Search results for " CRA"

showing 10 items of 611 documents

Unmanned aerial vehicle measurements of volcanic carbon dioxide fluxes

2008

[i] We report the first measurements of volcanic gases with an unmanned aerial vehicle (UAV). The data were collected at La Fossa crater, Vulcano, Italy, during April 2007, with a helicopter UAV of 3 kg payload, carrying an ultraviolet spectrometer for remotely sensing the SO 2 flux (8.5 Mg d- 1 ), and an infrared spectrometer, and electrochemical sensor assembly for measuring the plume CO 2 /SO 2 ratio; by multiplying these data we compute a CO 2 flux of 170 Mg d -1 . Given the deeper exsolution of carbon dioxide from magma, and its lower solubility in hydro-thermal systems, relative to SO 2 , the ability to remotely measure CO 2 fluxes is significant, with promise to provide more profound…

event.disaster_typegeographygeography.geographical_feature_categorySpectrometerMeteorologyAtmospheric sciencesPlumeSettore GEO/08 - Geochimica E VulcanologiaVolcanic GasesGeophysicsFlux (metallurgy)Impact craterVolcanoMagmaPanacheGeneral Earth and Planetary Scienceseventvolcano monitoring unmanned aerial vehicles volcanic gas monitoringGeology
researchProduct

Gas hazard assessment at the Monticchio crater lakes of Mt. Vulture, a volcano in Southern Italy

2009

Geochemical investigations have shown that there is a considerable inflow of gas into both crater lakes of Monticchio, Southern Italy. These lakes are located in two maars that formed 140 000 years ago during Mt. Vulture volcanos last eruptive activity. Isotopic analyses suggest that CO2 and helium are of magmatic origin; the latter displays 3 He ⁄ 4 He isotope ratios similar to those measured in olivines of the maar ejecta. In spite of the fact that the amount of dissolved gases in the water is less than that found in Lake Nyos (Cameroon), both the results obtained and the historical reports studied indicate that these crater lakes could be highly hazardous sites, even though they are loca…

event.disaster_typegeographygeography.geographical_feature_categorybiologyGeochemistryGeologyHazard analysisSettore GEO/08 - Geochimica E VulcanologiaMaarGas hazard crater lake Mt. VultureVolcanic GasesVolcanoImpact craterCrater lakebiology.animaleventEjectaGeomorphologyGeologyVultureTerra Nova
researchProduct

A fast dual boundary element method for 3D anisotropic crack problems

2009

In the present paper a fast solver for dual boundary element analysis of 3D anisotropic crack problems is formulated, implemented and tested. The fast solver is based on the use of hierarchical matrices for the representation of the collocation matrix. The admissible low rank blocks are computed by adaptive cross approximation (ACA). The performance of ACA against the accuracy of the adopted computational scheme for the evaluation of the anisotropic kernels is investigated, focusing on the balance between the kernel representation accuracy and the accuracy required for ACA. The system solution is computed by a preconditioned GMRES and the preconditioner is built exploiting the hierarchical …

fast BEM solverdual boundary element methodlarge-scale computationsanisotropic crack problemSettore ING-IND/04 - Costruzioni E Strutture Aerospaziali
researchProduct

Quantification of the depletion of ozone in the plume of Mount Etna

2015

Volcanoes are an important source of inorganic halogen species into the atmosphere. Chemical processing of these species generates oxidised, highly reactive, halogen species which catalyse considerable O3 destruction within volcanic plumes. A campaign of ground-based in situ O3, SO2 and meteorology measurements was undertaken at the summit of Mount Etna volcano in July/August 2012. At the same time, spectroscopic measurements were made of BrO and SO2 columns in the plume downwind. Depletions of ozone were seen at all in-plume measurement locations, with average O3 depletions ranging from 11–35 nmol mol−1 (15–45%). Atmospheric processing times of the plume were estimated to be between 1 and …

geographyAtmospheric ScienceOzoneBrominegeography.geographical_feature_categorychemistry.chemical_elementAtmospheric scienceslcsh:QC1-999PlumeSettore GEO/08 - Geochimica E Vulcanologialcsh:ChemistryAtmospherechemistry.chemical_compoundlcsh:QD1-999chemistryImpact craterVolcanoTRACERlcsh:PhysicsNOx
researchProduct

Magmatic Gas Composition Reveals the Source Depth of Slug-Driven Strombolian Explosive Activity

2007

Strombolian-type eruptive activity, common at many volcanoes, consists of regular explosions driven by the bursting of gas slugs that rise faster than surrounding magma. Explosion quakes associated with this activity are usually localized at shallow depth; however, where and how slugs actually form remain poorly constrained. We used spectroscopic measurements performed during both quiescent degassing and explosions on Stromboli volcano (Italy) to demonstrate that gas slugs originate from as deep as the volcano-crust interface (approximately 3 kilometers), where both structural discontinuities and differential bubble-rise speed can promote slug coalescence. The observed decoupling between de…

geographyMultidisciplinarygeography.geographical_feature_categoryMineralogyVolcanismStrombolian eruptionVolcanic rockVolcanoImpact craterGas slugIsland arcGas compositionPetrologyGeologyScience
researchProduct

Evidence of a recent input of magmatic gases into the quiescent volcanic edifice of Panarea, Aeolian Islands, Italy

2004

- Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Naples, Italy. - Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, Palermo, Italy. - Dipartimento Chimica e Fisica della Terra ed Applicazioni, Palermo, Italy.

geographyPaleontologyGeophysicsgeography.geographical_feature_categoryMediterranean seaVolcanoImpact craterGeneral Earth and Planetary SciencesAeolian processesGeologySeismologyWest mediterraneanGeophysical Research Letters
researchProduct

Volcanic and anthropogenic contribution to heavy metal content in lichens from Mt. Etna and Vulcano island (Sicily)

1998

Major and trace element concentrations were determined in two lichen species (Parmelia conspersa and Xanthoria calcicola) from the island of Vulcano and all around Mt. Etna. In both areas, the average concentrations of Al, Ca, Mg, Fe, Na, K, P and Ti are substantially greater than those of other elements. Several elements (Br, Pb, Sb, Au, Zn, Cu) resulted enriched with respect to the local substrates. The Br and Pb enrichment factors turned out to be the highest among those calculated in both areas. Data indicate that mixing between volcanic and automotive-produced particles clearly explains the range of Pb/Br shown by lichen samples. Sb is also enriched, revealing a geogenic origin at Vulc…

geographyParmeliageography.geographical_feature_categorybiologyHealth Toxicology and MutagenesisPhosphorusTrace elementchemistry.chemical_elementMineralogyGeneral MedicineToxicologybiology.organism_classificationPollutionchemistryVolcanoImpact craterEnvironmental chemistryBiomonitoringLichenChemical compositionEnvironmental Pollution
researchProduct

Detrital footprint of the Mozambique ocean: U–Pb SHRIMP and Pb evaporation zircon geochronology of metasedimentary gneisses in eastern Madagascar

2003

Abstract The southern East African Orogen is a collisional belt where the identification of major suture zones has proved elusive. In this study, we apply U–Pb isotopic techniques to date detrital zircons from a key part of the East African Orogen, analyse their possible source region and discuss how this information can help in unravelling the orogen. U–Pb sensitive high-mass resolution ion microprobe (SHRIMP) and Pb evaporation analyses of detrital zircons from metasedimentary rocks in eastern Madagascar reveal that: (1) the protoliths of many of these rocks were deposited between ∼800 and 550 Ma; and (2) these rocks are sourced from regions with rocks that date back to over 3400 Ma, with…

geographyProvenancegeography.geographical_feature_categoryDharwar CratonGondwanaPaleontologyCratonGeophysicsGeochronologySuture (geology)ProtolithGeologyEarth-Surface ProcessesZirconTectonophysics
researchProduct

Passive degassing at Nyiragongo (D.R. Congo) and Etna (Italy) volcanoes

2014

Volcanoes are well known as an impressive large natural source of trace elements into the troposphere. Etna (Italy) and Nyiragongo (D.R. Congo) are two stratovolcanoes located in different geological settings, both characterized by persistent passive degassing from their summit craters. Here, we present some results on trace element composition in volcanic plume emissions, atmospheric bulk deposition (rainwater) and their uptake by the surrounding vegetation, with the aim to compare and identify differences and similarities between these two volcanoes. Volcanic emissions were sampled by using active filter-packs for acid gases (sulfur and halogens) and specific teflon filters for particulat…

geographyTrace elementsgeography.geographical_feature_categorylcsh:QC801-809Trace elementGeochemistryMineralogyParticulatesvolcanic emissionslcsh:QC851-999Settore GEO/08 - Geochimica E VulcanologiaTroposphereAtmospherelcsh:Geophysics. Cosmic physicsGeophysicsDeposition (aerosol physics)VolcanoImpact craterrainwater biomonitoringStratovolcanolcsh:Meteorology. Climatologyvolcanic degassing trace elements biomonitoring atmospheric depositionGeology
researchProduct

High-temperature metamorphism and crustal melting at ca. 3.2 Ga in the eastern Kaapvaal craton, southern Africa

2018

Abstract The question of whether high-grade metamorphism and crustal melting in the early Archaean were associated with modern-style plate tectonics is a major issue in unravelling early Earth crustal evolution, and the eastern Kaapvaal craton has featured prominently in this debate. We discuss a major ca. 3.2 Ga tectono-magmatic-metamorphic event in the Ancient Gneiss Complex (AGC) of Swaziland, a multiply deformed medium- to high-grade terrane in the eastern Kaapvaal craton consisting of 3.66–3.20 Ga granitoid gneisses and infolded greenstone remnants, metasedimentary assemblages and mafic dykes. We report on a 3.2 Ga granulite-facies assemblage in a metagabbro of the AGC of central Swazi…

geographyUnderplatinggeography.geographical_feature_categoryP-T reconstruction010504 meteorology & atmospheric sciencesArcheanGeochemistryMetamorphismGeologyCrustKaapvaal craton010502 geochemistry & geophysicsGrey gneiss01 natural sciencesMesoarchaeanCratonZircon ageHf-Nd isotopesGeochemistry and PetrologySwazilandMaficMetamorphic faciesGeology0105 earth and related environmental sciencesTerranePrecambrian Research
researchProduct