Search results for "gass"

showing 10 items of 164 documents

Trasmissione del calore nei letti fluidizzati con gas sino a medie temperature

2007

fluido di sostegno gassosoSettore ING-IND/10 - Fisica Tecnica Industrialetrasmissione del caloreLetti fluidizzati
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Volcanic gas monitoring of quiescent volcanoes using permanent Multi-GAS networks

2014

The Multi-component Gas Analyzer System (Multi-GAS) has recently consolidated as a standard technique for the nearly real-time in-situ observation of major volcanogenic components (H2O, CO2, SO2, H2S,H2) in volcanic gas plumes. The Multi-GAS has been initially operated at open-vent volcanoes, where it has revealed ideal for long-term continuous observations at for instance Etna and Stromboli volcanoes in Italy, therein paving the way to the acquisition of unprecedentedly long and continuous volcanic gas time-series. We here initially review the present state of the expanding network of permanent Multi-GAS instruments, now covering about 10 volcanoes worldwide. We then specifically focus on …

gas monitoringvolcanic degassingSettore GEO/08 - Geochimica E Vulcanologia
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BVLOS UAS Operations in Highly-Turbulent Volcanic Plumes.

2020

Long-range, high-altitude Unoccupied Aerial System (UAS) operations now enable in-situ measurements of volcanic gas chemistry at globally-significant active volcanoes. However, the extreme environments encountered within volcanic plumes present significant challenges for both air frame development and in-flight control. As part of a multi-disciplinary field deployment in May 2019, we flew fixed wing UAS Beyond Visual Line of Sight (BVLOS) over Manam volcano, Papua New Guinea, to measure real-time gas concentrations within the volcanic plume. By integrating aerial gas measurements with ground- and satellite-based sensors, our aim was to collect data that would constrain the emission rate of …

gas sensingMeteorologyFlight operationslcsh:Mechanical engineering and machineryUAVBVLOSlcsh:QA75.5-76.95Volcanic GasesArtificial Intelligenceeventlcsh:TJ1-1570Original Researchevent.disaster_typeRobotics and AIgeographygeography.geographical_feature_categoryplumeTurbulenceaerial roboticManamNew guineaComputer Science ApplicationsPlumeaerial robotic Volcanic degassing aerial robotic gas sensing Manam plume UAV unmanned aircraft system (UAS) volcanovolcanoVolcanoVolcanic plumeSoftware deploymentEnvironmental scienceunmanned aircraft system (UAS)lcsh:Electronic computers. Computer scienceFrontiers in robotics and AI
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Industrial Robot Collision Handling in Harsh Environments

2014

Doktorgradsavhandling i mekatronikk, Universitetet i Agder, 2014 The focus in this thesis is on robot collision handling systems, mainly collision detection and collision avoidance for industrial robots operating in harsh environments (e.g. potentially explosive atmospheres found in the oil and gas sector). Collision detection should prevent the robot from colliding and therefore avoid a potential accident. Collision avoidance builds on the concept of collision detection and aims at enabling the robot to find a collision free path circumventing the obstacle and leading to the goal position. The work has been done in collaboration with ABB Process Automation Division with focus on applicatio…

gasskollisjonshåndteringoljekollisjonVDP::Technology: 500::Information and communication technology: 550industriroboterVDP::Social science: 200::Economics: 210::Business: 213eksplosjonsfare
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Geogenic degassing from active tectonic areas of the Balkan Peninsula

2021

During the last decades, great interest of the scientific community has been addressed to the estimation of geogenic Carbon degassing from tectonically active areas (Tamburello et al., 2018). Due to its high solubility in water, CO2 can be dissolved, transported and released to the atmosphere by groundwater. The quantity released by such process is probably of the same order of magnitude as that directly emitted from active volcanoes. The quantification of this contribution has a substantial implication for the modelling of the global atmospheric carbon cycle. The Balkan peninsula, one of the geodynamically most active regions in Europe, is characterized by intense geogenic degassing. Until…

geogenic degassing Carbon dioxide Helium Methane Balkan PeninsulaSettore GEO/08 - Geochimica E Vulcanologia
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Geochemistry and volatile content of magmas feeding explosive eruptions at Telica volcano (Nicaragua)

2017

Telica volcano, in north-west Nicaragua, is a young stratovolcano of intermediate magma composition producing frequent Vulcanian to phreatic explosive eruptions. The Telica stratigraphic record also includes examples of (pre)historic sub-Plinian activity. To refine our knowledge of this very active volcano, weanalyzedmajor element composition and volatile content of melt inclusions fromsomestratigraphically significant Telica tephra deposits. These include: (1) the Scoria Telica Superior (STS) deposit (2000 to 200 years Before Present; Volcanic Explosive Index, VEI, of 2–3) and (2) pyroclasts from the post-1970s eruptive cycle (1982; 2011). Based on measurements with nanoscale secondary ion…

geographyExplosive eruptiongeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySettore GEO/07 - Petrologia E PetrografiaPyroclastic rock010502 geochemistry & geophysics01 natural sciencesTelica Nicaragua degassingSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcanoGeochemistry and PetrologyMagmaStratovolcanoScoriaTephraGeology0105 earth and related environmental sciencesMelt inclusions
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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
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Heterogeneity of volatile sources along the Halmahera arc, Indonesia

2021

co-auteur étranger; International audience; The parallel Halmahera and Sangihe arcs in eastern Indonesia are sites of active arc-arc collision of considerable interest in developing understanding of the geodynamics and geochemistry of subduction zones. Owing to the comparative remoteness of the region, few ground-based studies of the volcanoes have been undertaken. Here, we report and integrate gas measurements and (isotope) geochemical analyses of lava samples for Dukono, Ibu, Gamkonora, Gamalama, and Makian volcanoes of the Halmahera arc. Summing gas fluxes for all five volcanoes indicates arcscale emission budgets for H 2 O, CO 2 , SO 2 , H 2 S, and H 2 of 96300±27000, 2093±450, 944±400,…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMantle wedgeSubductionLavaArc-scale degassing budget Halmahera volcanoes Sediment contribution and fluid flux Variability of arc magmaGeochemistryPartial meltingVariability of arc magmaCrustHalmahera volcanoesGeodynamics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Sediment contribution and fluid fluxGeophysicsVolcano13. Climate actionGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGeology0105 earth and related environmental sciences
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Passive vs. active degassing modes at an open-vent volcano (Stromboli, Italy)

2012

Abstract We report here on a UV-camera based field experiment performed on Stromboli volcano during 7 days in 2010 and 2011, aimed at obtaining the very first simultaneous assessment of all the different forms (passive and active) of SO 2 release from an open-vent volcano. Using the unprecedented spatial and temporal resolution of the UV camera, we obtained a 0.8 Hz record of the total SO 2 flux from Stromboli over a timeframe of ∼14 h, which ranged between 0.4 and 1.9 kg s −1 around a mean value of 0.7 kg s −1 and we concurrently derived SO 2 masses for more than 130 Strombolian explosions and 50 gas puffs. From this, we show erupted SO 2 masses have a variability of up to one order of mag…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMean valueFluxInduced seismicity010502 geochemistry & geophysics01 natural sciencesStrombolian eruptionSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyLong periodTemporal resolutionEarth and Planetary Sciences (miscellaneous)Infrared radiometervolcanic degassing Strombolian explosions puffing UV camera high time resolution SO2 fluxGeologySeismology0105 earth and related environmental sciencesEarth and Planetary Sciences Letters
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Gas geochemistry and CO2 output estimation at the island of Milos, Greece

2018

Abstract Twenty gas samples have been collected from the natural gas manifestations of Milos Island, the majority of which is found underwater along its coast. Furthermore, three anomalous degassing fumarolic areas (Kalamos, Paleochori and Adamas) have been recognized on-land. Almost all the gases are CO2-dominated with CO2 ranging from 88 to 99% vol for the samples taken underwater, while the on-land manifestations show a wider range (15–98%) due to air contamination. Methane reaches up to 1.0% vol, H2 up to 3.2% vol and H2S up to 3.5% vol indicating a hydrothermal origin of the gases. The isotope composition of He points out to mantle contributions up to 45%, while the C-isotope compositi…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesVolcanic arcStable isotope ratioGeochemistry010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationMantle (geology)MethaneSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundGeophysicsHydrothermal gases Stable isotopes Geogenic degassing Carbon dioxideVolcanochemistryGeochemistry and PetrologyCarbon dioxideGeothermal gradientGeology0105 earth and related environmental sciencesJournal of Volcanology and Geothermal Research
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