Search results for "S.E.M."

showing 10 items of 5492 documents

Chronospeciation of uranium released in soil during a long-term DU shell weathering experiment.

2021

Corrosion process was investigated of depleted uranium (DU) ammunition fragments buried for three years in aerobic soils continuously irrigated with water. The continuing corrosion process was triggered through formation of soluble uranyl oxyhydrate phases such as metaschoepite and becquerelite, which were identified by micro-Raman and X-ray diffraction spectroscopy. The soil was not amended by phosphates and, therefore, no uranyl phosphates were found as corrosion products on the DU surfaces by X-ray photoelectron spectroscopy. A speciation modelling at high temporal sequence (chronospeciation approach) indicated that the abundant Fe oxyhydroxides in the soil immobilized the U(IV) released…

010504 meteorology & atmospheric sciencesHealth Toxicology and Mutagenesischemistry.chemical_elementWeathering010501 environmental sciences01 natural sciencesCorrosionFerrihydritechemistry.chemical_compoundPore water pressureSoilRadiation MonitoringEnvironmental ChemistrySoil Pollutants RadioactiveWaste Management and Disposal0105 earth and related environmental sciencesTotal organic carbonGeneral MedicineUraniumUranylPollutionCorrosionchemistryEnvironmental chemistrySoil waterUraniumJournal of environmental radioactivity
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Shallow vent architecture during hybrid explosive-effusive activity at Cordón Caulle (Chile, 2011-12): Evidence from direct observations and pyroclas…

2013

International audience; In June 2011, an eruption of rhyolite magma began at the Puyehue-Cordón Caulle volcanic complex, southern Chile. By January 2012, explosive activity had declined from sustained pyroclastic (Plinian to sub-Plinian) fountaining to mixed gas and ash jetting punctuated by Vulcanian blasts. This explosive activity was accompanied by synchronous effusion of obsidian lava in a hybrid explosive-effusive eruption. Fortuitous climatic conditions permitted ground-based observation and video recording of transient vent dynamics as well as real-time collection of proximal juvenile ash as it sedimented from the active plume. The main eruptive vent complex and site of lava effusion…

010504 meteorology & atmospheric sciencesLava[SDE.MCG]Environmental Sciences/Global ChangesSilicicPyroclastic rockMineralogyrhyolite010502 geochemistry & geophysics01 natural sciencestube pumiceobsidianGeochemistry and PetrologyPuyehue-Cordón CaulleRhyolite[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyTephraPetrology0105 earth and related environmental sciencesgeographyVulcanian eruptiongeography.geographical_feature_categoryPeléan eruptionexplosive-effusive transitionGeophysicsVolcanopermeabilityGeologyVulcanian
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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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Comparison of SMOS and SMAP soil moisture retrieval approaches using tower-based radiometer data over a vineyard field

2014

International audience; The objective of this study was to compare several approaches to soil moisture (SM) retrieval using l-band microwave radiometry. The comparison was based on a brightness temperature (TB) data set acquired since 2010 by the L-band radiometer ELBARA-II over a vineyard field at the Valencia Anchor Station (VAS) site. ELBARA-II, provided by the European Space Agency (ESA) within the scientific program of the SMOS (Soil Moisture and Ocean Salinity) mission, measures multiangular TB data at horizontal and vertical polarization for a range of incidence angles (30°–60°). Based on a three year data set (2010–2012), several SM retrieval approaches developed for spaceborne miss…

010504 meteorology & atmospheric sciencesMean squared errorMeteorology[SDE.MCG]Environmental Sciences/Global Changes0211 other engineering and technologiesSoil Science02 engineering and technologyAstrophysics::Cosmology and Extragalactic Astrophysics01 natural sciencesPhysics::Geophysics14. Life underwaterComputers in Earth SciencesTime series021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingAtmospheric soundingValencia Anchor StationRadiometerGeologyInversion (meteorology)SMAP15. Life on landBrightness temperatureSoil waterEnvironmental scienceRadiometrySoil moisture retrievalELBARA[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processingSMOSRemote Sensing of Environment
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Phanerozoic geological evolution of Northern and Central Africa: An overview.

2005

61 pages; International audience; The principal paleogeographic characteristics of North and Central Africa during the Paleozoic were the permanency of large exposed lands over central Africa, surrounded by northerly and northwesterly dipping pediplanes episodically flooded by epicontinental seas related to the Paleotethys Ocean. The intra-continental Congo–Zaire Basin was also a long-lived feature, as well as the Somali Basin from Late Carboniferous times, in conjunction with the development of the Karoo basins of southern Africa. This configuration, in combination with eustatic sea-level fluctuations, had a strong influence on facies distributions. Significant transgressions occurred duri…

010504 meteorology & atmospheric sciencesPaleozoicPhanerozoicInversion (geology)Northeastern Africa010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesDevonianPaleontologyPassive margin[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg14. Life underwaterNorthern AfricaWestern Africa0105 earth and related environmental sciencesEarth-Surface Processes[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsgeographyNeotethysgeography.geographical_feature_categoryRiftCentral AfricaRiftingArabiaTectonicsInversionMagmatismGeologyOrogeny[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsCraton13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPaleogeographyOrdovicianPaleotethysGeology
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Applying the USLE Family of Models at the Sparacia (South Italy) Experimental Site

2016

Soil erosion is a key process to understand the land degradation, and modelling of soil erosion will help to understand the process and to foresee its impacts. The applicability of the Universal Soil Loss Equation (USLE) at event scale is affected by the fact that USLE rainfall erosivity factor does not take into account runoff explicitly. USLE-M and USLE-MM, including the effect of runoff in the event rainfall– runoff erosivity factor, are characterized by a better capacity to predict event soil loss. The specific objectives of this paper were (i) to determine the suitable parameterization of USLE, USLE-M and USLE-MM by using the dataseries of Sparacia experimental site and (ii) to evaluat…

010504 meteorology & atmospheric sciencesScale (ratio)Soil ScienceSoil scienceDevelopment01 natural sciencesDeposition (geology)Soil lossplot soil loUSLE-MMSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental Chemistry0105 earth and related environmental sciencesGeneral Environmental ScienceEvent (probability theory)Hydrologysoil erosionSediment04 agricultural and veterinary sciencesUniversal Soil Loss Equation040103 agronomy & agricultureLand degradationUSLE-M0401 agriculture forestry and fisheriesEnvironmental scienceSurface runoffEvent scaleLand Degradation & Development
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Geodynamic control on carbonate diagenesis: Petrographic and isotopic investigation of the Upper Jurassic formations of the Paris Basin (France).

2007

23 pages; International audience; The Oxfordian and Kimmeridgian carbonates of the eastern edge of the Paris Basin display poor reservoir properties (Φb15% and Kb0.1 md). The petrographic investigation and the resultant paragenetic sequence show that this is due to extensive precipitation of 2 types of almost synchronous blocky LMC (Low Magnesian Calcite) cements during mesogenesis (burial). Stable isotope investigation of these non-recrystallized cements, through both microdrilling sampling and in-situ SIMS (Secondary IonMass Spectrometry) analysis, shows that they originated from slightly buffered meteoric fluids (−3‰SMOW to −8‰SMOW) flowing through the Malm carbonate aquifers of the east…

010504 meteorology & atmospheric sciencesStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCarbonates010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyBasin evolution01 natural sciencesUnconformityDiagenesisPetrographyPaleontologychemistry.chemical_compoundUnconformities[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryLower Cretaceous0105 earth and related environmental sciencesStable isotopesgeographygeography.geographical_feature_categoryGeologyMassif[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesDenudationchemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMeteoric waterCarbonateGeology
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Black shale deposition during Toarcian super-greenhouse driven by sea level

2013

Abstract. One of the most elusive aspects of the Toarcian oceanic anoxic event (T-OAE) is the paradox between carbon isotopes that indicate intense global primary productivity and organic carbon burial at a global scale, and the delayed expression of anoxia in Europe. During the earliest Toarcian, no black shales were deposited in the European epicontinental seaways, and most organic carbon enrichment of the sediments postdated the end of the overarching positive trend in the carbon isotopes that characterises the T-OAE. In the present study, we have attempted to establish a sequence stratigraphic framework for Early Toarcian deposits recovered from a core drilled in the Paris Basin using a…

010504 meteorology & atmospheric sciencesStratigraphylcsh:Environmental protection[SDE.MCG]Environmental Sciences/Global ChangesGeochemistry010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyWater columnlcsh:Environmental pollution[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySequence stratigraphylcsh:TD169-171.8Earth ScienceSea levellcsh:Environmental sciences0105 earth and related environmental sciencesTotal organic carbonlcsh:GE1-350Global and Planetary ChangePaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryAnoxic waters[ SDE.MCG ] Environmental Sciences/Global ChangesIsotopes of carbon13. Climate action[SDU]Sciences of the Universe [physics][SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphylcsh:TD172-193.5Enhanced weatheringOil shaleGeology
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Soil erosion processes in European vineyards: A qualitative comparison of rainfall simulation measurements in Germany, Spain and France

2016

Small portable rainfall simulators are considered a useful tool to analyze soil erosion processes in cultivated lands. European research groups in Spain (Valencia, Málaga, Lleida, Madrid and La Rioja), France (Reims) and Germany (Trier) have used different rainfall simulators (varying in drop size distribution and fall velocities, kinetic energy, plot forms and sizes, and field of application) to study soil loss, surface flow, runoff and infiltration coefficients in different experimental plots (Valencia, Montes de Málaga, Penedès, Campo Real and La Rioja in Spain, Champagne in France and Mosel-Ruwer valley in Germany). The measurements and experiments developed by these research teams give…

010504 meteorology & atmospheric sciencesWater en Landgebruiksoil hydrologyOceanography01 natural sciencesRUISSELLEMENTSoilvineyardsBodemSoil Water and Land UseQualitative comparisonlcsh:ScienceWaste Management and DisposalWater Science and Technology2. Zero hungerSoil classification04 agricultural and veterinary sciencesqualitative comparisonPE&RCInfiltration (hydrology)INFILTRATIONERODIBILITE DU SOLPRECIPITATIONErosionWEPPSIMULATION DE PLUIESoil hydrologyEAU DU SOLSoil scienceVIGNESoil lossETUDE COMPARATIVE[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology0105 earth and related environmental sciencesEarth-Surface ProcessesTerroirHydrologysoil erosionWater and Land UseTERRE CULTIVABLEECOULEMENT DE SURFACErainfall simulation15. Life on landBodemfysica en LandbeheerVineyardsRainfall simulationBodem Water en LandgebruikSoil Physics and Land Managementrainfall simulation; soil erosion; soil hydrology; qualitative comparison; vineyardsrainfall simulation soil erosion soil hydrology qualitative comparison vineyards040103 agronomy & agricultureRainfall simulationSoil erosion0401 agriculture forestry and fisheriesEnvironmental sciencelcsh:QSurface runoffMETHODOLOGIE
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Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the co…

2013

11 pages; International audience; The Neodymium(Nd) isotope composition of fish remains has beenwidely used to track past changes in oceanic circulation. Although the number of published Nd isotope data for the Cretaceous has markedly increased in the last years, no consensus has been reached on the structure of the oceanic circulation and its evolution during the Late Cretaceous. Yet this period is characterised bymajor geodynamical and climatic changes andmarked by the disappearance of global oceanic anoxic events inwhich changes in oceanic circulation modesmay have played a significant role. In this study we present the first record of Nd isotopic composition of fish remains from contine…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousIsotopic signaturePaleontologyContinental marginJapanGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryoceanic circulation14. Life underwater[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesRadiogenic nuclide[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySeafloor spreadingCretaceous[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPeriod (geology)Seawaterneodymium isotopesGeology
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