Search results for "erosion"

showing 10 items of 637 documents

Prevalence of tooth erosion and associated factors in 13-16-year old adolescents in Greece

2012

Objectives: The aim of this study was to estimate the prevalence of dental erosion and to investigate possible associations among dental erosion and medical history, dietary and lifestyle habits in a sample of adolescents in Greece. Study design: The study sample consisted of 770 adolescents, 374 boys and 396 girls aged 13 to 16 years. All individuals were clinically examined and answered questions regarding their medical history, rate and frequency of drinks and food consumption and lifestyle habits. Statistical analysis of the questionnaire items was performed by using the multiple logistic regression analysis model. Results: Two hundreds and sixty adolescents were diagnosed as having den…

Oral Medicine and Pathologybusiness.industryResearchTooth ErosionFood consumptionPrevalenceOdontología:CIENCIAS MÉDICAS [UNESCO]Ciencias de la saludBedtimestomatognathic diseasesEnvironmental healthUNESCO::CIENCIAS MÉDICASMedicineStatistical analysisMedical historyMultiple logistic regression analysisbusinessLifestyle habitsGeneral DentistryJournal of Clinical and Experimental Dentistry
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Erosion and screening of tungsten during inter/intra-ELM periods in the JET-ILW divertor

2020

Abstract Intra-ELM tungsten sources, which dominate the total W source, are quantified in the inner and outer divertor of JET-ILW. The amount of the sputtered W atoms for individual ELMs demonstrates a clear dependence on the ELM frequency. It decreases when the pedestal temperature is lower and, correspondingly, the ELM frequency is higher. Nevertheless, the entire gross erosion W source (the number of eroded W atoms per second due to ELMs) increases initially with ELM frequency and reaches its maximum at fELM ≈ 50–55 Hz followed by its reduction in the high frequency range. The in/out asymmetry of the intra-ELM W sources during ELMs is a critical issue and is investigated in this contribu…

PFCNuclear and High Energy PhysicsMaterials scienceMaterials Science (miscellaneous)media_common.quotation_subjectJET-ILWTungsten erosionchemistry.chemical_elementTungsten01 natural sciencesAsymmetry010305 fluids & plasmasDivertor screening of tungstenPedestal0103 physical sciencesDuct (flow)PSImedia_common010302 applied physicsDivertorlcsh:TK9001-9401Tungsten imaging spectroscopyNuclear Energy and EngineeringchemistryW Divertorlcsh:Nuclear engineering. Atomic powerAtomic physicsddc:624Nuclear Materials and Energy
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Identifying sedimentary structures and spatial distribution of tsunami deposits with GPR - examples from Spain and Greece

2011

Shallow drilling in coastal areas like southern Spain and different parts of Greece (Corinth region and Argolis Gulf) proved evidence for tsunamis. Sedimentary analyses were conducted to identify tsunamigenic deposits, but did not reveal sedimentary structures or spatial distribution of tsunamites in a regional scale. Since drilling is time-intensive and expensive (depending on extend), this method can by far not cover an entire coastal area. On the other hand, distribution and preservation of tsunamigenic deposits seems to be highly variable. We used ground penetrating radar (GPR) in combination with electrical resistivity tomography (ERT) measurements and sedimentological research methods…

PaleontologyBasement (geology)Ground-penetrating radarErosionDrillingSedimentSedimentary rockElectrical resistivity tomographyGeomorphologyGeologySedimentary structures2011 6th International Workshop on Advanced Ground Penetrating Radar (IWAGPR)
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Late Pleistocene to Early Holocene natural and human influenced sediment dynamics and soil formation in a 0-order catchment in SW-Germany (Palatinate…

2013

This paper presents the dynamics of sedimentation processes and soil development of a steeply sloping 0-order catchment in the sandy Lower Bunter of the south-western mid-range mountains in the Palatinate Forest (Germany) during the transition period from the Late Glacial to the Early Holocene. Field investigations, chemical, physical, micromorphological and anthracological analyses revealed a complex palaeosol-sediment sequence along the thalweg of a dry valley, where a significant amount of the sediment from the adjacent slopes had been captured. The deposition of aeolian sands in the lowermost sediment layer took place in the early Late Glacial. The subsequent sediments were deposited by…

PaleontologyPreborealErosionGeochemistrySedimentAeolian processesYounger DryasGlacial periodSiltDeposition (geology)GeologyEarth-Surface ProcessesQuaternary International
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Reconstitution du squelette d'astérides fossiles à partir d'ossicules isolés : intérêt taxinomique et phylogénétique

1999

Abstract Dissociated ossicles of asteroids are frequent in neritic sediments. Until now, this material was mainly used in the identification of species. A new method, associating a morphological analysis and counting of plates, allows the architecture of the skeleton and the shape of the body to be reconstructed. This method provides new elements for taxonomic and phylogenetic comparisons. It also provides indications on the adaptation of the asteroids to their environment. In geological beds, frequencies of the different kinds of plates will allow qualification of bioerosion and taphonomic sorting.

PaleontologyTaphonomyPhylogenetic treeFunctional morphologySorting (sediment)Morphological analysisBioerosionPaleoecologyOcean EngineeringTaxonomy (biology)BiologyEcology Evolution Behavior and SystematicsComptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science
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Geomorphological west-east-section through the north chilean andes near antofagasta

2006

The extremely arid western slope of the Andes near Antofagasta is an area of young tectonic movements on the one hand, but of very low erosion rates on the other. Therefore the relief is characterized by very old erosional forms, but fresh and clearly visible tectonic forms. This is quite evident from the following characteristics of a west-east-section from the Coastal Cordillera to the High Cordillera: 1. The great height and steepness of the western escarpment of the Coastal Cordillera, devoid of deep valleys. 2. The preservation of the miocene and pliocene caliche deposits with highly soluble nitrates in the eastern part of the Coastal Cordillera and of the landforms covered by them. 3.…

PaleontologyTectonicsgeographyTectonic subsidencegeography.geographical_feature_categoryLandformSection (archaeology)ErosionCalicheEscarpmentAridGeology
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Il processo di desertificazione per erosione di massa nel territorio “Alto Belice Corleonese” (Sicilia occidentale).

2008

Pedologia Applicata Land evaluation collina argillosa Erosione Sicilia Carte tematicheSettore AGR/14 - Pedologia
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Can the Caper (Capparis spinosa L.) Still Be Considered a Difficult-to-Propagate Crop?

2021

As a perennial xerophytic shrub, characterized by plesiomorphic features, the caper (Capparis spinosa L.) is naturally spread throughout the Mediterranean basin and occupies an important ecological role, as well as an economic one, in traditional and specialized systems for commercial production. This species, in spite of its wide diffusion, is currently considered at risk of genetic erosion, mainly due to overgrazing and overharvesting for domestic uses and for trade. This situation is made more serious because of the lack of efficient propagation techniques, determining the caper as a “difficult-to-propagate species”. In this review, we report the main available sexual and vegetative prop…

Perennial plantvegetative propagationVegetative reproductionved/biology.organism_classification_rank.speciesPlant Science<i>Capparis spinosa</i>HorticultureBiologyShrubCapparis spinosaSB1-1110CropfoodCapparis spinosa; In vitro propagation; Mediterranean basin; Seed propagation; Vegetative propagationin vitro propagationOvergrazingGenetic erosionved/biologyCapparis spinosaMediterranean basinPlant culturefood.foodSettore AGR/03 - Arboricoltura Generale E Coltivazioni ArboreeAgronomyseed propagationDormancyHorticulturae
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Role of secondary circulation on bank erosion in a large amplitude meandering laboratory channel

2009

This paper reports peculiar results of experimental investigation on the evolution of flow secondary circulation motion along a meander wave. The experiments have been conducted in a large amplitude meandering laboratory channel for two values of the width-to-depth ratio. Attention is focalised on how secondary motion affects the bank shear stress distribution, influencing the bank stability. The analysis essentially highlights that, especially for small width-to-depth ratio, as the channel curvature increases besides the classical central-region secondary circulation cell a counter-rotating circulation cell forms in the outer-bank region. Such counterrotating circulation cell allows to obt…

Physics::Fluid Dynamicsflow velocityOpen-channel flow ; meander wave ; secondary motion ; bank stability.secondary currentBank erosionPhysics::Atmospheric and Oceanic PhysicsSettore ICAR/01 - Idraulica
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Sedimentological implications of an unusual form of the trace fossil Rhizocorallium from the Lower Muschelkalk (Middle Triassic), S. Poland

2011

Specimens of the trace fossil Rhizocorallium isp. with retrusive limbs occur in 10–20-cm-thick composite beds: the bottom layers contain abundant Planolites and Thalassinoides trace fossils, and the top layers are built of horizontally bedded pelitic limestone and contain less bioturbational structures. The first specimens of Rhizocorallium isp. occur just 2–3 cm above the lower surfaces of the top layers. The horizontal protrusive sections are 1 cm high and 1 cm wide. At some sites, the horizontal tunnels end, and the limbs become first obliquely retrusive (45°) at a distance of 1.5–2.5 cm, and then vertically retrusive at a distance of 4–6 cm, or at once vertically retrusive at a similar …

PlanolitesbiologyStratigraphyPalaeontologyPaleontologyGeologyTrace fossilbiology.organism_classificationRhizocoralliumPaleontologyTempestiteThalassinoidesPeliteErosionSedimentologyGeologyFacies
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