Search results for "bepress|Physical Sciences and Mathematics|Earth Sciences"

showing 10 items of 2332 documents

Unrest at the Nevados de Chillán volcanic complex: a failed or yet to unfold magmatic eruption?

2018

Resuming erupting activity at volcanoes that have been long quiescent poses a significant challenge to hazard assessment, as it require assessment of whether the change in activity is an isolated event or the beginning of a new eruptive sequence. Such inception is often poorly characterised as quiescent volcanoes tend to be poorly equipped and not extensively monitored, especially with respect to gas geochemistry. Here, we report gas composition and flux measurements from a newly opened vent at the very onset of eruptive activity at the Nevados de Chillán volcanic complex (Chile) in January-February 2016. The molar proportions of H2O, CO2, SO2, H2S and H2 gases are found to be 98.4, 0.97, 0…

event.disaster_typeBasaltTrail By FireQE1-996.5geographygeography.geographical_feature_categoryAndesiteGeochemistryUV cameraGeologyEruption triggerDaciteVolcanic GasesBasaltic andesiteLithic fragmentVolcanoVolcanic unrestMagma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanologyevent[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentVolcanic gasesMulti-GASGeology
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The importance of fracture-healing on the deformation of fluid-filled layered systems

2014

International audience; Understanding the fracturingehealingerefracturing cycle is a fundamental part of studying the deformation dynamics and the permeability evolution of rock systems. Previous studies, however, have not examined the influence of healing i.e. fracture-closure through vein formation and the mechanical properties of the " healed " fractures (veins) on the rock deformation. We present results from a two-dimensional coupled hydro-mechanical model which simulates large time and spatial scale dynamic fracturing and healing of a porous medium under the influence of gravity, tectonic stretching and elevated fluid pressures. Our results show that healing decreases the local porosi…

fault010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph][SDU.STU]Sciences of the Universe [physics]/Earth SciencesBone healing010502 geochemistry & geophysics01 natural sciencesjointevolution[PHYS.MECA.SOLID]Physics [physics]/Mechanics [physics]/Solid mechanics [physics.class-ph]Fluid dynamicstectonicsGeotechnical engineering[PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph]PorosityElastic modulus0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsGeologyhealingPermeability (earth sciences)fracturenetwork[PHYS.COND.CM-MS]Physics [physics]/Condensed Matter [cond-mat]/Materials Science [cond-mat.mtrl-sci]Delayed fractureSaturation (chemistry)Porous mediumGeology
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Os, Sr, Nd, Pb, O isotope and trace element data from the Ferrar flood basalts, antarctica: evidence for an enriched subcontinental lithospheric sour…

1996

Os, Sr, Nd, Pb and O isotopes and trace element data are reported for basaltic andesite and andesite whole rocks and, in part, for selected mineral separates from the Jurassic Ferrar flood basalt province. Radiogenic Sr (> 0.709), unradiogenic Nd (εNd= −3 to −5), and radiogenic Pb isotopes, as well as low Nb/La ratios of 0.4 – 0.6 and Nb/La ratios between 0.45 and 0.6 are found for all rocks including our most primitive sample (Mg# = 71.9). This indicates involvement of either continental crust or enriched lithospheric mantle in magma genesis. 187Re/188Os correlates strongly with 187Os/188Os, with an age of 172 ± 5 Ma, in agreement with published Arsingle bondAr data. Initial 187Os/188Os of…

flood basalts010504 meteorology & atmospheric sciencesGeochemistryFerrar Group551010502 geochemistry & geophysics01 natural sciencesMantle (geology)magma contaminationBasaltic andesite[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/PlanetologyGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology0105 earth and related environmental sciencesgeochemistryPeridotiteBasaltAndesiteContinental crustTrace elementGeophysics13. Climate actionSpace and Planetary ScienceFlood basaltFerrar Group; flood basalts; magma contamination; geochemistryGeology
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Zones d'ammonites et de foraminifères du Vraconnien au Turonien : Une comparasion entre les domaines boréal et téthysien (NW Europe / Tunisie central…

2008

International audience; Depuis la fin du 19ème siècle, l'intervalle comprenant l'Albien supérieur élevé, le Cénomanien, le Turonien et le Coniacien basal a été subdivisé d'abord en zones d'ammonites puis, à partir du milieu du 20ème siècle, en zones de foraminifères planctoniques, deux groupes de macro- et de microfossiles particulièrement efficaces en bio-chronostratigraphie grâce à leur taux d'évolution rapide. Toutefois, des différences de compositions fauniques entre le domaine boréal (Europe du Nord-Ouest) et le domaine téthysien (Méditerranée) ont longtemps empêché des corrélations précises entre ces deux domaines. Aujourd'hui, dans un intervalle de temps couvrant environ 16 millions …

foraminifèresCrétacéStratigraphyzones[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDE.MCG.CPE] Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpezonationlcsh:StratigraphyCénomanienTéthys[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylcsh:QE701-760lcsh:QE640-699ammonitesAlbienlcsh:QE1-996.5PaleontologyGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryVraconnienTuronienlcsh:GeologyGeographylcsh:Paleontology[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyCenomanianHumanitiesCarnets de géologie (Notebooks on geology)
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Analysis of cloudiness and solar radiation diurnal cycles for a better understanding of the forests greenness mean annual cycle in Central Africa.

2016

To better understand the Central Africa forests sensitivity toclimate variability, we jointly analyse the mean annual cycles of greenness, rainfall, cloudiness and solarradiation for the target region 0-5°N/12-19°E using high resolution satellite data. Our results demonstrate theimportance of the diurnal scale for understanding the mean annual cycles of rainfall, cloudiness and solarradiation and the way they shape those of forest greenness. They also suggest that whereas the March-Mayrainy season appears optimal for greenness especially because of favorable light conditions, water availabilityis the main controlling factor in December-January the main dry season and in February at the star…

forests[ SDV.BV ] Life Sciences [q-bio]/Vegetal BiologyAfrique CentraleCentral Africacycles diurnessolar radiationcloudinessforêtsradiation solaire[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDV.BV]Life Sciences [q-bio]/Vegetal Biologynébulosité[SDV.BV] Life Sciences [q-bio]/Vegetal Biologydiurnal cycles[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology
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Cycles diurnes de rayonnement solaire et forets en Afrique Centrale.

2018

The sunlightconditions prevailing in Central Africa, and their potential impact on forests traits and functioning, have neverbeen fully explored. Using satellite estimates documenting mostly the period 2005-2013, and accounting forscale interactions between the diurnal and annual cycles, we demonstrate that the seasonality of sunlight levelsstrongly vary across Central Africa forests. Gabon stands out with a main dry season strongly light-deficient,cool and moist. An original map of terra firme forest types developed by CIRAD shows that most of theevergreen forests of Central Africa develop in Gabon. We postulate that despite a mean annual precipitationamount below 2000 mm/yr, the Gabonese …

forestsforêtsAfrique Centrale[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyCentral Africacycles diurnes[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatologysolar radiationdiurnal cyclesrayonnement solaire
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Les difficultés de la construction d’un registre explicatif de la formation des chaînes de montagnes par des apprenants confrontés à un texte histori…

2021

En sciences de la terre et dans le cadre de la théorie de la tectonique des plaques, les processus orogéniques peuvent être difficiles à concevoir par des lycéens et des enseignants. Dans ce papier, on s’interroge, par le biais d’un questionnaire, sur les difficultés à la construction d’un registre explicatif de la formation des chaînes de montagnes par les apprenants. Nous confrontons aussi, dans un atelier-débat, les explications de l’orogenèse proposées par des enseignants à celles avancées par Avicenne. Les registres explicatifs des apprenants sont multiples et l’usage de l’histoire des sciences leur a permis de travailler dans un registre explicatif mobiliste.

formation des chaînes de montagneEarth sciencesSocial Sciences and Humanitieshistory of scienceGéosciencesexplanatory registermountain formationregistre explicatifSciences Humaines et Socialeshistoire des sciences
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Évolution du stress gélif et idéotypes de pois d'hiver dans le contexte de changement climatique, à une échelle régionale.

2017

11 pages; International audience; Pea (Pisum sativum L.) is an important crop in temperate regions for its high seed protein concentration that is particularly sensitive to abiotic stresses. The abrupt temperature increase known as the “1987/1988 temperature regime shift” that occurs over Europe is questioning how winter pea will perform in the changing climate. This study assessed the winter frost damage evolution along from 1961 to 2015 in Burgundy-Franche-Comté by using: (1) daily observed and gridded regional temperature data and (2) a validated crop winter frost stress model calibrated for pea. This study shows a global decrease of the frost stress nevertheless resulting from a subtle …

frost resistance010504 meteorology & atmospheric sciencesmodeling;temperature abrupt shift;winter pea;frost resistance;Burgundy-Franche-ComteBurgundy-Franche-Comté[SDV.SA.AGRO]Life Sciences [q-bio]/Agricultural sciences/AgronomyContext (language use)lcsh:TP670-69901 natural sciencesBiochemistryBourgogne Franche-Comtéwinter peatemperature abrupt shift[ SDV.SA.AGRO ] Life Sciences [q-bio]/Agricultural sciences/AgronomyEffects of global warmingTemperate climateRegime shiftmodélisation0105 earth and related environmental sciences2. Zero hungerAbiotic componentGlobal warmingIdeotypemodeling04 agricultural and veterinary sciences15. Life on landpois d'hiverrésistance au gelGeographyAgronomy[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyrupture des températuresFrost040103 agronomy & agriculture0401 agriculture forestry and fisheries[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatologylcsh:Oils fats and waxesAgronomy and Crop ScienceFood ScienceOilseeds and fats, crops and lipids
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Possible influence of Zoophycos bioturbation on radiocarbon dating and environmental interpretation

2002

Abstract In paleoenvironmental studies of marine sediments bioturbation is often neglected and/or only treated as a diffusion-like process affecting only the uppermost sediment with decreasing intensity with depth. Deep dwelling animals, like the Zoophycos producing animal, however, affect the sediment composition by transporting material over vertical distances of up to 1 m below the seafloor. In Arabian Sea sediment cores 70KL, 64KL and 57KL a significant downward transport of particles by Zoophycos can be observed. Within the Zoophycos burrows the faunal composition of both planktonic and benthic foraminiferal assemblages as well as the isotopic signature of foraminiferal carbonate diffe…

fungiPaleontologySediment550 - Earth sciencesOceanographyBurrowIsotopes of oxygenlaw.inventionPaleontologyIsotopic signatureBenthic zonelawZoophycosRadiocarbon datingBioturbationGeologyMarine Micropaleontology
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The behavior of Rare-Earth Elements, Zr and Hf during biologically-mediated deposition of silica-stromatolites and carbonate-rich microbial mats

2015

Abstract Venere Lake, in the Pantelleria Island thermal system (Central Mediterranean Sea) consists of a mix of seawater and hydrothermal volcanic fluids containing high levels of dissolved SiO 2 . Close to the lake's thermal springs, siliceous stromatolites are deposed under high bacterial activity conditions whereas roughly interlaminated Ca-carbonates and microbial mats are widely scattered in the lake. The dissolved REE speciation in lake waters is dominated by [REE(CO 3 ) 2 ] − , [REE(CO 3 )] + and [REE(H 3 SiO 4 )] 2 + complexes. On the contrary the most abundant Zr and Hf species are hydroxyl- and fluoride-complexes. The behavior of REE Zr and Hf in the Venere lake waters is controll…

geochemistry rare earth elements Zr/Hf ratio Silica-stromatolites Pantelleria IslandMineralmedia_common.quotation_subjectGeochemistry[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeologyPhosphateHydrothermal circulationchemistry.chemical_compoundSpeciationDeposition (aerosol physics)chemistry13. Climate actionEnvironmental chemistryCarbonateSeawater14. Life underwaterMicrobial matGeologymedia_common
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