Search results for " Be"

showing 10 items of 23740 documents

Apparent boudinage in dykes

2004

Intrusive rocks may be arranged in the form of strings of lenses or beads, as found on the Cap de Creus Peninsula, NE Spain, and in the South Finland Migmatite-Granite Belt. These structures first appear to be the result of stretching and boudinage of intrusive sheets or dykes. However, closer examination reveals that they are not boudins, but are instead primary intrusive structures. A detailed study was performed on a swarm of pegmatite intrusions at Cap de Creus. Layering is often continuous between beads, and, in some cases, individual beads exhibit a very irregular shape. These observations are shown to be incompatible with an origin by boudinage. Analogue experiments were used to test…

010504 meteorology & atmospheric sciencesDeformation (mechanics)Irregular shapeMineralogyGeologyBead010502 geochemistry & geophysics01 natural sciences/dk/atira/pure/sustainabledevelopmentgoals/life_below_watervisual_artBoudinageMagmavisual_art.visual_art_mediumSDG 14 - Life Below WaterLayeringPetrologyGeologyPegmatite0105 earth and related environmental sciencesWall rockJournal of Structural Geology
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Unionid shells (Hyriopsis cumingii) record manganese cycling at the sediment-water interface in a shallow eutrophic lake in China (Lake Taihu)

2017

Abstract Aquatic eutrophication is becoming a serious environmental problem throughout the world. The utility of bivalves as bio-filters to improve water quality and reduce algal blooms has been widely acknowledged, but the potential usefulness of bivalve shells as retrospective monitors of eutrophication-induced environmental change has received little attention. Here, we present the first multi-year, high-resolution Mn/Ca shell records of the freshwater mussel, Hyriopsis cumingii (Lea, 1852) from a shallow eutrophic lake (Lake Taihu, China). Mn/Ca shell time-series of the two studied shells exhibit a high degree of synchrony after being placed in a precise temporal context by means of gro…

010504 meteorology & atmospheric sciencesEnvironmental changeAquatic ecosystemPaleontologyMussel010501 environmental sciencesOceanography01 natural sciencesAlgal bloomOceanographySediment–water interfaceWater qualityBivalve shellEutrophicationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Noble gas magmatic signature of the Andean Northern Volcanic Zone from fluid inclusions in minerals

2021

Trace volatile elements like He are key for understanding the mantle source signature of magmas and to better constrain the relative roles of subduction and crustal processes to the variability of along-arc chemical and isotopic signatures of magmatic fluids. Here we report on noble gas abundances and isotopic data of Fluid Inclusions (FIs) in eruptive products and/or fumarolic gases from the Colombia-Ecuador segment of Andean Northern Volcanic Zone (NVZ). FIs in olivine phenocrysts from Ecuador (El Reventador, Cotopaxi and Tungurahua) yield air-normalized corrected He-3/He-4 ratios of 7.0-7.4 R-A, within the MORB range (8 +/- 1 R-A). With exception of the Cotopaxi lavas (opx = 50 km at the…

010504 meteorology & atmospheric sciencesGeochemistryAndean Volcanic Belt Helium voclanic gases Crustal thickness Fluid inclusions Helium Noble gases Northern Volcanic Zoneengineering.material010502 geochemistry & geophysics01 natural sciencesHeliumMantle (geology)Noble gaseGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCrustal thickneFluid inclusions[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentVolatilesFluid inclusions0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryOlivineSubductionGeologyNorthern Volcanic ZoneFluid inclusionNoble gasesCrustal thicknessVolcanoAndean Volcanic BeltengineeringPhenocrystGeology
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Oligo-Miocene lacustrine microbial and metazoan buildups from the Limagne Basin (French Massif Central)

2018

The Limagne Basin (French Massif Central) is an extensive continental lacustrine system accommodating microbial and metazoan buildups from Chattian to Aquitanian age. A description of these buildups and their associated biotic components in Grand Gandaillat and Crechy quarries provides insights into their spatio-temporal distribution patterns. Flats, cauliflowers, domes, cones and coalescent columnar morphologies have been identified with a main laminated mesofabric and laminated, columnar, filamentous and caddisfly-coated microfabrics. Two low-gradient margin models emerged based on the changes in the distribution, morphology and size of the microbial and metazoan-rich deposits through tim…

010504 meteorology & atmospheric sciencesGeochemistryCarbonatesVolcanismEcological successionStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesVolcanismMarlCycle ClimateEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryPaleontologyMassif15. Life on landTectonicTectonicsVolcanoSedimentary rockLacustrine/palustrine[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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The oldest granite clast in the Moodies conglomerate, Barberton greenstone belt, South Africa, and its likely origin

2018

010504 meteorology & atmospheric sciencesGeochemistryGeologyGreenstone belt010502 geochemistry & geophysics01 natural sciencesGeology0105 earth and related environmental sciencesConglomerateSouth African Journal of Geology
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Social Representations of Flooding of Future Teachers of Primary Education (Social Sciences): A Geographical Approach in the Spanish Mediterranean Re…

2020

The risk of flooding is the main natural hazard that affects the European Mediterranean region. This hazard has worsened in recent decades due to the occupation of flood areas and the effects of climate change. Therefore, understanding and gaining a more in-depth knowledge of social representations of flooding is important. In addition, interest in this subject is accentuated in the case of future teachers. This is because it is mandatory to teach this subject in Primary Education (Grades 1&ndash

010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentPrimary educationLand managementClimate changeTJ807-830Educació primàriainstructionManagement Monitoring Policy and LawTD194-19501 natural sciencesgeographyRenewable energy sourcesEffects of global warmingNatural hazardparasitic diseasesGE1-350Social scienceInstruction0105 earth and related environmental sciencesFlood mythEnvironmental effects of industries and plantsGeographyRenewable Energy Sustainability and the Environmentfungi05 social sciencesFlooding (psychology)Educació ambientalfood and beverages050301 educationHazardFloodsEnvironmental sciencesGeographyCanvi mediambiental globalfloodsAnálisis Geográfico Regional0503 educationCanvis climàtics
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2021

Abstract Contaminated soils are lands in Europe deemed less favourable for conventional agriculture. To overcome the problem of their poor fertility, bio-fertilization could be a promising approach. Soil inoculation with a choice of biological species (e.g. earthworm, mycorrhizal fungi, diazotroph bacteria) can be performed in order to improve soil properties and promote nutrients recycling. However, questions arise concerning the dynamics of the contaminants in an inoculated soil. The aim of this study was to highlight the soil-plant-earthworm interactions in the case of a slightly contaminated soil. For this purpose, a pot experiment in controlled conditions was carried out during 2 month…

010504 meteorology & atmospheric sciencesHealth Toxicology and MutagenesisBiomass010501 environmental sciencesToxicologycomplex mixtures01 natural sciencesNutrient0105 earth and related environmental sciences2. Zero hungerbiologyChemistryEarthwormTrace elementfood and beveragesGeneral Medicine15. Life on landbiology.organism_classificationPollutionSoil contamination6. Clean waterBioavailability13. Climate actionEnvironmental chemistryBioaccumulationSoil waterEnvironmental Pollution
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Comparing flow resistance law for fixed and mobile bed rills

2019

Rills caused by run-off concentration on erodible hillslopes have very irregular profiles and cross-section shapes. Rill erosion directly depends on the hydraulics of flow in the rills, which may differ greatly from hydraulics of flow in larger and regular channels. In this paper, a recently theoretically deduced rill flow resistance equation, based on a power–velocity profile, was tested experimentally on plots of varying slopes (ranging from 9% to 26%) in which mobile and fixed bed rills were incised. Initially, measurements of flow velocity, water depth, cross-section area, wetted perimeter, and bed slope, carried out in 320 reaches of mobile bed rills and in 165 reaches of fixed rills, …

010504 meteorology & atmospheric sciencesHydraulicsfixed bedFlow (psychology)0207 environmental engineering02 engineering and technology01 natural scienceslaw.inventionWetted perimetersymbols.namesakelawFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalirill hydraulic020701 environmental engineering0105 earth and related environmental sciencesWater Science and Technologygeographysoil erosiongeography.geographical_feature_categoryrill flowplot measurementRillFlow conditionsFlow velocitymobile bedsymbolsflow resistanceSediment transportGeologyHydrological Processes
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Microbiology and atmospheric processes: biological, physical and chemical characterization of aerosol particles

2008

Abstract. The interest in bioaerosols has traditionally been linked to health hazards for humans, animals and plants. However, several components of bioaerosols exhibit physical properties of great significance for cloud processes, such as ice nucleation and cloud condensation. To gain a better understanding of their influence on climate, it is therefore important to determine the composition, concentration, seasonal fluctuation, regional diversity and evolution of bioaerosols. In this paper, we will review briefly the existing techniques for detection, quantification, physical and chemical analysis of biological particles, attempting to bridge physical, chemical and biological methods for …

010504 meteorology & atmospheric sciencesIndoor bioaerosollcsh:LifeBiological particles[SDU.STU]Sciences of the Universe [physics]/Earth SciencesNanotechnology[SDU.ASTR] Sciences of the Universe [physics]/Astrophysics [astro-ph]01 natural sciences[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]03 medical and health scienceslcsh:QH540-549.5[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processes[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere0303 health sciences[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph][SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmosphere030306 microbiologyChemistrylcsh:QE1-996.5[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentAerosolCharacterization (materials science)lcsh:Geologylcsh:QH501-531[PHYS.ASTR.CO] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]13. Climate action[SDU.STU] Sciences of the Universe [physics]/Earth SciencesIce nucleuslcsh:EcologyBiochemical engineeringAerosol sampling
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Igneous petrology, zircon geochronology and geochemistry of multiply emplaced granitoid bodies from the Palaeoproterozoic Usagaran domain in central …

2019

Abstract This study reports igneous petrology, zircon ages and geochemistry for Palaeoproterozoic I-type granitic, granodioritic, Qtz-monzonitic, Qtz-monzodioritic and monzodioritic rocks from the Usagaran domain of southwestern Tanzania. These rocks can be subdivided into three groups according to their age, T-t evolution and geochemistry. The oldest group is made up of amphibolite-facies calcic-alkalic gneisses, ranging in age between ∼1984 and ∼1910 Ma, which have been divided into two subgroups regarding their T-t evolution. The first subgroup shows a constant increase in T, and the second subgroup first shows a decrease in T, followed by an increase in T. The second group consists of a…

010504 meteorology & atmospheric sciencesMantle wedgeGeochemistryPartial meltingGeologyMozambique Belt010502 geochemistry & geophysics01 natural sciencesContinental arcGeochronologyMagmaIgneous differentiationGeology0105 earth and related environmental sciencesEarth-Surface ProcessesZirconJournal of African Earth Sciences
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