Search results for "FLUID"

showing 10 items of 5513 documents

Development of branching brittle and ductile shear zones: A numerical study

2017

Continental collision zones are usually associated with large-scale strike-slip shear zones. In most cases these shear zones are complex and consist of multiple strands, varying in width, length, and total displacement. Here we present 2-D numerical models to simulate the formation of such shear zones at different depth levels within the crust, under either brittle (frictional/plastic) or ductile conditions. Localization of shear zones is initiated by a material contrast (heterogeneity) of the material parameters. We systematically test the rate of strain-weakening in brittle and in ductile regimes to understand its influence on the development of shear zone networks. Our simulations sugges…

010504 meteorology & atmospheric sciencesGeometry010502 geochemistry & geophysics01 natural sciencesCondensed Matter::Soft Condensed MatterPhysics::Fluid DynamicsShear rateSimple shearStress fieldGeophysicsBrittlenessShear (geology)Geochemistry and PetrologyCritical resolved shear stressShear stressGeotechnical engineeringShear zoneGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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Collapse of a two-dimensional brittle granular column: Implications for understanding dynamic rock fragmentation in a landslide

2015

We investigate numerically the failure, collapse and flow of a two-dimensional brittle granular column over a horizontal surface. In our discrete element simulations, we consider a vertical monolayer of spherical particles that are initially held together by tensile bonds, which can be irreversibly broken during the collapse. This leads to dynamic fragmentation within the material during the flow. Compared to what happens in the case of a non-cohesive granular column, the deposit is much rougher, and the internal stratigraphic structure of the column is not preserved during the collapse. As has been observed in natural rockslides, we find that the deposit consists of large blocks laying on …

010504 meteorology & atmospheric sciencesGeometryLandslideRockslide01 natural sciences010305 fluids & plasmasEarth surfaceGeophysicsBrittlenessFragmentation (mass spectrometry)0103 physical sciencesMonolayerUltimate tensile strengthGeotechnical engineeringGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Geophysical Research: Earth Surface
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Understanding volcanoes in the Vanuatu arc

2016

We report the first helium isotope survey of volcanic gases, hot springs and some olivine phenocrysts along the Vanuatu island arc, from Tanna in the south to Vanua Lava in the north. Low CO2 content and low He-3/He-4 ratios in thermal fluids of Epi (4.0 +/- 0.1 R-a), Efate (4.5 +/- 0.1 R-a) and Pentecost (5.3 +/- 0.5 R-a) islands coherently indicate reduced mantle gas leakage and crustal contamination by radiogenic helium on these extinct volcanic systems of the former (Pliocene) arc. Instead, presently active Vanuatu volcanoes display He-3/He-4 and C/He-3 ratios typical of subduction-related volcanic arcs: He-3/He-4 ratios range from 6.4 +/- 0.5 Ra in southernmost Tanna and 7.23 +/- 0.09 …

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryVanuatu arcHelium isotopes[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesVolcanic fluidsVolcanic GasesGeochemistry and Petrologyevent0105 earth and related environmental sciencesBasaltevent.disaster_typegeographygeography.geographical_feature_categoryVolcanic arcHotspot contributionFumaroleExtinct and active volcanoesMantle sourceSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionVanuatu arc Volcanic fluids Helium isotopes Extinct and active volcanoes Mantle source Hotspot contributionIsland arcPhenocrystGeology
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The imprint of subduction fluids on subducted MORB-derived melts (Sierra del Convento Mélange, Cuba)

2011

International audience; Major and trace element signatures and Sr-Nd-Pb isotope data for muscovite (Ms)-bearing amphibolite blocks and associated muscovite-bearing trondhjemite and quartz-muscovite rocks from the Sierra del Convento melange (eastern Cuba) indicate that Proto-Caribbean oceanic crust underwent wet partial melting processes during Mesozoic subduction and after accretion to the upper plate. Trace element normalized patterns of Ms-bearing amphibolites are enriched in light rare earth elements (LREE) and large-ion lithophile elements (LILE) and evidence variable trace element transfer from the Proto-Caribbean subducting slab to the mantle wedge. Ms-bearing trondhjemites show LREE…

010504 meteorology & atmospheric sciencesMantle wedge[SDE.MCG]Environmental Sciences/Global ChangesFluid compositionTrondhjemiteGeochemistrySedimentary imprint010502 geochemistry & geophysics01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochemistry and PetrologyOceanic crust0105 earth and related environmental sciencesBasaltTrace elementsSubductionbiologyPartial meltingTrace elementGeologySr-Nd-Pb isotopesbiology.organism_classification13. Climate actionAdakiteLileGeologySlab meltsLithos
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Hydrochemical mercury distribution and air-sea exchange over the submarine hydrothermal vents off-shore Panarea Island (Aeolian arc, Tyrrhenian Sea)

2017

Abstract There is a growing concern about the mercury (Hg) vented from submarine hydrothermal fluids to the marine surrounding and exchange of dissolved gaseous mercury (DGM) between the sea surface and the atmosphere. A geochemical survey of thermal waters collected from submarine vents at Panarea Island (Aeolian Islands, southern Italy) was carried out in 2015 (15–17th June and 17–18th November), in order to investigate the concentration of Hg species in hydrothermal fluids and the vertical distribution in the overlying water column close to the submarine exhalative area. Specific sampling methods were employed by Scuba divers at five submarine vents located along the main regional tecton…

010504 meteorology & atmospheric sciencesMineralogychemistry.chemical_element010501 environmental sciencesOceanographyAir-sea exchange01 natural sciencesHydrothermal circulationWater columnEnvironmental ChemistryHydrothermal fluidMercury evasion0105 earth and related environmental sciencesWater Science and TechnologySubmarineGeneral ChemistryDissolved gaseous mercuryDilutionMercury (element)Hydrothermal fluidschemistryEnvironmental chemistryAeolian processesSeawaterDissolved gaseous mercury; Mercury evasion; Air-sea exchange; Hydrothermal fluids; Panarea IslandPanarea IslandGeologyHydrothermal ventMarine Chemistry
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Steroid Biomarkers Revisited - Improved Source Identification of Faecal Remains in Archaeological Soil Material.

2017

Steroids are used as faecal markers in environmental and in archaeological studies, because they provide insights into ancient agricultural practices and the former presence of animals. Up to now, steroid analyses could only identify and distinguish between herbivore, pig, and human faecal matter and their residues in soils and sediments. We hypothesized that a finer differentiation between faeces of different livestock animals could be achieved when the analyses of several steroids is combined (Δ5-sterols, 5α-stanols, 5β-stanols, epi-5β-stanols, stanones, and bile acids). We therefore reviewed the existing literature on various faecal steroids from livestock and humans and analysed faeces …

010504 meteorology & atmospheric sciencesPhysiologySwineSocial Scienceslcsh:MedicinePlant ScienceBreeding01 natural sciencesFecesSoilchemistry.chemical_compoundChenodeoxycholic acidMedicine and Health SciencesBilelcsh:ScienceMammalsMultidisciplinaryEcologyOrganic CompoundsGoatsAgricultureRuminantsBreedBody FluidsTrophic InteractionsCoprostanolChemistrySterolsArchaeologyCommunity EcologyPhysical SciencesVertebratesSteroidsLivestockDonkeyAnatomyResearch Article010506 paleontologyLivestockEquinesBiologyGas Chromatography-Mass SpectrometryBile Acids and SaltsGoosePlant-Animal Interactionsbiology.animalAnimalsHumansHerbivoryHorsesFeces0105 earth and related environmental sciencesHerbivorebusiness.industryPlant EcologyOrganic ChemistryEcology and Environmental Scienceslcsh:RChemical CompoundsOrganismsBiology and Life SciencesArchaeologychemistryAmnioteslcsh:QbusinessBiomarkersPLoS ONE
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Potential-vorticity dynamics of troughs and ridges within Rossby wave packets during a 40-year reanalysis period

2020

Rossby wave packets (RWPs) are fundamental to midlatitude dynamics and govern weather systems from their individual life cycles to their climatological distributions. Renewed interest in RWPs as precursors to high-impact weather events and in the context of atmospheric predictability motivates this study to revisit the dynamics of RWPs. A quantitative potential vorticity (PV) framework is employed. Based on the well established PV-thinking of midlatitude dynamics, the processes governing RWP amplitude evolution comprise group propagation of Rossby waves, baroclinic interaction, the impact of upper-tropospheric divergent flow, and direct diabatic PV modification by nonconservative processes.…

010504 meteorology & atmospheric sciencesRadiative coolingBaroclinityRossby waveContext (language use)010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesInstabilityPotential vorticityLatent heatBarotropic fluidMeteorology. ClimatologyQC851-999Geology0105 earth and related environmental sciencesWeather and Climate Dynamics
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The Graham Bank (Sicily Channel, central Mediterranean Sea). Seafloor signatures of volcanic and tectonic controls

2018

Abstract Graham Bank is a dominant physiographic element of the NW Sicily Channel (central Mediterranean Sea), affected in the last 100 years by numerous well-documented volcanic eruptions. We present the first results of a geomorphological study where the Graham Bank region in the depth interval 7–350 m was mapped for the first time with multi-beam echosounder and high-resolution seismic and multi-channel seismic reflection profiles. We describe in high resolution the detailed geomorphological features of Graham Bank, and how the superficial expression of different process and dynamics occurring in the sub-seafloor evidence volcanic and tectonic controls on seafloor morphology across a rel…

010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSeamount010502 geochemistry & geophysics01 natural sciencesFluid seepagePaleontologyMediterranean seaEcho soundingSlope instability14. Life underwater0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyFluid seepage; Graham Bank; Slope instability; Volcanic seamountgeography.geographical_feature_categoryVolcanic seamountFluid seepage Slope instability Volcanic seamount Graham BankGraham BankSeafloor spreadingTectonicsVolcanoSedimentary rockChannel (geography)Geology
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2D Hydro-Mechanical-Chemical Modeling of (De)hydration Reactions in Deforming Heterogeneous Rock: The Periclase-Brucite Model Reaction

2020

Deformation at tectonic plate boundaries involves coupling between rock deformation, fluid flow, and metamorphic reactions, but quantifying this coupling is still elusive. We present a new two-dimensional hydro-mechanical-chemical numerical model and investigate the coupling between heterogeneous rock deformation and metamorphic (de)hydration reactions. We consider linear viscous compressible and power-law viscous shear deformation. Fluid flow follows Darcy's law with a Kozeny-Carman type permeability. We consider a closed isothermal system and the reversible (de)hydration reaction: periclase and water yields brucite. Fluid pressure within a circular or elliptical inclusion is initially bel…

010504 meteorology & atmospheric sciencesShear zoneChemical process modelingMetamorphic rockThermodynamicsNumerical simulationengineering.materialDeformation (meteorology)010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsPhysics::Fluid DynamicsGeochemistry and PetrologyFluid dynamicsCoupling (piping)Brucite-Periclase reaction0105 earth and related environmental sciencesBruciteReaction-induced weakeningGeophysics13. Climate actionengineeringHydro-Mechanical-Chemical modelPericlaseShear zoneGeologyRock deformation coupled to reactions
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Evidence of active fluid seepage (AFS) in the southern region of the central Mediterranean Sea

2018

Abstract Active fluid seepage (AFS) at the seafloor is a global phenomenon associated with seafloor morphologies in different geodynamic contexts. Advanced geophysical techniques have allowed geoscientists to characterise pockmarks, mounds and flares associated with AFS. We present a range of new marine geological data acquired in the southern region of the central Mediterranean Sea (northern Sicily continental margin, northwestern Sicily Channel and offshore of the Maltese Islands), which allow us to identify AFSs. AFSs are spatially distributed as clusters, aligned or isolated at different depths, ranging from few decametres offshore of the Maltese Islands; up to 400 m offshore of norther…

010504 meteorology & atmospheric sciencesSicily ChannelSettore GEO/02 - Geologia Stratigrafica E SedimentologicaRange (biology)Settore GEO/03 - Geologia Strutturale010502 geochemistry & geophysics01 natural sciencesFluid seepagePaleontologyGas flaresMediterranean seaContinental marginElectrical and Electronic EngineeringInstrumentation0105 earth and related environmental sciencesMoundgeographyFluid seepage; Gas flares; Mound; Pockmark; Sicily Channel; Instrumentation; Electrical and Electronic Engineeringgeography.geographical_feature_categoryContinental shelfApplied MathematicsPockmarkFluid seepage; Gas flares; Mound; Pockmark; Sicily ChannelGas flareCondensed Matter PhysicsSeafloor spreadingPockmarkSubmarine pipelineGeologyChannel (geography)
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