Search results for "Vulcano"

showing 10 items of 469 documents

CHEMICAL AND MINERALOGICAL CHARACTERIZATION OF ETNEAN VOLCANIC EMISSIONS USING ACTIVE BIOMONITORING TEC HNIQUE (MOSS-BAGS)

2011

biomonitoring moss-bags trace elementsSettore GEO/08 - Geochimica E Vulcanologia
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A computational study of point defects and diffusion in enstatite

2009

In order to contribute to the understanding of diffusion processes in enstatite (Mg2Si2O6), we have used atomistic simulation techniques to study point defects in this mineral. We present results for a variety of Scottky and Frenkel defects of all atomic species present in it. We have furthermore calculated the activation energy for magnesium diffusion. We break diffusion down into a succession of hops between neighboring sites. Each hop is associated with a migration energy barrier. By making a series of hops, the diffusing ion may cross the unit cell. The maximum migration energy necessary to attain movement in a direction is the activation energy for diffusion in that direction. The defe…

Settore GEO/06 - Mineralogiaenstatite defects diffusion computer simulationsSettore GEO/08 - Geochimica E Vulcanologia
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Alteration effects of volcanic ash in seawater: Anomalous Y/Ho ratios in coastal waters of the Central Mediterranean sea

2007

This paper presents the results of a study based on data collected during the oceanographic cruise ANSIC 2001 carried out in the Ionian Sea during the explosive activity of Mount Etna in the summer of 2001. Anomalous low values of Y/Ho ratios in seawater suggest extensive scavenging processes on the surfaces of smectitic alteration products, with Y and Ho fractionation controlled by the differences in their electronic configurations and behaviour during solution/surface complexation equilibria. These processes can also be traced through the presence of significant tetrad effects recorded in the chondrite-normalised Rare Earth Elements and Yttrium (YREEs) patterns of suspended particulate ma…

Geochemistrychemistry.chemical_elementYttriumFractionationParticulatesSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundMontmorilloniteMediterranean seachemistryGeochemistry and PetrologySeawaterScavengingY/HoGeologyY/Ho ratio REE Geochemical behaviour volcanic ash.Volcanic ash
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SEA-LEVEL AND CLIMATIC CHANGES DURING THELAST 41,000 YEARS IN THE OUTER SHELF OF THE SOUTHERN TYRRHENIAN SEA: EVIDENCE FROM FORAMINIFERA AND SEISMOST…

2012

Sea Level Changes QuaternarySettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/01 - Paleontologia E PaleoecologiaVariazioni del livello marino QuaternarioSettore GEO/08 - Geochimica E Vulcanologia
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Rain-ash interaction during paroxysmal events as potential input of toxic trace element in the environment: example from Mt. Etna Volcano

2012

Rain Ash EtnaSettore GEO/08 - Geochimica E Vulcanologia
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New insight into halogen release from experimental studies on BrO/Br ratios in volcanic plumes

2014

Plumes halogens BrSettore GEO/08 - Geochimica E Vulcanologia
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Surface hydrographic changes at the western flank of the sicily channel associated with the last sapropel

2021

Abstract In the eastern Mediterranean Sea, the early Holocene was characterized by major climatic and oceanographic changes that led to the formation of the last sapropel (S1) between 10.8 and 6.1 kyr cal. BP. These hydrographic changes might have altered the water exchange between the eastern and western Mediterranean sub-basins through the Strait of Sicily, but the existing evidences are inconclusive. In the present study we show new evidence from sediment core NDT-6-2016 located at the western flank of the Sicily channel, a key location to monitor the surface/intermediate water exchange between the two Mediterranean sub-basins. We perform paleo-hydrographic reconstructions based on plank…

Mediterranean climate010506 paleontology010504 meteorology & atmospheric sciencesOceanographyMonsoon01 natural sciencesPlanktic foraminifera Sapropel Strait of Sicily Surface hydrographyForaminiferaPaleoceanografiaPaleoceanographyMediterranean SeaHydrography14. Life underwaterHoloceneGlobigerinoides0105 earth and related environmental sciencesGlobal and Planetary ChangebiologyMediterrània (Mar)Globigerina bulloidesSapropelSettore GEO/01 - Paleontologia E PaleoecologiaHidrografiabiology.organism_classificationSettore GEO/08 - Geochimica E VulcanologiaSapropel; Planktic foraminifera; Surface hydrography; Strait of SicilyOceanography13. Climate actionHydrographyGeology
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A New Web-Based Catalog of Earth Degassing Sites in Italy

2008

Italy is a region characterized by intense and widespread processes of Earth degassing. High-temperature gases are released by crater plumes and fumaroles in volcanic environments throughout Italy. Also prevalent are numerous low-temperature gas emissions rich in carbon dioxide (CO2). These low-temperature emissions are located in a large area, mainly in the western sector of central and southern Italy (Figure 1).

geographygeography.geographical_feature_categoryEarth scienceGas emissionsSoil degassing - gas hazard - catalog soil manifestationsFumaroleSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundchemistryVolcanoImpact craterCarbon dioxidegas emissions in ItalyGeneral Earth and Planetary Sciencescatalogue of gas emissionsCO2 degassing; catalogue of gas emissions; gas emissions in ItalyCO2 degassingGeologyEarth (classical element)Eos, Transactions American Geophysical Union
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CO2 flux measurements in volcanic areas using the dynamic concentration method: the influence of the soil permeability.

2006

In order to evaluate the influence of soil permeability on soil CO2 flux measurements performed with the dynamic concentration method, several tests were carried out using soils characterized by different permeability values and flow rates. A special device was assembled in the laboratory to create a one-dimensional gas flow through a soil of known permeability. Using the advective-diffusion theory, a physical model to predict soil concentration gradients was also developed. The calculated values of CO2 concentrations at different depths were compared with those measured during the tests and a good agreement was found. Four soils with different gas permeability (3.6 x 10(-2) to 1.23 x 10(2)…

LITTERMOUNT-ETNARESPIRATIONVULCANO-ISLANDCARBON-DIOXIDE EVOLUTIONEARTHQUAKEFAULTSEMISSIONSSCALEREGION
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Diffuse soil CO2 degassing from Linosa island

2014

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Volcano monitoringLineamentGeochemistrysoil degassingfluid geochemistryCO2lcsh:QC851-999Instruments and techniques; Soil degassing; Volcano monitoring; GeophysicsSequential Gaussian simulationSoil co2 fluxFlux (metallurgy)Soil degassingGeomorphologygeographygeography.geographical_feature_categoryRiftlcsh:QC801-809Instruments and techniquesSettore GEO/08 - Geochimica E VulcanologiaTectonicslcsh:Geophysics. Cosmic physicsGeophysicsVolcanoLinosaSoil CO_2 fluxlcsh:Meteorology. ClimatologyGeologyChannel (geography)
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