Search results for "geochemistry."

showing 10 items of 2961 documents

Noble gas geochemistry in seismic (Umbria, Italy) and volcanic (Grand Comore Island, Indian Ocean) regions: New methodologies and implications

2020

The noble gases are among the most powerful geochemical tools in different geological settings. For this reason, they represent one of the most valuable tracers of geochemical processes whose variations can be straightforwardly ascribed to magmatic/crustal dynamics. In this dissertation, noble gas (He, Ne, Ar) geochemistry applied in both seismic and volcanic regions are presented. The PhD research has firstly been devoted to the test on the field of an auto-sampler for high-frequency collection of the water samples in order to be analysed for their dissolved noble gases. Then, I developed a lab-based methodology for the in-vacuum extraction of noble gases from waters collected in the coppe…

noble gaseismically-active regionsvolcanically-active regiongeochemistrySettore GEO/08 - Geochimica E Vulcanologia
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Natural Halogen Emissions to the Atmosphere: Sources, Flux, and Environmental Impact

2022

Understanding the atmospheric geochemical cycle of both natural and anthropogenic halogens is important because of the detrimental effect halogens have on the environment, notably on tropospheric and stratospheric ozone. Oceans are the primary natural source for atmospheric Cl, F, Br, and I, but anthropogenic emissions are still important, especially for Cl. While emissions of human-made halocarbons (e.g., chlorofluorocarbons or CFCs) are expected to continue to decrease allowing progressive stratospheric ozone recovery, volcanic activity (e.g., clusters of mid-scale explosive eruptions or large-scale explosive eruptions) might disturb this recovery over the next decades. This review provid…

ozone depletionmethyl halidesvolcanic gasesGeochemistry and Petrologybrominevery-short lived substancesEarth and Planetary Sciences (miscellaneous)oceansElements
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A revision of the structure and stratigraphy of pre-Green Tuff ignimbrites at Pantelleria (Strait of Sicily)

2013

International audience; At Pantelleria, peralkaline silicic magmas were erupted across a range of eruptive typologies and magnitudes: pyroclastic flows, Plinian to strombolian pumice fallout and lava flows. In this paper we focus on the intermediate cycle of eruptive activity which is bracketed by ignimbrite units slightly older than the two caldera collapses which marked the volcanological activity of the island. This age interval (180-85 ka) was punctuated by six ignimbrite-forming eruptions (silicic and variably peralkaline) for a cumulative erupted magma volume of approximately 6 km3 dense rock equivalent. Based on new 40Ar/39Ar (Na,K)-feldspar ages and petrographic data, we propose an …

pantellerite010504 meteorology & atmospheric sciencesLava[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrySilicicPyroclastic rock010502 geochemistry & geophysics01 natural sciencesPeralkaline rock40Ar/39Ar datingGeochemistry and PetrologyPumiceperalkaline magma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderaPeralkaline magmasGeomorphology0105 earth and related environmental sciencesIgnimbritesSettore GEO/07 - Petrologia E PetrografiaStrombolian eruptionignimbriteGeophysicsDense-rock equivalentPantellerites40Ar/39Ar dating.GeologyPantelleria
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Guano-related phosphate-rich minerals in European caves

2019

International audience; Guano is a typical deposit found in caves derived from the excretions of bats and in minor cases of birds. These organic deposits decompose and form a series of acid fluids and gases that can interact with the minerals, sediments, and rocks present in the cave. Over sixty phosphates are known and described from caves, but guano decay also often leads to the formation of nitrates and sulfates. In this study twenty-two European caves were investigated for their guano-related secondary minerals. Using various analytical techniques, seventeen phosphates, along with one sulfate (gypsum), were recognized as secondary products of guano decay. Among those minerals, some are …

phosphatesGypsum010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistrybat guanocave minerals phosphate bat guanoengineering.material010502 geochemistry & geophysics01 natural sciencessecondary cave mineralsApatitechemistry.chemical_compoundCavesecondary cave minerals phosphates minerogenesis limestone caves bat guanominerogenesisBiology (General)Sulfatelimestone cavephosphate0105 earth and related environmental sciencesEarth-Surface Processescave mineralsQE1-996.5geographygeography.geographical_feature_categoryMineralSettore GEO/07 - Petrologia E PetrografiaGeology15. Life on landPhosphatehumanitiessecondary cave mineralchemistryminerogenesivisual_artlimestone cavesGuanoengineeringvisual_art.visual_art_mediumPyrite[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Raman Investigations to Identify Corallium rubrum in Iron Age Jewelry and Ornaments

2016

International audience; During the Central European Iron Age, more specifically between 600 and 100 BC, red precious corals (Corallium rubrum) became very popular in many regions, often associated with the so-called (early) Celts. Red corals are ideally suited to investigate several key questions of Iron Age research, like trade patterns or social and economic structures. While it is fairly easy to distinguish modern C. rubrum from bone, ivory or shells, archaeologists are confronted with ancient, hence altered, artifacts. Due to ageing processes, archaeological corals lose their intensive red color and shiny surface and can easily be confused with these other light colored materials. We pr…

polyeneslcsh:QE351-399.2[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryDistribution networks02 engineering and technologyBiology010502 geochemistry & geophysics01 natural sciencescorals; shells; Raman spectroscopy; biogenic carbonates; carotenoids; polyenes; color fading; material degradation; archaeology[CHIM.ANAL]Chemical Sciences/Analytical chemistryArchaeological researchMaterial DegradationCorallium rubrumcoral0105 earth and related environmental sciencesmaterial degradationlcsh:MineralogyEcologycarotenoidscolor fadingGeologyOrnamentsarchaeology021001 nanoscience & nanotechnologyGeotechnical Engineering and Engineering Geologybiogenic carbonatesshellscoralsIron AgeRaman spectroscopy0210 nano-technology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyMinerals
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Crystal field and magnetism with Wannier functions: Rare-earth doped aluminum garnets

2015

Using the recently developed method we calculate the crystal field parameters in yttrium and lutetium aluminum garnets doped with seven trivalent Kramers rare-earth ions. We then insert calculated parameters into the atomic-like Hamiltonian taking into account the electron-electron, spin-orbit and Zeeman interactions and determine the multiplet splitting by the crystal field as well as magnetic $\hat{g}$ tensors. We compare calculated results with available experimental data.

rare earthsWannier functionZeeman effectStrongly Correlated Electrons (cond-mat.str-el)Condensed matter physicsMagnetismab initio calculationsFOS: Physical scienceschemistry.chemical_elementGeneral ChemistryYttriumLutetiumIongarnetssymbols.namesakeCondensed Matter::Materials ScienceCondensed Matter - Strongly Correlated ElectronschemistryGeochemistry and PetrologysymbolsCondensed Matter::Strongly Correlated ElectronsHamiltonian (quantum mechanics)crystal fieldMultiplet
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The crater lake of Ilamatepec (Santa Ana) volcano, El Salvador: insights into lake gas composition and implications for monitoring

2019

We here present the first chemical characterization of the volcanic gas plume issuing from the Santa Ana crater lake, a hyper-acidic crater lake (pH of − 0.2 to 2.5) in north-western El Salvador. Our results, obtained during regular surveys in 2017 and 2018 using a Multi-GAS instrument, demonstrate a hydrous gas composition (H2O/SO2 ratios from 32 to 205) and SO2 as the main sulfur species (H2S/SO2 = 0.03–0.1). We also find that gas composition evolved during our investigated period, with the CO2/SO2 ratio decreasing by one order of magnitude from March 2017 (37.2 ± 9.7) to November 2018 (< 3). This compositional evolution toward more magmatic (SO2-rich) compositions is interpreted in the c…

ratio010504 meteorology & atmospheric sciences/SOGeochemistry2FluxContext (language use)010502 geochemistry & geophysics01 natural sciencesVolcanic gas plumeGeochemistry and PetrologyCrater lakeWet volcanoGas compositionPrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryPlumeSanta Ana volcanoCOVolcanoVolume (thermodynamics)Crater lakeGas scrubbingGeologyMulti-GAS
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KOSMOS 2017 Peru Side Experiment: nutrients, phytoplankton abundances, enzyme rates, photophysiology

2022

This data was collected during an short-term incubation experiment in March 2017 that investigated the response of a surface plankton community to upwelling. This experiment was carried in the framework of the SFB754-funded KOSMOS mesocosm study that took place in La Punta, Callao, Peru between February-April 2017. A total of six different treatments were used to disentangle chemical and biological characteristics of deep water that influence surface plankton blooms: 2 different deep water sources with different nutrient concentrations; 3 treatments to distinguish the effects of inorganic nutrients, organic nutrients and deep water microbial populations. Measured variables include inorganic…

ratioDay of experimentSFB754colored dissolved organic matter at 325 nmNitriteChlorophyll aAbsorption coefficient colored dissolved organic matter at 254 nmClimate - Biogeochemistry Interactions in the Tropical Ocean (SFB754)colorimetric determinationFluorometerFluorometricNitrateNanoplanktonPhytoplankton cells phycocyanin-containing (FL-4)PicoeukaryotesFluorometer fast repetition rateCalculatedFlow cytometryNutrient consumption ratioforward scatterSynechococcusupwelling systemsMesocosm experimentSpectrophotometricClimate Biogeochemistry Interactions in the Tropical Ocean SFB754SilicateBiogeochemistryBiospheric SciencesMaximum photochemical quantum yield of photosystem IIenzyme activitycell sizeDissolved inorganic nitrogen/dissolved inorganic phosphorus ratioKOSMOS_2017chainsAbsorption coefficient colored dissolved organic matter 250 nm/365 nm ratioeastern tropical South Pacific OceanKOSMOSExcess phosphateAbsorption coefficient colored dissolved organic matter at 325 nmNatural SciencesGeosciencescolored dissolved organic matter at 254 nmphycocyanin containing FL 4Absorption coefficientPhosphateTank numberPhytoplankton cells chainsNetwork of Leading European AQUAtic MesoCOSM Facilities Connecting Mountains to Oceans from the ArctReplicatenutrientsfast repetition rateDATE TIMECryptophytesMicrophytoplanktonPhytoplankton cellsLeucine aminopeptidase activityDissolved inorganic nitrogen dissolved inorganic phosphorus ratiofungiEnzymatic assayContinuous flow analyserTreatmentDATE/TIMEcolored dissolved organic matter 250 nm 365 nmPhytoplanktonPhytoplankton cell size forward scatterNetwork of Leading European AQUAtic MesoCOSM Facilities Connecting Mountains to Oceans from the Arctic to the Mediterranean (AQUACOSM)CDOMContinuous flow analyser colorimetric determinationNitrate and Nitrite
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Investigation of a Gravel-Bed River’s Pattern Changes: Insights from Satellite Images

2021

Changes in river pattern have been documented in the literature. The recognition of islands and vegetated patches, which is indicative of the evolution processes, requires simultaneous information at different points and at different times and field studies are still difficult and scarce. The present work, focusing the attention on a gravel-bed river, explores the possibility to conduct a first-step pattern changes analysis by identifying the evolution of the morphological features and taking information of islands and vegetated patches from satellite images easily available from Google Earth. The study is conducted by combining the information taken from both the satellite images and the f…

river pattern010504 meteorology & atmospheric sciencesriverFlow (psychology)Flux010502 geochemistry & geophysicslcsh:Technology01 natural sciencesDeposition (geology)Settore ICAR/01 - Idraulicalcsh:ChemistryGeneral Materials Sciencelcsh:QH301-705.5Instrumentation0105 earth and related environmental sciencesFluid Flow and Transfer Processeslcsh:TProcess Chemistry and TechnologyGeneral EngineeringSedimentvegetated patcheVegetationpredictionlcsh:QC1-999Field (geography)Computer Science Applicationsimagesmonitoringlcsh:Biology (General)lcsh:QD1-999lcsh:TA1-2040morphological evolutionSatellitePhysical geographylcsh:Engineering (General). Civil engineering (General)Sediment transportlcsh:PhysicsGeologyApplied Sciences
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Fosildiagénesis del anélido Rotularia spirulaea (Lamarck, 1818) (Polychaeta, Serpulidae) en el Eoceno del dominio pirenaico occidental

2018

The presence of the fossil polychaete Rotularia spirulaea (Lamarck, 1818) in Eocene deposits (middle Lutecian – upper Bartonian and (?) Priabonian) belonging to the western Pyrenean Domain is verified. In this paper, a fossildiagenetic study has been carried out. Fossils from three areas, corresponding to diff erent depositional settings, have been analysed. In area 1, sediments of the Ardanatz Sandstone and Ilundain Marls formations [Pamplona Basin and adjoining areas (Navarre)], were sampled. Here, the specimens of R. spirulaea  were not substantially affected by taphonomic reworking and the original microstructure of the carbonate tube is preserved. The test consists of a thick external …

rotularia spirulaea morphology fossildiagenesis paleogene pyrenees.CalciteRotulariafood.ingredientbiologyOutcropGeochemistryPaleontologybiology.organism_classificationQE701-760DiagenesisSedimentary depositional environmentForaminiferachemistry.chemical_compoundfoodchemistryMarlCarbonateGeologySpanish Journal of Palaeontology
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