar radiation and the circumsolar radiation may compensate — at least partly — the extinction losses of the direct solar…

AtmosphereRadiant fluxExtinction (optical mineralogy)Skymedia_common.quotation_subjectIrradianceDiffuse sky radiationAstronomyEnvironmental scienceRadiant energyAtmospheric sciencesSolar irradiancemedia_common
researchProduct

CO2 and H2S concentrations in the atmosphere at the Solfatara of Pozzuoli

1984

The CO2 and H2S concentration in the Solfatara atmosphere has been measured. The concentrations of both gases are higher neraby the more active areas and decrease away from them. A sharp horizontal and vertical gradient of the CO2 content has been recognized.

Atmospherechemistry.chemical_compoundCO2 contentchemistryGeochemistry and PetrologyHydrogen sulfideCarbon dioxideMineralogyVolcanismSedimentologyGeologyFumaroleBulletin Volcanologique
researchProduct

2016

Abstract. Cloud residues and out-of-cloud aerosol particles with diameters between 150 and 900 nm were analysed by online single particle aerosol mass spectrometry during the 6-week study Hill Cap Cloud Thuringia (HCCT)-2010 in September–October 2010. The measurement location was the mountain Schmücke (937 m a.s.l.) in central Germany. More than 160 000 bipolar mass spectra from out-of-cloud aerosol particles and more than 13 000 bipolar mass spectra from cloud residual particles were obtained and were classified using a fuzzy c-means clustering algorithm. Analysis of the uncertainty of the sorting algorithm was conducted on a subset of the data by comparing the clustering output with parti…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryMineralogy010501 environmental sciencesAtmospheric sciencesmedicine.disease_causecomplex mixtures01 natural sciencesSootAerosolchemistry.chemical_compoundLiquid water contentmedicineCloud condensation nucleiParticleAerosol mass spectrometrysense organsSulfateSea salt aerosol0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
researchProduct

Electron microscopy of particles collected at Praia, Cape Verde, during the Saharan Mineral Dust Experiment: particle chemistry, shape, mixing state …

2011

A large field experiment of the Saharan Mineral Dust Experiment (SAMUM) was performed in Praia, Cape Verde, in January and February 2008. The aerosol at Praia is a superposition of mineral dust, sea-salt, sulphates and soot. Particles smaller than 500 nm are mainly mineral dust, mineral dust–sulphate mixtures, sulphates and soot–sulphate mixtures. Particles larger then 2.5 μm consist of mineral dust, sea-salt and few mineral dust–sulphate mixtures. A transition range exists in between. The major internal mixtures are mineral dust–sulphate and soot–sulphate. Mineral dust–sea-salt mixtures occur occasionally, mineral dust–soot mixtures were not observed. The aspect ratio was 1.3–1.4 for dry p…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryMineralogy010501 environmental sciencesMineral dustmedicine.disease_causecomplex mixtures01 natural sciencesSootAerosolCape verdeAbsorption edgemedicineParticleParticle sizeAbsorption (electromagnetic radiation)0105 earth and related environmental sciencesTellus B: Chemical and Physical Meteorology
researchProduct

Properties of individual contrails: a compilation of observations and some comparisons

2017

International audience; Mean properties of individual contrails are characterized for a wide range of jet aircraft as a function of age during their life cycle from seconds to 11.5 h (7.4-18.7 km altitude, -88 to -31 °C ambient temperature), based on a compilation of about 230 previous in situ and remote sensing measurements. The airborne, satellite, and ground-based observations encompass exhaust contrails from jet aircraft from 1972 onwards, as well as a few older data for propeller aircraft. The contrails are characterized by mean ice particle sizes and concentrations, extinction, ice water content, optical depth, geometrical depth, and contrail width. Integral contrail properties includ…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyreviewice010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesoptical depthlcsh:Chemistryremote sensingPhase (matter)ddc:551Relative humidityOptical depth0105 earth and related environmental sciencesJet (fluid)Institut für Physik der AtmosphäreIce crystalsFernerkundung der AtmosphäreAtmosphärische Spurenstoffecontraillcsh:QC1-999Warm frontdatain-situlcsh:QD1-999Extinction (optical mineralogy)[SDU]Sciences of the Universe [physics]Environmental scienceCirrusmeasurementslcsh:PhysicsAtmospheric Chemistry and Physics
researchProduct

The scavenging of two different types of marine aerosol particles calculated using a two-dimensional detailed cloud model

2011

Our 2-D dynamic model including spectral microphysics and scavenging has been evaluated for a warm precipitating convective cloud at Day 261 (18 September 1974) of the GATE campaign. Two different chemical species ((NH 4 ) 2 SO 4 and NaCl) of aerosol particles were followed in the air, inside the drops in the cloud, and inside the drops reaching the ground. Concerning the dynamics and microphysics, as well as the scavenging and wet deposition, the model results agree quite well with available observations. The cloud rained after 19 min of cloud life time. For the considered aerosol loading of the atmosphere, rough estimates are derived for the total material processed by such a warm convect…

Atmospheric Science010504 meteorology & atmospheric sciencesMicrophysicsChemistryDrop (liquid)Analytical chemistryMineralogy01 natural sciencesAerosol13. Climate actionLiquid water contentCloud baseMixing ratioRelative humidityScavenging0105 earth and related environmental sciencesTellus B
researchProduct

Ground-based off-line aerosol measurements at Praia, Cape Verde, during the Saharan Mineral Dust Experiment: microphysical properties and mineralogy

2011

A large field experiment of the Saharan Mineral Dust Experiment (SAMUM) was performed in Praia, Cape Verde, in January and February 2008. This work reports on the aerosol mass concentrations, size distributions and mineralogical composition of the aerosol arriving at Praia. Three dust periods were recorded during the measurements, divided by transitional periods and embedded in maritime-influenced situations. The total suspended particle mass/PM 10 /PM 2.5 were 250/180/74 μg/m 3 on average for the first dust period (17–21 January) and 250/230/83 μg/m 3 for the second (24–26 January). The third period (28 January to 2 February) was the most intensive with 410/340/130 μg/m 3 . Four modes were…

Atmospheric Science010504 meteorology & atmospheric sciencesMineralogy010501 environmental sciencesengineering.materialMineral dust01 natural sciencesAerosolCape verdedust ; aerosol ; clay particles ; microphysical propertiesIlliteengineeringEnvironmental sciencePlagioclaseKaoliniteHaliteQuartz0105 earth and related environmental sciencesTellus B
researchProduct

Electrical conductivity of magma in the course of crystallization controlled by their residual liquid composition.

2005

International audience; The electrical conductivity of a magma in the course of crystallization was experimentally investigated in the temperature range of 1350–1018°C. Large samples of basaltic composition with a homogeneous crystal content were synthesized in a gas mixing furnace at 1 atm pressure. The samples were analyzed by electron microprobe. The relative proportions of the phases as a function of temperature were determined. Depending on temperature, the phase assemblies included quenched silicate liquid, ±plagioclase, ±pyroxene, ±Fe-Ti oxides. The crystal content varied from 0 to 80 wt %. In response to partial crystallization, the residual liquid changed composition from basalt, t…

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesMagmaSoil ScienceMineralogyThermodynamicsSilicate meltLiquidusAquatic ScienceConductivity010502 geochemistry & geophysicsOceanography01 natural sciencesSilicate melt.law.inventionchemistry.chemical_compoundGeochemistry and PetrologyElectrical resistivity and conductivityLiquid crystallawEarth and Planetary Sciences (miscellaneous)Electrical conductivity[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyElectrical measurementsCrystallization0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyFractional crystallization (geology)EcologyPaleontologyForestrySilicateGeophysicschemistry13. Climate actionSpace and Planetary ScienceGeology
researchProduct

Anisotropic scaling of tectonic stylolites: A fossilized signature of the stress field?

2010

International audience; [1] Vertical stylolites are pressure solution features, which are considered to be caused by horizontal tectonic loading, with the largest principal compressive stress being (sub-) parallel to the Earth's surface. In the present study we analyze the roughness of such tectonic stylolites from two tectonic settings in southern Germany and northeastern Spain, aiming to investigate their scaling properties with respect to the stress during formation. High-resolution laser profilometry was carried out on opened stylolite surfaces of nine samples. These data sets were then analyzed using one-and two-dimensional Fourier power spectral approaches. We found that tectonic styl…

Atmospheric Science010504 meteorology & atmospheric sciences[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSoil ScienceMineralogyGeometryAquatic Science010502 geochemistry & geophysicsOceanography01 natural sciencesPhysics::GeophysicsStress (mechanics)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)AnisotropyScaling0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[PHYS]Physics [physics]EcologyCauchy stress tensorPaleontologyForestryStress fieldTectonicsGeophysics13. Climate actionSpace and Planetary ScienceStylolitePressure solutionGeologyJournal of Geophysical Research
researchProduct

2012

Abstract. One of the major uncertainties in the understanding of Earth's climate system is the interaction between solar radiation and aerosols in the atmosphere. Aerosols exposed to high humidity will change their chemical, physical, and optical properties due to their increased water content. To model hydrated aerosols, atmospheric chemistry and climate models often use the volume weighted mixing rule to predict the complex refractive index (RI) of aerosols when they interact with high relative humidity, and, in general, assume homogeneous mixing. This study explores the validity of these assumptions. A humidified cavity ring down aerosol spectrometer (CRD-AS) and a tandem hygroscopic DMA…

Atmospheric Science010504 meteorology & atmospheric sciencesbusiness.industryChemistryScatteringMie scatteringAnalytical chemistry010501 environmental sciencesMolar absorptivity01 natural sciencesAerosolOptics13. Climate actionExtinction (optical mineralogy)Differential mobility analyzerRelative humiditybusinessMixing (physics)0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
researchProduct