Search results for "Ridge"

showing 10 items of 531 documents

Experimental investigation on different rainfall energy harvesting structures

2018

In this paper proposes an experimental comparison between different rainfall harvesting devices and the study of the corresponding electrical rectifying circuit. More in detail, three harvesting structures are considered: the cantilever, the bridge and the floating circle. For each of the proposed structure, different waveforms have been acquired and discussed. The processed data have been compared in order to suggest the best choice for the rectifying circuit, from the simplest one to the most endorsed in the technical literature.

010302 applied physicsCantileverComputer scienceRenewable Energy Sustainability and the EnvironmentRainfall energy harvester02 engineering and technologySettore ING-IND/32 - Convertitori Macchine E Azionamenti Elettrici021001 nanoscience & nanotechnology01 natural sciencesTechnical literatureBridge (nautical)Settore ING-IND/31 - ElettrotecnicaTransducer0103 physical sciencesAutomotive EngineeringElectronic engineeringWaveform0210 nano-technologyEnergy harvestingPiezoelectric effectHardware_LOGICDESIGN
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3D modeling of growth ridge and edge facet formation in 〈100〉 floating zone silicon crystal growth process

2019

Abstract A 3D quasi-stationary model for crystal ridge formation in FZ crystal growth systems for silicon is presented. Heat transfer equations for the melt and crystal are solved, and an anisotropic crystal growth model together with a free surface shape solver is used to model the facet growth and ridge formation. The simulation results for 4″ and 5″ crystals are presented and compared to experimental ridge shape data.

010302 applied physicsMaterials scienceSiliconPhysics::Opticschemistry.chemical_elementCrystal growthGeometry02 engineering and technologyEdge (geometry)021001 nanoscience & nanotechnologyCondensed Matter PhysicsRidge (differential geometry)01 natural sciencesInorganic ChemistryMonocrystalline siliconCrystalchemistryCondensed Matter::SuperconductivityFree surface0103 physical sciencesMaterials ChemistryFacet0210 nano-technologyJournal of Crystal Growth
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Effect of process parameters and crystal orientation on 3D anisotropic stress during CZ and FZ growth of silicon

2017

Abstract Simulations of 3D anisotropic stress are carried out in and oriented Si crystals grown by FZ and CZ processes for different diameters, growth rates and process stages. Temperature dependent elastic constants and thermal expansion coefficients are used in the FE simulations. The von Mises stress at the triple point line is ~5–11% higher in crystals compared to crystals. The process parameters have a larger effect on the von Mises stress than the crystal orientation. Generally, the crystal has a higher azimuthal variation of stress along the triple point line (~8%) than the crystal (~2%). The presence of a crystal ridge increases the stress beside the ridge and decreases it on the ri…

010302 applied physicsMaterials scienceSiliconTriple pointPhysics::Opticschemistry.chemical_element02 engineering and technology021001 nanoscience & nanotechnologyCondensed Matter PhysicsRidge (differential geometry)01 natural sciencesThermal expansionInorganic ChemistryStress (mechanics)CrystalCrystallographychemistryCondensed Matter::Superconductivity0103 physical sciencesMaterials Chemistryvon Mises yield criterionComposite material0210 nano-technologyLine (formation)Journal of Crystal Growth
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Magnetostructural correlations in CuII−NC−WV linkage: the case of [CuII(diimine)]2+−[WV(CN)8]3− 0D assemblies

2009

International audience; We report on the syntheses, crystal structures, and magnetic properties of two cyano-bridged molecular assemblies: [CuII(phen)3]2{[CuII(phen)2]2[WV(CN)8]2}(ClO4)2·10H2O (phen = 1,10-phenanthroline) (1) and {[CuII(bpy)2]2[WV(CN)8]} {[CuII(bpy)2][WV(CN)8]}·4H2O (bpy = 2,2′-bipyridyl) (2). Compound 1 consists of cyano-bridged [CuII2WV2]2− molecular rectangles and isolated [CuII(phen)3]2+ complexes. The molecular structure of 2 reveals cyano-bridged trinuclear [CuII2WV]+ and dinuclear [CuIIWV]− ions. Magnetic interactions in 1 are interpreted in terms of the model of a tetranuclear moiety consisting of two ferromagnetic CuII−NC−WV units (J1 = +39(4) cm−1) interacting ant…

010405 organic chemistryStereochemistryChemistryCrystal structureCrystal structureMagnetic response[CHIM.MATE]Chemical Sciences/Material chemistry010402 general chemistry01 natural sciencesAntiferromagnetic coupling0104 chemical sciencesIonInorganic ChemistryCrystallographyFerromagnetismTheoryofComputation_ANALYSISOFALGORITHMSANDPROBLEMCOMPLEXITYMagnetic propertiesMoleculeMoietyChemical synthesisPhysical and Theoretical ChemistryCyano bridged molecular assembliesDiimine
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A geological field trip to the Côte d'Ivoire-Ghana transform margin

1998

Abstract During the Equanaute survey (June 1992), fourteen submersible dives were performed between 4950 and 2250 m water depths across the southern slope of the Cote d'Ivoire-Ghana Marginal Ridge (CIGMR), in the eastern Equatorial Atlantic. The CIGMR, a high-standing topographic marginal ridge along the Cote d'Ivoire-Ghana transform margin, is believed to result from a complex structural evolution due to the specific wrench-related rifting between Western Equatorial Africa and Northeastern Brazil, in Early Cretaceous times. In this paper we report and discuss geological observations made during dives, and sample analyses to resolve the lithology, paleoenvironmental conditions, age and orig…

010504 meteorology & atmospheric sciencesCôte d’Ivoire-GhanaLithologyAtlantique EquatorialMid-Atlantic RidgeAquatic ScienceStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontology14. Life underwaterGéologieCôte d’lvoire-Ghana0105 earth and related environmental sciencesEquatorial AtlanticgeographyRiftgeography.geographical_feature_categoryMarge transformanteGeology15. Life on landTectonics13. Climate actionRidgeClastic rockSedimentary rockTransform marginGeologyOceanologica Acta
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Mountain building in NW Sicily from the superimposition of subsequent thrusting and folding events during Neogene: structural setting and tectonic ev…

2017

We present a 1:25.000 scale geological map of the Kumeta-Pizzuta ridge in north-western Sicily (Italy), achieved by integrating stratigraphic, structural and geophysical data. In this area, the tectonic edifice results from the piling-up of deep-water-, carbonate platform- and pelagic platform-derived tectonic units (Imerese and Sicilide, Panormide and Trapanese domains, respectively) resulting from deformations of the former southern Tethyan continental margin. The structural setting shows interference of tectonic events, different types of structural styles and different scales of deformational patterns. Early overthrust of the Imerese on the Trapanese units (since the late Serravallian) …

010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformGeography Planning and Development010502 geochemistry & geophysicsNeogene01 natural sciencesgeological mapContinental marginlcsh:G3180-9980Sicily; Kumeta ridge; backthrust; geological mapEarth and Planetary Sciences (miscellaneous)SuperimpositionSicily0105 earth and related environmental scienceslcsh:Mapsgeographygeography.geographical_feature_categoryKumeta ridgeGeologic mapTectonicsMountain formationRidgeSeismologyGeologybackthrust
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Submarine morphology of the Comoros volcanic archipelago

2021

co-auteur étranger; International audience; A detailed morpho-bathymetric study of the Comoros archipelago, based on mostly unpublished bathymetric data, provides a first glimpse into the submarine section of these islands. It offers a complete view of the distribution of volcanic structures around the archipelago, allowing to discuss the origin and evolution of this volcanism. Numerous volcanic cones and erosional-depositional features have been recognized throughout the archipelago. The magmatic supply is focused below one or several volcanoes for each island, but is also controlled by lithospheric fractures evidenced by volcanic ridges, oriented along the supposed Lwandle-Somali plate bo…

010504 meteorology & atmospheric sciencesVolcanic ridges[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographySubmarine volcanismVolcanism010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyComoros archipelagoGeochemistry and PetrologyLithosphereComoros archipelago Mass slope instabilities Morpho-bathymetry Mounds Submarine volcanism Volcanic cones Volcanic ridges[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyVolcanic conesMass slope instabilitiesBathymetry14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMorpho-bathymetrySubmarineGeologyPlate tectonicsVolcanoArchipelagoMoundsVolcanic coneGeology
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Seafloor expression of oceanic detachment faulting reflects gradients in mid-ocean ridge magma supply

2019

International audience; Oceanic detachment faulting is a major mode of seafloor accretion at slow and ultraslow spreading mid-ocean ridges, and is associated with dramatic changes in seafloor morphology. Detachments form expansive dome structures with corrugated surfaces known as oceanic core complexes (OCCs), and often transition to multiple regularly-spaced normal faults that form abyssal hills parallel to the spreading axis. Previous studies have attributed these changes to along-axis gradients in lithospheric strength or magma supply. However, despite the recognition that magma supply can influence fault style and seafloor morphology, the mechanics controlling the transition from oceani…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Fault (geology)010502 geochemistry & geophysics01 natural sciencesGeochemistry and PetrologyLithospheremagmatismEarth and Planetary Sciences (miscellaneous)PetrologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographyoceanic core complexesgeography.geographical_feature_categoryMid-ocean ridgeSeafloor spreadingDetachment faultnumerical modelingGeophysicsSpace and Planetary ScienceRidgeAbyssal hillMagmatismmid-ocean ridgesmarine geologyfaultingGeologyEarth and Planetary Science Letters
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Turia river delta and coastal barrier-lagoon of Valencia (Mediterranean coast of Spain): Geomorphological processes and global climate fluctuations s…

2019

Abstract Extensive drillings and 31 new C-14 datings were used to establish the geomorphological evolution of the Turia river delta and coastal barrier-lagoon system of Valencia (Spain) over the last three millennia. Integration of geomorphological, stratigraphic, malacological, sedimentological and geoarchaeological data enables us to relate river Turia avulsions and alluvial episodes to the development of coastal spits and barriers. Geomorphological changes in the study area may also be associated with global climate events, sea-level fluctuations or anthropogenic periods in the Turia catchment. Six phases may be differentiated: (1) a major early alluviation phase during the Iberian perio…

010506 paleontologyArcheologyGlobal and Planetary ChangegeographyRiver deltageography.geographical_feature_category010504 meteorology & atmospheric sciencesCoastal plainGeologyCoastal geography01 natural sciencesPaleoclimatologyBeach ridgeAlluviumPhysical geographyProgradationEcology Evolution Behavior and SystematicsHoloceneGeology0105 earth and related environmental sciencesQuaternary Science Reviews
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Late Quaternary coastal uplift of southwestern Sicily, central Mediterranean sea

2021

Abstract Mapping and luminescence aging of raised marine terraces and aeolian ridges along an ∼90 km coastal stretch in southwestern Sicily provide the first quantitative assessment of vertical tectonic deformation in this region, which spans the frontal part of an active thrust belt. We recognized a staircase of eleven terraces and nine related aeolian ridges. The elevation profile of terraces parallel to the coast shows a >90 km long bell-shaped pattern, onto which shorter-wavelength (∼10 km long) undulations are superimposed. Luminescence ages from terraced beach deposits and aeolian sediments constrain the position of paleoshorelines formed during MIS 5e, 7a and 7c, with a maximum uplif…

010506 paleontologyArcheologyMarine terracesEarly Pleistocene010504 meteorology & atmospheric sciencesPleistoceneLuminescence datingSettore GEO/03 - Geologia StrutturaleFold growth01 natural sciencesMarine terracePaleontologyMediterranean seaContinental marginAeolian ridgeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangegeographyFrontal thrust beltgeography.geographical_feature_categoryThermoluminescence datingBedrockGeologyPleistoceneMediterranean seaAeolian ridgesAeolian processesQuaternaryGeologySouthwestern sicilyQuaternary Science Reviews
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