Search results for "Vulcan"

showing 10 items of 510 documents

Geochemical characteristics of waters in mineralised area of Peloritani Mountains (Sicily, Italy)

2009

Abstract This paper presents the results of a study on the geochemistry of waters circulating in the mineralised area of the south-eastern sector of Mt. Peloritani (north-eastern Sicily, Italy), aimed at basic understanding of the geochemical processes influencing their chemical composition. Chemico-physical parameters and data on 26 major and minor chemical elements are reported for 103 water samples. Water chemistry is mainly dominated by dissolution of carbonates and hydrolysis of aluminosilicate minerals. Total dissolved salts (TDS) range from 80 to 1398 mg/L. All the waters exhibit E H characteristic of an oxygenated environment. Excluding two samples, which show very high H + activity…

ChemistryDolomiteCarbonate mineralsGeochemistryTrace elementWeatheringPollutionSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundmineralised area trace elements hydrogeochemistryGeochemistry and PetrologyEnvironmental ChemistryKaoliniteCarbonateClay mineralsChemical compositionApplied Geochemistry
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Sicilian bottled natural waters: Major and trace inorganic components

2013

Sixteen bottled waters of various Sicilian brands, 11 natural mineral waters and five normal drinking waters, were analyzed for major and trace inorganic components by ion chromatography (IC) and inductively coupled plasma-mass spectrometry (ICP-MS), respectively. The bottled waters represent a variety of water types with significantly different compositions in terms of salinity, major components and trace elements. Chemically, they range from Ca–HCO3 and Ca–SO4 to Na–HCO3 types. Total dissolved solids ranges from 54 to 433 mg/L, total hardness from 25 to 238 mg/L CaCO3, and measured Na content from 5.7 to 57 mg/L. According to total dissolved ions, all the bottled waters were classified as…

ChemistryIon chromatographyBottled waterMass spectrometryTotal dissolved solidsPollutionSettore GEO/08 - Geochimica E VulcanologiaSalinityNutrientGeochemistry and PetrologyEnvironmental chemistryEnvironmental ChemistryWater qualitybottled natural waters major and trace elements municipal watersChemical compositionApplied Geochemistry
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Environmental RNA outperforms eDNA metabarcoding in assessing impact of marine pollution: A chromium-spiked mesocosm test

2022

Environmental (e)DNA metabarcoding holds great promise for biomonitoring and ecotoxicological applications. However, few studies have compared the performance of eDNA versus eRNA metabarcoding in assessing organismal response to marine pollution, in experimental conditions. Here, we performed a chromium (Cr)-spiked mesocosm experimental test on benthic foraminiferal community to investigate the effects on species diversity by analysing both eDNA and eRNA metabarcoding data across different Cr concentrations in the sediment. Foraminiferal diversity in the eRNA data showed a significant negative correlation with the Cr concentration in the sediment, while a positive response was observed in t…

ChromiumEnvironmental EngineeringHealth Toxicology and MutagenesisPublic Health Environmental and Occupational HealtheRNAGeneral MedicineGeneral ChemistryForaminiferaMesocosmBiodiversitySettore GEO/01 - Paleontologia E PaleoecologiaEcotoxicologyPollutionSettore GEO/08 - Geochimica E VulcanologiaMetabarcodingEnvironmental ChemistryDNA Barcoding TaxonomicRNAeDNAEcosystemEnvironmental Monitoring
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Post-fragmentation vesiculation timescales in hydrous rhyolitic bombs from Chaitén volcano

2020

Abstract Bubble nucleation and growth dynamics exert a primary control on the explosivity of volcanic eruptions. Numerous theoretical and experimental studies aim to capture the complex process of melt vesiculation, whereas textural studies use vesicle populations to reconstruct magma behaviour. However, post-fragmentation vesiculation in rhyolitic bombs can create final quenched bubble (vesicle) textures that are not representative of the nature of fragmenting magma within the conduit. To examine bubble growth in hydrous rhyolitic bombs, we have used heated stage microscopy to directly observe vesiculation of a Chaiten rhyolite melt (with an initial dissolved water content of ~0.95 wt %) a…

Coalescence (physics)010506 paleontologyVulcanian eruptionBubbleClose-packing of equal spheresGeologyVolcanic explosivity index010502 geochemistry & geophysics01 natural sciencesRhyoliteGrowth ratePetrologyVolcanic bombGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of South American Earth Sciences
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Constructive Optimization of Vulcanization Installations in Order to Improve the Performance of Conveyor Belts

2019

Conveyor belts of special importance must have superior mechanical characteristics. The joining by vulcanization of the conveyor belts allows to obtain superior performances, but it has been found that at the vulcanizing joint of the conveyor belts, there is a &ldquo

Computer science020209 energyfinite element methodMechanical engineering02 engineering and technologylcsh:TechnologyConstructiveArticlelaw.inventionconstructive optimizationjointingNatural rubberlaw0502 economics and business0202 electrical engineering electronic engineering information engineeringGeneral Materials Sciencelcsh:Microscopylcsh:QC120-168.85050210 logistics & transportationInsert (composites)lcsh:QH201-278.5lcsh:T“bell”-type defect05 social sciencesVulcanizationconveyor beltsFinite element methodStiffeninglcsh:TA1-2040visual_artvisual_art.visual_art_mediumlcsh:Descriptive and experimental mechanicslcsh:Electrical engineering. Electronics. Nuclear engineeringlcsh:Engineering (General). Civil engineering (General)lcsh:TK1-9971Materials
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Estudio Hidrogeoquimico De Las Áreas Termales Del Complejo Volcánico Copahue-Caviahue

2016

Hydrogeochemical study on Thermal areas of the Copahue-Caviahue Volcanic Complex The hydrothermal system hosted in the Copahue- Caviahue Volcanic Complex consists of different geothermal areas around the Copahue volcano, whose last eruptive cycle started on December 22 of 2012. This work presents new data from the samplings of November 2012 and march 2013 in Las Maquinas, Las Maquinitas, villa de Copahue and Chancho-Có areas. These acid-sulfate and steam heated waters, presented changes in their SO4-2 concentrations, especially in Las Maquinas and Las Maquinitas areas. Meanwhile, SO4-2/Cl- ratios presented a strong decrease in the samples from November 2012, regarding the samples from 2013.…

Copahue volcano hydrothermal system water geochemistry REE volcano riskSettore GEO/08 - Geochimica E Vulcanologia
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Fluorine adsorption by volcanic soils at Mt. Etna, Italy

2012

Abstract Fluorine adsorption experiments were performed on 28 samples of the first 5 cm of topsoil collected on the flanks of Mt. Etna. The soil samples were equilibrated with F-rich rainwater (3.25 mg/L) at a soil/water weight ratio of 1/25. Aliquots of the supernatant were collected after 1, 7, 72, 720 and 5640 h and analysed for F content. The soil samples could be subdivided into three groups based on their F-adsorption behaviours after 1 h and at the end of the experiment: (1) negative adsorption (F released from the soil to the solution) after 1 h and negative or moderately positive adsorption at the end, (2) from negative after 1 h to strongly positive adsorption at the end, and (3) …

DESORPTIONTopsoilSoil testDRINKING-WATERNEW-ZEALANDSoil scienceSiltSORPTIONATMOSPHEREPollutionSettore GEO/08 - Geochimica E VulcanologiaAdsorptionMOBILITYGeochemistry and PetrologySoil pHACIDSoil waterALLOPHANEEnvironmental ChemistryDEPOSITIONAllophaneERUPTIONGroundwaterGeologyApplied Geochemistry
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Development and application of active and passive DOAS instrumentation for the remote sensing measurement of volcanic gas emissions and continuous ge…

2011

DOASdegassing volcanoevolcanic gaSettore GEO/08 - Geochimica E Vulcanologia
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The CO2 output from the Sperchios Basin area (central Greece): the role of hidden degassing from streams

2018

The Sperchios Basin is an actively spreading rift area with deeply rooted extensional faults and also a site of quaternary volcanic activity. Such geologic conditions favoured the formation of many hydrothermal systems, whose surface expressions are among the biggest thermal springs of the whole Greece. Degassing of deeply derived geogenic CO2 is highlighted by strong bubbling within the main pools of the springs. Flux measurements were made in the Thermopyles spring with the floating chamber method and results showed that bubbling gases in the spring release about 1 ton/day of CO2. The outgoing stream has a flow of more than 250 l/s of water rich in CO2 (about 16 mmol/l). Although no bubbl…

Degassing Greece gas manifestions Carbon dioxideSettore GEO/08 - Geochimica E Vulcanologia
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Active alkaline traps to determine acidic-gas ratios in volcanic plumes: Sampling techniques and analytical methods

2014

In situ measurements have been the basis for monitoring volcanic gas emissions for many years and—being complemented by remote sensing techniques—still play an important role to date. Con- cerning in situ techniques for sampling a dilute plume, an increase in accuracy and a reduction of detection limits are still necessary for most gases (e.g., CO2, SO2, HCl, HF, HBr, HI). In this work, the Raschig-Tube tech- nique (RT) is modified and utilized for application on volcanic plumes. The theoretical and experimental absorption properties of the RT and the Drechsel bottle (DB) setups are characterized and both are applied simultaneously to the well-established Filter packs technique (FP) in the …

Detection limitgeographyAnalytegeography.geographical_feature_categoryalkaline traps plume sampling sulfur and halogen Etna volcanoDifferential optical absorption spectroscopyIon chromatographyMineralogySettore GEO/08 - Geochimica E VulcanologiaPlumeGeophysicsVolcanoGeochemistry and PetrologyAbsorption (electromagnetic radiation)Inductively coupled plasma mass spectrometryGeologyGeochemistry, Geophysics, Geosystems
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