Search results for " geochimica"

showing 10 items of 446 documents

The key role played by the Augusta basin (southern Italy) in the mercury contamination of the Mediterranean Sea.

2011

The Augusta basin, located in SE Sicily (southern Italy), is a semi-enclosed marine area, labelled as a highly contaminated site. The release of mercury into the harbour seawater and its dispersion to the blue water, make the Augusta basin a potential source of anthropogenic pollution for the Mediterranean Sea. A mass balance was implemented to calculate the HgT budget in the Augusta basin. Results suggest that an average of ∼0.073 kmol of HgT is released, by diffusion, on a yearly basis, from sediments to the seawater, with a consequent output of 0.162 kmol y(-1) to coastal and offshore waters; this makes the Augusta area an important contributor of mercury to the Mediterranean Sea. Owing …

010504 meteorology & atmospheric scienceschemistry.chemical_element010501 environmental sciencesManagement Monitoring Policy and LawStructural basin01 natural sciencesMediterranean seaOcean gyreMediterranean SeaWater Pollution ChemicalSeawater14. Life underwater0105 earth and related environmental sciencescomputer.programming_languagegeographygeography.geographical_feature_categoryPublic Health Environmental and Occupational HealthSedimentGeneral MedicineMercury6. Clean waterMercury (element)Settore GEO/08 - Geochimica E VulcanologiaOceanographychemistryHg sediment Augusta basinItaly13. Climate actionHarbourSeawaterSubmarine pipelinecomputerGeologyWater Pollutants ChemicalEnvironmental MonitoringJournal of environmental monitoring : JEM
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Mercury emissions from soils and fumaroles of Nea Kameni volcanic centre, Santorini (Greece)

2013

There have been limited studies to date targeting mercury emissions from volcanic fumarolic systems, and no mercury flux data exist for soil or fumarolic emissions at Santorini volcanic complex, Greece. We present results from the first geochemical survey of Hg and major volatile (CO2, H2S, H2O and H-2) concentrations and fluxes in the fumarolic gases released by the volcanic/hydrothermal system of Nea Kameni islet; the active volcanic center of Santorini. These data were obtained using a portable mercury spectrometer (Lumex 915+) for gaseous elemental mercury (GEM) determination, and a Multi-component Gas Analyzer System (Multi-GAS) for major volatiles. Gaseous Elemental Mercury (GEM) conc…

010504 meteorology & atmospheric sciencesvolcanogenic mercury volcanic degassing Santorini mercury flux inventory trace metalsEarth sciencetrace metalsAir pollutionchemistry.chemical_element010502 geochemistry & geophysicsmedicine.disease_cause01 natural scienceschemistry.chemical_compoundGeochemistry and Petrologymercury flux inventorymedicinevolcanogenic mercuryAir quality index0105 earth and related environmental sciencesgeographySantorinigeography.geographical_feature_categoryFumaroleSettore GEO/08 - Geochimica E VulcanologiaMercury (element)GeophysicschemistryVolcano13. Climate actionEnvironmental chemistryCarbon dioxideSoil watervolcanic degassingGeologyGEOCHEMICAL JOURNAL
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Copper supply during the Final Neolithic at the Saint-Blaise/Bains des Dames site (Neuchâtel, Switzerland)

2009

The Saint-Blaise/Bains des Dames stratified site in Neuchâtel, Switzerland, contains several occupations that span the Late through Final Neolithic, including the Horgen, Lüscherz, and Auvernier-Cordé periods. As part of a study on prehistoric metallurgy in western Switzerland, we compare the lead isotope ratios (multicollector inductively coupled plasma mass spectrometer) and elemental compositions (instrumental neutron activation analysis) of the site's numerous copper finds to a database of corresponding measurements for copper ores throughout Europe. The results show a considerable variation in copper compositions present at the site, suggesting complex economic relationships and multip…

010506 paleontologyArcheologyProvenance[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryLead isotope analysischemistry.chemical_element01 natural sciencesPrehistoryFinal Neolithic- Archeometry- Pb isotope analysis - Archeometallurgy - CopperGEO/08 - GEOCHIMICA E VULCANOLOGIA550 Earth sciences & geology0601 history and archaeologyMC-ICP-MSComputingMilieux_MISCELLANEOUSddc:599.90105 earth and related environmental sciences[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory060102 archaeologyMc icp msMetal analysisFinal Neolithic06 humanities and the artsMetal analysisArchaeologyCopperGeographychemistryAnthropologyCopper
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Influence of dissolved organic matter on rare earth elements and yttrium distributions in coastal waters

2010

International audience; Data collected during this study indicate that dissolved Y and REE (rare earth element) behaviour can be monitored through shale-normalised ratios. Relationships occurring between these ratios suggest that leaching from lithogenic materials is the main source of REE in the studied area. This process involves riverine detrital matter in the inner area of the Gulf of Palermo. Features of shale-normalised patterns and the relationship recognised between dissolved Fe and Y/Ho suggest that REE are released from Fe-rich coatings of atmospheric dust. Observed similarities between dissolved Fe and chlorophyll- content suggest that leaching of Fe-rich atmospheric particulates…

010506 paleontologyMineralogyrare earth elementsMediterranean010502 geochemistry & geophysics01 natural sciencesMediterranean seaDissolved organic carbonMediterranean Sea[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyOrganic matter14. Life underwaterScavengingEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental Sciencechemistry.chemical_classificationEcologyRare-earth elementAuthigenicParticulatesREE; Mediterranean; Ce anomalyREESettore GEO/08 - Geochimica E VulcanologiachemistryCe anomaly13. Climate actionEnvironmental chemistryGeneral Earth and Planetary SciencesSeawaterchlorophyll-YREE Ce anomaly Central Mediterranean late Quaternary Palaeoenvironmental reconstructionGeologyChemistry and Ecology
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The end of the Messinian salinity crisis: Evidences from the Chelif Basin (Algeria).

2007

How did the Messinian Salinity Crisis end is a matter of intense debate between two opposite concepts i.e., the generalised dilution event, the so-called Lago–Mare, followed by the sudden restoration of the marine conditions at the base of the Zanclean, or the early partial or complete marine refill that would have happened earlier during the upper Messinian. The Chelif Basin of Northwestern Algeria, one of the greatest Messinian marginal basins of the Mediterranean, provides an exceptional opportunity to study in detail how this major paleoenvironmental change occurred through continuous sedimentary records of the Miocene–Pliocene boundary. Five sections representative of both the central …

010506 paleontologyOstracodSettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OForaminiferaStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaPaleontologyMessinianOstracodZanclean14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyStable IsotopesMediterranean basinPaleontologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneAlgeriaClastic rockLago–MareSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyChelif basinGeologyMarine transgression
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Carbon-isotope records of the Early Jurassic (Toarcian) Oceanix Anixic Event from the Valdorbia (Umbria-Marche Apennines) and Monte Mangart (Julian A…

2009

The Toarcian oceanic anoxic event (ca 183 Ma) coincides with a global perturbation marked by enhanced organic carbon burial and a general decrease in calcium carbonate production, probably triggered by changes in the composition of marine plankton and elevated carbon dioxide levels in the atmosphere. This study is based on high-resolution sampling of two stratigraphic successions, located in Valdorbia (Umbria-Marche Apennines) and Monte Mangart (Julian Alps), Italy, which represent expressions of the Toarcian oceanic anoxic event in deep-water pelagic sediments. These successions are characterized by the occurrence of black shales showing relatively low total organic carbon concentrations (…

010506 paleontologystratigraphic correlationStratigraphy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesBiostratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontologyCarbon isotopes cyclostratigraphy Early Jurassic oceanic anoxic event stratigraphic correlation.oceanic anoxic event14. Life underwateroceanic anoxiceventComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesCarbon isotopes; cyclostratigraphy; Early Jurassic; oceanic anoxic event; stratigraphic correlationCarbon isotopes; cyclostratigraphy; Early Jurassic; oceanic anoxicevent; stratigraphic correlation.AmmoniteCarbon dioxide in Earth's atmosphereEarly JurassicCarbon isotopesGeologyPelagic sedimentCyclostratigraphyAnoxic waterslanguage.human_languageSettore GEO/08 - Geochimica E Vulcanologia13. Climate actionIsotopes of carbonlanguageSedimentary rockcyclostratigraphyGeology
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Volcanic CO2 seep geochemistry and use in understanding ocean acidification

2020

AbstractOcean acidification is one of the most dramatic effects of the massive atmospheric release of anthropogenic carbon dioxide (CO2) that has occurred since the Industrial Revolution, although its effects on marine ecosystems are not well understood. Submarine volcanic hydrothermal fields have geochemical conditions that provide opportunities to characterise the effects of elevated levels of seawater CO2 on marine life in the field. Here, we review the geochemical aspects of shallow marine CO2-rich seeps worldwide, focusing on both gas composition and water chemistry. We then describe the geochemical effects of volcanic CO2 seepage on the overlying seawater column. We also present new g…

0106 biological sciencesSettore BIO/07 - Ecologia010504 meteorology & atmospheric sciencesGeochemistryMarine life01 natural scienceschemistry.chemical_compoundAlgaeEnvironmental ChemistrySubmarine hydrothermalismMarine ecosystem0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyCalcifying speciesCarbon dioxide in Earth's atmospherebiology010604 marine biology & hydrobiologyNatural analoguesCoralline algaeOcean acidificationbiology.organism_classificationEcosystem effectsSettore GEO/08 - Geochimica E VulcanologiachemistryCarbon dioxideEnvironmental scienceSeawater
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Geochemical survey of Levante Bay, Vulcano Island (Italy), a natural laboratory for the study of ocean acidification

2013

Abstract Shallow submarine gas vents in Levante Bay, Vulcano Island (Italy), emit around 3.6t CO2 per day providing a natural laboratory for the study of biogeochemical processes related to seabed CO2 leaks and ocean acidification. The main physico-chemical parameters (T, pH and Eh) were measured at more than 70 stations with 40 seawater samples were collected for chemical analyses. The main gas vent area had high concentrations of dissolved hydrothermal gases, low pH and negative redox values all of which returned to normal seawater values at distances of about 400 m from the main vents. Much of the bay around the vents is corrosive to calcium carbonate; the north shore has a gradient in s…

0106 biological sciencesSettore BIO/07 - EcologiaBiogeochemical cycle010504 meteorology & atmospheric sciencesCarbonatesAquatic ScienceOceanography01 natural sciencesCalcium CarbonateMarine geochemistrychemistry.chemical_compoundCarbon capture and storageSeawater14. Life underwaterSeabed0105 earth and related environmental sciences010604 marine biology & hydrobiologyCarbonate saturation stateOcean acidificationOcean acidificationCarbon DioxidePollutionSettore GEO/08 - Geochimica E VulcanologiaVolcanic ventsOceanographyCalcium carbonatechemistryBaysItaly13. Climate actionCarbon dioxideCarbonateSeawaterBayGeologyWater Pollutants ChemicalEnvironmental MonitoringMarine Pollution Bulletin
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Impact on Air Quality of the COVID-19 Lockdown in the Urban Area of Palermo (Italy).

2020

At the end of 2019, the first cases of coronavirus disease (COVID-19) were reported in Wuhan, China. Thereafter, the number of infected people increased rapidly, and the outbreak turned into a national crisis, with infected individuals all over the country. The COVID-19 global pandemic produced extreme changes in human behavior that affected air quality. Human mobility and production activities decreased significantly, and many regions recorded significant reductions in air pollution. The goal of our investigation was to evaluate the impact of the COVID-19 lockdown on the concentrations of the main air pollutants in the urban area of Palermo (Italy). In this study, the trends in the average…

2019-20 coronavirus outbreak010504 meteorology & atmospheric sciencesCoronavirus disease 2019 (COVID-19)Urban PopulationHealth Toxicology and MutagenesisPneumonia ViralAir pollutionlcsh:Medicine010501 environmental sciencesUrban areamedicine.disease_cause01 natural sciencesArticleSettore BIO/01 - Botanica GeneralelockdownAir pollutantsEnvironmental healthAir PollutionmedicineHumansAir quality indexPandemics0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorylcsh:RPublic Health Environmental and Occupational HealthOutbreakCOVID-19Particulatesair qualityurban environmentCO–NO2–O3–PM10Settore GEO/08 - Geochimica E VulcanologiaAir quality COVID-19 CO–NO2–O3–PM10 Lockdown Urban environmentItalyQuarantineEnvironmental scienceCoronavirus InfectionsInternational journal of environmental research and public health
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Thermomineral waters of Greece: geochemical characterization

2020

75 °C). In terms of pH most results vary from 5.5 to 823 °C) ii) warm (23 40 °C) iii) thermal (40 75 °C) and iv) hyperthermal (&gtfew springs show either very low pH (&lt10) proposing serpentinization processes. Regarding TDS concentrations collected waters can be subdivided into low salinity (up to 1.5 g/L) brackish (up to 20 g/L) and saline (up to 43 g/L). The medium high salinities can be justified by mixing with sea water and/or strong waterrock interaction processes. Isotope composition of O and H ranges from 12.7 to +2.7 ‰ SMOW and from 91 to +12 ‰ SMOW respectively and is generally comprised between the Global Meteoric Water Line and the East Mediterranean Meteoric Water Line. Only few water samples show a positive shift for δ18O possibly related to high temperature waterrock interaction processes. Carbon dioxide (18 997000 μmol/mol) or N2 (1100 989000 μmol/mol) or CH4 (&ltMany geothermal areas of Greece are located in regions affected by Miocene or Quaternary volcanism and in continental basins characterised by elevated heat flow. Moreover the majority of them is found along the coast as well as in islands of the Aegean Sea and thus thermal water is often brackish to saline due to marine intrusion into costal aquifer. In the present study almost 300 thermal and cold mineral water samples were collected along the Hellenic territory with their physicochemical parameters (temperature pH electrical conductivity and Eh) and the amount of bicarbonates (titration with 0.1N HCl) being determined in situ. Additionally gases found either in free or dissolved phase were sampled. Both water and gas samples were analysed at the INGVPa laboratories for major ions (Ion Chromatography) silica (Inductively Coupled Plasma Optical Emission Spectrometry) chemical composition of free and dissolved gases (Gas Chromatography) water isotopes (O and H) and carbon and helium isotopes of free and dissolved gases (Mass Spectrometry). The temperature of the investigated waters ranges from 6.5 to 98°C pH from 1.96 to 11.98 whilst Total Dissolved Solids (TDS) from 0.06 to 43 g/L. Based on the temperature parameter waters can be divided into four groups: i) cold (&lt0.5 913000 μmol/mol) are the prevailing gas species found in the studied sites. The δ13CCO2 values ranged from 20.1 to +8.5 ‰ whilst the isotope ratio of He from 0.21 to 6.71 R/RA.4) suggesting interaction with H2Srich gases or very high pH values (&gtSettore GEO/08 - Geochimica E Vulcanologia
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