Search results for "METAL"

showing 10 items of 7908 documents

Passive and Active Biomonitoring of Atmospheric Aerosol with the Use of Mosses

2021

Abstract The aim of the carried out research was passive and active biomonitoring of woodlands in the Opole province. Pleurozium schreberi mosses were used during the research, in which the following heavy metals concentrations were determined: Mn, Fe, Ni, Cu, Zn, Cd and Pb. Concentrations were determined with absorption atomic spectrometry (AAS). On the basis of the carried out research, concentrations of heavy metals in moss samples used in the passive and active biomonitoring methods were compared. The obtained results indicate that Pleurozium schreberi mosses can be successfully used in both passive and active biomonitoring, however, these methods should not be used interchangeably in a…

010504 meteorology & atmospheric sciencesChemistry010501 environmental sciences01 natural sciencesactive biomonitoringAerosolmossesEnvironmental chemistrypassive biomonitoringBiomonitoringGeneral Materials Scienceheavy metalsatomic absorption spectrometry0105 earth and related environmental sciencesEcological Chemistry and Engineering S-Chemia I Inzynieria Ekologiczna S
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Geochemical insights into the relationship of rock varnish and adjacent mineral dust fractions

2020

Abstract Rock varnishes are μm-thin, dark, manganese(Mn)-rich crusts that accrete in the order of few μm/ka on weathering-resistant lithologies. Although these crusts can form in all climates, they are best known in arid to semi-arid settings. Aeolian dust is understood as a major contributor to the distinct trace metal and REE enrichments in rock varnish. However, the exact proportions of abiotic and biotic formation mechanisms that may explain the oxidation-reactions of Mn2+ to Mn4+, present as Mn oxyhydroxides in the varnish, are still a matter of ongoing debate. We present here the first systematic study of trace element enrichment processes between the uppermost layer of the varnish se…

010504 meteorology & atmospheric sciencesDesert varnishVarnishTrace elementGeochemistryGeologyMineral dust010502 geochemistry & geophysics01 natural sciencesGeochemistry and Petrologyvisual_artvisual_art.visual_art_mediumAeolian processesTrace metalClay mineralsQuartzGeology0105 earth and related environmental sciencesChemical Geology
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Anthropogenic lead distribution in soils under arable land and permanent grassland estimated by Pb isotopic compositions

2008

International audience; The role of land use on fate of metals in soils is poorly understood. In this work, we studied the incorporation of lead in two neighboring soils with comparable pedogenesis but under long-term different agricultural management. Distributions of anthropogenic Pb were assessed from concentrations and isotopic compositions determined on bulk horizon samples, systematical 5–10 cm increment samples, and on 24-h EDTA extracts. Minor amounts of anthropogenic lead were detected until 1-m depth under permanent grassland, linked to high earthworm activity. In arable land, exogenous Pb predominantly accumulated at depths <60 cm. Although the proximity between the two sites ens…

010504 meteorology & atmospheric sciencesHealth Toxicology and MutagenesisMETAL POLLUTIONLANTHANUM010501 environmental sciencesToxicology01 natural sciencesanalyse de solIsotopesSoil PollutantsLAND USEIsotope analysis2. Zero hungerbiologySolid Phase ExtractionprairiePb ISOTOPIC COMPOSITIONSAgricultureGeneral Medicineanalyse comparativePollutionSoil contaminationDeposition (aerosol physics)Environmental chemistryFranceArable landEnvironmental MonitoringMETAL POLLUTION;LAND USE;Pb ISOTOPIC COMPOSITIONS;ANTHROPOGENIC;LANTHANUMIndustrial WastePoaceaesol cultivéplombmétal lourdEdetic Acid0105 earth and related environmental sciencesHydrologyLand useEnvironmental and SocietyEarthworm15. Life on landbiology.organism_classificationANTHROPOGENICpollution du sol[SDE.ES]Environmental Sciences/Environmental and SocietyPedogenesisLead13. Climate actionSoil waterEnvironmental scienceEnvironnement et Société
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Changes in SO2 Flux Regime at Mt. Etna Captured by Automatically Processed Ultraviolet Camera Data

2019

We used a one-year long SO2 flux record, which was obtained using a novel algorithm for real-time automatic processing of ultraviolet (UV) camera data, to characterize changes in degassing dynamics at the Mt. Etna volcano in 2016. These SO2 flux records, when combined with independent thermal and seismic evidence, allowed for capturing switches in activity from paroxysmal explosive eruptions to quiescent degassing. We found SO2 fluxes 1.5&#8722;2 times higher than the 2016 average (1588 tons/day) during the Etna&#8217;s May 16&#8722;25 eruptive paroxysmal activity, and mild but detectable SO2 flux increases more than one month before its onset. The SO2 flux typically peaked during a lava fo…

010504 meteorology & atmospheric sciencesLava2SO<sub>2</sub> fluxesAutomatic processing010502 geochemistry & geophysicsAtmospheric sciencesmedicine.disease_causeUV Camerafluxe01 natural sciencesFlux (metallurgy)Thermalmedicinelcsh:Scienceexplosive basaltic volcanism0105 earth and related environmental sciencesSOExplosive eruptionEtna VolcanofluxesEtna volcanoGeneral Earth and Planetary Scienceslcsh:QEtna volcano; Explosive basaltic volcanism; SO; 2; fluxes; UV cameraGeologyUltravioletRemote Sensing
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Sustaining persistent lava lakes: Observations from high-resolution gas measurements at Villarrica volcano, Chile

2016

International audience; Active lava lakes – as the exposed upper part of magmatic columns – are prime locations to investigate the conduit flow processes operating at active, degassing volcanoes. Persistent lava lakes require a constant influx of heat to sustain a molten state at the Earth's surface. Several mechanisms have been proposed to explain how such heat transfer can operate efficiently. These models make contrasting predictions with respect to the flow dynamics in volcanic conduits and should result in dissimilar volatile emissions at the surface. Here we look at high-frequency SO2 fluxes, plume composition, thermal emissions and aerial video footage from the Villarrica lava lake i…

010504 meteorology & atmospheric sciencesLavaEarth scienceUAVUV camera010502 geochemistry & geophysics01 natural sciencesElectrical conduitFlux (metallurgy)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeophysic0105 earth and related environmental sciencesgeographyTrail By Firegeography.geographical_feature_categoryTrail ByLava domeFireconduit dynamicPlumeGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGas slugMagmavolcanic degassingGeologyMulti-GAS
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Using mosses as biomonitors to study trace element emissions and their distribution in six different volcanic areas

2017

Volcanoes emit SO2, CO2, and H2S, but also trace elements gases and particles such as As, Cd, Cr, Cu, Hg, Ni, Pb, and Sb. Active moss bag biomonitoring, an easy to apply and low budget method, was used to determine trace element release from volcanic areas of different geological context and climates. Exposure height variations (0.7–1.6 m above ground) due to different availability of natural tie points did not affect the results. Accumulation was linear for exposure durations from three days to nine weeks, so values were comparable by normalization to moss exposure time. Uncovered moss bags showed higher accumulation than co-exposed covered ones because of additional dust and wet deposit…

010504 meteorology & atmospheric sciencesLavaMineralogyContext (language use)010501 environmental sciences01 natural sciencesVolcanic GasesGeochemistry and PetrologyBiomonitoringeventGeophysicVolatiles0105 earth and related environmental sciencesevent.disaster_typeVolatile elementVolcanic emissiongeographygeography.geographical_feature_categorybiologyTrace elementActive biomonitoringbiology.organism_classificationMossGeophysicsVolcanoMetal(loid)GeologyJournal of Volcanology and Geothermal Research
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Trace elements in the thermal groundwaters of Vulcano Island (Sicily)

2000

The chemical concentrations of many trace elements that have never before been examined in Vulcano Island groundwaters are reported. Chemical data indicate that rock composition is not the only factor determining the metal content in the aqueous system. The observed concentrations depend mainly on: (1) the chemical composition of the host rocks; (2) the chemical–physical conditions of the weathering solution (temperature, acidity, redox conditions); (3) input of magmatic gases; (4) adsorption of metal ions on oxide particles, formation of soluble complexes and/or precipitation of solid phases. Chloride complexes in solution are of minimal significance for all elements with the exception of …

010504 meteorology & atmospheric sciencesMetal ions in aqueous solutionMineralogyWeathering010502 geochemistry & geophysics01 natural sciencesChlorideMetalchemistry.chemical_compoundGeochemistry and Petrologymedicine[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentChemical compositionComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAqueous solutionTrace element6. Clean waterGeophysicschemistry13. Climate actionvisual_artEnvironmental chemistryvisual_art.visual_art_mediumCarbonateGeologymedicine.drug
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Massive Oe/Be stars at low metallicity: Candidate progenitors of long GRBs?

2010

At low metallicity the B-type stars rotate faster than at higher metallicity, typically in the SMC. As a consequence, it was expected a larger number of fast rotators in the SMC than in the Galaxy, in particular more Be/Oe stars. With the ESO-WFI in its slitless mode, the SMC open clusters were examined and an occurence of Be stars 3 to 5 times larger than in the Galaxy was found. The evolution of the angular rotational velocity seems to be the main key on the understanding of the specific behaviour and of the stellar evolution of such stars at different metallicities. With the results of this WFI study and using observational clues on the SMC WR stars and massive stars, as well as the theo…

010504 meteorology & atmospheric sciencesMetallicityAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciencesAstrophysicsAstrophysics::Cosmology and Extragalactic Astrophysics01 natural sciencesstars: rotation0103 physical sciencesMagellanic CloudsAstrophysics::Solar and Stellar Astrophysics010303 astronomy & astrophysicsStellar evolutionSolar and Stellar Astrophysics (astro-ph.SR)Astrophysics::Galaxy Astrophysics0105 earth and related environmental sciencesPhysics[SDU.ASTR.SR]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Solar and Stellar Astrophysics [astro-ph.SR]Astronomy and Astrophysicsgamma rays: general[PHYS.ASTR.SR]Physics [physics]/Astrophysics [astro-ph]/Solar and Stellar Astrophysics [astro-ph.SR]GalaxyStarsAstrophysics - Solar and Stellar AstrophysicsSpace and Planetary Sciencestars: supernovae: generalAstrophysics::Earth and Planetary AstrophysicsOpen cluster
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2016

Gianluca Tramontana was supported by the GEOCARBON EU FP7 project (GA 283080). Dario Papale, Martin Jung and Markus Reichstein acknowledge funding from the EU FP7 project GEOCARBON (grant agreement no. 283080) and the EU H2020 BACI project (grant agreement no. 640176). Gustau Camps-Valls wants to acknowledge the support by an ERC Consolidator Grant with grant agreement 647423 (SEDAL). Kazuhito Ichii was supported by Environment Research and Technology Development Funds (2-1401) from the Ministry of the Environment of Japan and the JAXA Global Change Observation Mission (GCOM) project (no. 115). Christopher R. Schwalm was supported by National Aeronautics and Space Administration (NASA) gran…

010504 meteorology & atmospheric sciencesMeteorologyFLUXNET0208 environmental biotechnology0207 environmental engineeringlcsh:Life02 engineering and technologySensible heatAtmospheric sciences7. Clean energy01 natural sciencesFlux (metallurgy)FluxNetMachine learning; Carbon fluxes; Energy fluxes; FLUXNET; Remote sensing; FLUXCOMlcsh:QH540-549.5Latent heatMachine learningCarbon fluxes020701 environmental engineeringEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesFLUXCOMMultivariate adaptive regression splineslcsh:QE1-996.5Empirical modellingPrimary production15. Life on landRemote sensingEnergy fluxes020801 environmental engineeringlcsh:Geologylcsh:QH501-531Kernel method13. Climate actionEnvironmental sciencelcsh:EcologyBiogeosciences
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Sr/Ca and Mg/Ca ratios of ontogenetically old, long-lived bivalve shells (Arctica islandica) and their function as paleotemperature proxies

2011

International audience; The Sr/Ca and Mg/Ca ratios of many biogenic skeletons provide useful paleotemperature estimates. As yet however, it has remained largely impossible to obtain such information from bivalve shells. In the present study, metal-to-calcium values in the hinge plate (aragonite, outer shell layer) of four ontogenetically old (85 to 374 year-old) specimens of the long-lived bivalve, Arctica islandica, were measured on a LA-ICP-MS. The shells were collected alive in 1868, 1986 and 2003 from three different localities around Iceland. With increasing ontogenetic age and decreasing growth rate, a distinct trend toward increasing Sr/Ca (max. 5.17 mmol/mol) and Mg/Ca values (max. …

010504 meteorology & atmospheric sciencesOntogenySea surface temperatureLongevityZoologyMineralogyAmbient waterengineering.materialSignificant negative correlation010502 geochemistry & geophysicsOceanography01 natural sciencesMetal-to-calcium ratioMole14. Life underwaterGrowth rateBivalve shellArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesVital effectbiologyAragonitePaleontologybiology.organism_classificationBivalve shell[SDE]Environmental Sciencesengineering
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